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    2009, Volume 16 Issue 4
    01 August 2009
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    State Key Laboratory of Continental Dynamics (Northwest University), Institute of Oil and Gas of Northwest University,  Xian  710069, China
    LIU Che-Xiang DIAO Gong-Ge ZHANG Can WANG Jian-Jiang
    2009, 16(4): 1-12. 
    Abstract ( 2180 )   PDF (1890KB) ( 1164 )  

    The evolution of Tibet Plateau is the most magnificent geodynamic movement and the most important geological event, which influenced fundamentally nearly all fields in geology. Its impact extended to a broad range, causing the direct response of Southeast Asia and Middle Asia and forming the broad Himalayan tectonic domain, which further affected South Asian, West Asian, North Asia and their boundary sea areas. The entirety of these regions is called the TibetHimalayan tectonic domain. In terms of its impact to the neighbor areas, the evolution of Tibet Plateau can be divided into three stages, including the soft collision stage between Indian plate and Eurasian plate and the hard collision stages of early intracontinental joined and late relatively integrated deformation in the Tibet area. The influence of soft collision (6044 Ma) was mainly in and near Yarlung Zangbo Suture Zone. The structural deformation, magmatic activities, metamorphic process and mineralization in the early intracontinental joined stage of hard collision (4422±2 Ma) occurred in Tibet and its edges, which only influenced the broad neighbor areas locally through huge and deep strikeslip faults. During the late stage of hard collision (22±2 Ma to now), the massifs in the area of the present Tibet Plateau underwent strong shortening by compression and joined. When these massifs were assembled and welded into a relatively integrated block, the evolution entered the third stage of relatively totally deformed in the Tibet area. The further collision of Indian plate and Eurasian plate, the main geologic events and deep geologic process in the Tibet Plateau began to influence surrounding terrains obviously. The period of the End Oligocene to the Early Miocene (20±24 Ma) is the important turning period in the evolution of Tibet Plateau. The structural deformation, sedimentary deposit, magmatic activities, metamorphic process and mineralization in Tibet Plateau have evident difference before and after the turning periods, which shows the great change of the geodynamic environment around the turning period. Then the Tibet Plateau started the relatively integrated movement and deformation stage and its influences to the mountain uplift and basin subsidence, to the concentration and dissipation of mineral deposits, and environmental changes were remarkable and increasing with time, which caused the episodic spreading and developing of the TibetHimalayan tectonic domain. The correlation between the regional structures and strata of Tibet Plateau and  EastSoutheast Asia indicates that the dynamic source of the important change in geodynamic environment of the Tibet Plateau was not limited to the inner area of the plateau but with a broad regional geodynamic background.

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    Differential deformation and hydrocarbon accumulation in the superimposed basins.
    SHANG Liang-Jie HUANG Ta-Zhu JIN Wen-Zheng LV Zhi-Zhou HE Chun-Bei NING Fei WANG Feng-Hao
    2009, 16(4): 13-22. 
    Abstract ( 2538 )   PDF (1787KB) ( 975 )  

    The purpose of this paper is to describe the characteristics of the differential deformation in superimposed basins and its control over the hydrocarbon accumulation. The differential deformation of superimposed basin is controlled by polyphase stress field transition, varied deformation medium, and various basin boundaries. The major characteristics of differential deformation are as follows. (1) Polyphase differential deformation controlled by the key tectonic movement and stress field transition. The horsegraben structures are formed under the regional extensional regime at the early stage; the detachment structures and buried hill-drape assemblages are generated relating to the convergent margins at the medium stage; the foldthrust belts are originated in the overlying foreland basins at the later stage. (2) Zonal differential deformation controlled by major fault belts is related to preexisting basement weak zones. The deformation intensity changed regularly in various structural zones. (3) Multilevel differential deformation controlled by decollement zones. The deeplevel detachment structures are associated with basinrange coupling; the mediumlevel detachment structures are related to basement decollement layers, and the shallowlevel detachment structures may have a bearing on plastic deformation associated with the salt bed or argillutite. (4) Segmental differential deformation controlled by transfer zones. The structural styles and kinematics may have a great difference in different segments because of the largescale transfer zones. The local transfer may form favorable oilgas traps. The differential deformation may be closely related to the development of  source rocks, the hydrocarbon accumulation epoch, the trap evolution, the distribution and preservation of  oilgas pools.

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    Subsidence process of extensional basin in postrift period and its dynamic setting.
    TONG Dian-Jun LIN Jian-Ye LEI Chao ZHANG Dun-Xia
    2009, 16(4): 23-30. 
    Abstract ( 1688 )   PDF (2429KB) ( 1298 )  

     Extensional basins closely related to the stretching and thinning of crust and lithosphere, have great potential for important mineral deposits and energy resources. Recently, researches of extensional basins including Atlantic passive continental marginal basin, Australian passive marginal basin, and Cenozoic basin in Eastern China, have indicated that not only in passive marginal basins, but also in  extensional basins of convergent plate setting, the postrift subsidence processes are not uniform and slow ones and not simply controlled by thermal relaxation and equilibration of the lithosphere, but present the characteristics of multiepisode and rapid subsidence, which reflect the controlling role of tectonic activity of the periphery plates and deep lithosphere dynamic factor. On these bases, the article describes briefly the progress of research on the rapid postrift subsidence of typical extensional basins at home and abroad. Combined with the quantitative modeling of the subsidence features of postrift evolution in the Qiongdongnan basin, we have discussed the dynamic mechanisms of episodic and rapid postrift subsidence.

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    JurassicCretaceous sedimentation and evolution of ancient oceanic basin in Bangong Lake Area, Tibet.
    XIE Guo-Gang MO Xuan-Hua DIAO Zhi-Dan DONG Guo-Chen
    2009, 16(4): 31-39. 
    Abstract ( 2484 )   PDF (1170KB) ( 1118 )  

     Based on the geological survey of 1∶250 000 scale in Kana and Ritu Areas, we recognized the vertical and horizontal variation of sedimentation, studied the sedimentary environment and reestablished the JurassicCretaceous sedimentary sequence in three strata areas of western Bangong LakeNujiang suture zone. It was specified that the sedimentation in Bangong LakeNujiang middle Tethys oceanic basin was clearly different from both the southern and northern continental margin of the ocean in JurassicCretaceous period. The evolution of the middle Tethys Oceanic basin can therefore be divided into three stages as earlymiddle Jurassic deepwater ocean, later Jurassic to early Cretaceous relict basin with shallowwater sedimentary rocks and later Cretaceous remnant oceanic basin withering away.

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    Tectonic evolution of remnant oceanic basin and its implication for hydrocarbon.
    LI Jiang-Hai CHENG Hai-Yan DIAO Xing
    2009, 16(4): 40-51. 
    Abstract ( 2020 )   PDF (2563KB) ( 1030 )  

    残余洋盆是板块拼合碰撞过程中残留的、未彻底闭合的洋盆,为碰撞陆块之间最晚闭合的区域。它们在走向上与蛇绿岩缝合带渐变过渡,普遍具有不规则的几何形态(三角形、贝壳形、凹四边形)和复杂的构造边界。盆地内充填大面积的巨厚三角洲浊流相(海底扇)沉积,物源来自于周边造山带的隆升剥蚀。残余洋盆的构造背景、几何形态、鉴别标志及其最终消亡过程,正成为大陆动力学需要深入研究的重大科学问题。由于欧亚大陆内各个陆块尺度较小和陆块数目较多,拼合的陆块边缘形态不完全匹配,古生代末以来,在古亚洲洋盆及特提斯洋盆聚合边界上广泛发育残余洋盆。已发现的残余洋盆实例有:孟加拉湾、黑海、南里海、南沙海槽、东地中海、准噶尔、松潘—甘孜等盆地。它们普遍具有海相沉积巨厚、盆地深度较大、快速而持续的沉降等特点。陆块几何形态不规则、陆块拼合的随机性、板块远大于陆块尺度,均是形成残余洋盆的重要原因。随着板块碰撞及陆块调整,残余洋盆主要发生被动式的消亡,包括巨厚的沉积充填(弧前增生楔及海底浊积扇)及多期构造变形。残余洋盆普遍具有重要的油气价值和勘探前景。

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     Coupling effect between coalification and tectonicthermal events—Geological records of geodynamics of sedimentary basin.
    CAO Dai-Yong LI Xiao-Meng DENG Jiao-Mei
    2009, 16(4): 52-60. 
    Abstract ( 2025 )   PDF (1318KB) ( 1019 )  

    The coal is an organic rock that is very sensitive to geologic conditions, such as temperature and pressure. Coalification process is actually an open system in which coal exchanges energy and materials with the surrounding environment. During the long process of geologic evolution, all types of tectonicthermal activities have occurred and inevitably led to diversification of coal in terms of physics, chemistry, textures and structures. Affected by various geologic agents, the organic matter and the inorganic matter in the coal were moved, differentiated and rebuilt, which influenced the coal seam distribution, coal rank and coal quality, and in some degree recorded a lot of geologic information about the geodynamic process of sedimentary basin. This paper introduces the research advances of coupling effect between coalification and tectonicthermal events at home and abroad, discusses the main scientific problems, and proposes some key research projects for this area.

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    Transformation and deformation of the Paleozoic basins in lower Yangtze areas.
    DING Dao-Gui WANG Dong-Yan LIU Yun-Li
    2009, 16(4): 61-73. 
    Abstract ( 1560 )   PDF (3311KB) ( 1090 )  

    Paleozoic sea facies basins including North JiangsuSouth Yellow Sea area have undergone three episodes of tectonic transformation and deformation since the end of the Middle Triassic. The first episode occurred in the IndoChinese epoch from the end of the Middle Triassic to the Early Middle Jurassic, in which the MesoPaleozoic marine basins underwent thrustingfolding deformation with progressively decreasing intensity, which is caused by the SENW overthrust of the decoupling body of JiangnanXuefeng basement(with the induced SN and EW overthrusting) and the transformation of faulted depression with resilient relaxation at the trailing edge. The second episode occurred in the Yanshan epoch from the Late Jurassic to the Early Cretaceous, in which the basins were superposed by the simple shear caused by the NNEtrending horizontal strikeslip structures (represented by the TanLu fracture zone) and the deformation induced by pullapart and faulting tectonic mechanism. The last episode occurred in the Himalayan epoch from the Late Cretaceous to the Paleogene, in which the lower Yangtze area underwent the transformation and deformation caused by the SN extension and detachment as well as domino type of pullingapart and faulting structures. These three episodes of transformation and deformation facilitated the early accumulation, later thermal evolution and redistribution of marine oil and gas in the Yangtze Plate. This paper discusses the three episodes of tectonic transformation and deformation of the Paleozoic sea facies basins in lower Yangtze area since the end of the Middle Triassic.

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    Analysis of structural kinematics of North Yellow Sea Basin.
    LI Wen-Yong CENG Xiang-Hui WANG Shen-Guo AN Zhan-Feng
    2009, 16(4): 74-86. 
    Abstract ( 1897 )   PDF (1480KB) ( 939 )  

    Based on the new geologicalgeophysical data and structural geometry of North Yellow Sea Basin, we have systemically analyzed the characteristics of structural kinematics of North Yellow Sea Basin using the associative method of basin inverse modeling and macroanalysis for the first time. The result shows that North Yellow Sea Basin had undergone such movements as horizontal extension, horizontal compression, relative strikeslip, vertical differential elevation and subsidence, etc. During the Mesozoic and Cenozoic, in which horizontal extensional movements and vertical differential elevation and subsidence movements played the principal parts in the tectonic movements and in the formation and evolution of North Yellow Sea Basin. The horizontal extensional movements can be divided into three main extensional events—J3K1,E2 and E3, which controlled the evolution of North Yellow Sea Basin, and the extensional intensities of southnorth direction were all strong to weak from east to west, and the biggest extensional intensities of eastwest direction migrated westward from the Mesozoic to the Cenozoic. There were two main stages of the horizontal compressional movements—the Late Cretaceous and the Late EoceneEarly Miocene. The relative strikeslip movements occurred with the horizontal extensional movements and the horizontal compressional movements, which caused the majority of NNEdirection and NWdirection faults to have the characteristics of relatively compressoshear or tensoshear strikeslip. These characteristics are more obvious for the NNEdirection faults. The vertical differential elevation and subsidence movements had the episodicprogressive feature. The Late Jurassic, Early Cretaceous, Eocene, Oligocene and MiddleLate Miocene up to now were subsidence stages, among those the Eocene had the biggest subsidence velocity. The Late Cretaceous, Paleocene and Early Miocene were the risingdenudation stages. The settling of this basin during the Mesozoic and Cenozoic had an obvious migration tendency from east to west. The settling of the east depression was most distinct in the Mesozoic; the main subsidence stage of the central depression was in the Eocene; and the rapid settling of the west depression occurred mainly in the Eocene and continued to the Oligocene.

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     A quantitative study on the growth of boundary faults of the Xujiaweizi faulting depression in the Songliao Basin.
    ZHANG Jun-Long MENG Qi-An ZHANG Chang-Hou GAO Zhan-Wu
    2009, 16(4): 87-96. 
    Abstract ( 2080 )   PDF (2819KB) ( 794 )  

    The Xujiaweizi faulting depression lies in the central part of the Songliao Basin. It is controlled by Songxi and Xuxi faults. Based on the geologic interpretations of the seismic reflection data,we have investigated the growth rate and the evolution of the master faults forming basin boundaries by applying the method of analyzing the relationship of displacementlength along strike of normal faults and the approaches for analyzing growth rate along dip direction. It is revealed that the faults formed mainly in the Shahezi Period. The average growth rate of fault is estimated to be 35 m/Ma and 71 m/Ma for Xuxi and Songxi respectively and larger than 60 m/Ma for the boundary fault system as a whole. During the Shahezi Period, Songxi and Xuxi faults were developed independently with a little soft link around their overlapping part. The Yingcheng Period was another important stage with much more intensive activities of Songxi fault, leading to a larger and deeper faulting depression with thicker sediments infilling. The average growth rate of fault was 18 m/Ma for Xuxi, and 85 m/Ma for Songxi. Hard link occurred between them. Only weak and local faulting activity occurred around some linking areas after the Yingcheng Period. The oil and gas fields are mainly located in the areas where secondary tectonic element developed. This finding bears important implications for the further oil and gas exploration in Xujiaweizi Area.

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    The law of basement preexisting fabric controlling fault formation and evolution in rift basin.
    TONG Heng-Mao NIE Jin-Yang MENG Lian-Jian ZHANG Gong-Bei LI Xiao-Ning
    2009, 16(4): 97-104. 
    Abstract ( 2202 )   PDF (1208KB) ( 982 )  

     In this paper we use the new brittle faulting theory, the “noncoordination criteria”, to expound and analyze the mechanical mechanism of basement preexisting fabric controlling fault formation and evolution, to determine the law of change in preexisting basement fabric activity, and to investigate the controlling role of basement preexisting fabric on fault formation and evolution. Through the study we came to the following conclusions. (1)The basement preexisting fabric (particularly the preexisting fault) has priority in activity, which is the root cause of its control over fault formation and evolution in sedimentary basin. (2)The controlling power of preexisting fabric on basin faulting is determined by its activity that is controlled by the attitude and mechanical property of the preexisting fabric, as well as its stress state, and its activity can be quantitatively described using the activity coefficient (fAS) of preexisting fabric.(3)The faults controlled by basement preexisting fault exhibit remarkable regularity in their locations and trends (strikes), formation orders, inherited features, and the size distributions. (4)The controlling power of basement preexisting fault is the strongest when the fault is perpendicular to the extension direction of the controlled fault and the angle between the preexisting fault and the σ1 of the controlled fault is 45°-(/2); when the angle (α) between the strike of the preexisting fault and the extension direction of the controlled fault becomes smaller gradually, and the dipangle deviated from 45°+(/2), the controlling power will be reduced progressively. (5)The larger the size of the preexisting fault is, the more intensive the controlling power of the preexisting fault on fault formation and evolution will be. The faults controlled by largescale preexisting basement faults tend to constitute the structural framework in rift basin. (6)When the shear strength becoming smaller, the possibility of the occurrence of the rupture in the preexisting weakzone will be increasing, and its controlling power will steadily be enhanced, but its affection is relatively weak comparing to the basement preexisting fault. Using the abovementioned conclusions, a theoretical model for the structural interpretation of seismic data may be constructed. These conclusions may also be used as a theoretical guidance for indepth study of fault system formation and evolution in rift basin.

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    The influence of basement fault on the deformation of complex cover blocks in a uniform stress field—Enlightenment from sandbox experiment.
    MA Bao-Jun QI Jia-Fu NIU Shu-Yin SUN Ai-Qun CAO Ai-Feng SUN Zhi-Shen
    2009, 16(4): 105-116. 
    Abstract ( 2265 )   PDF (2909KB) ( 879 )  

     The activity of previous basement fault has great impact on the deformation of the cover, especially when the stress immediately acts on the basement. The sandbox experiments were employed to simulate the passive deformation of cover fault block in case the deep basement was deformed through strikeslip fault in a uniform stress field. The experiments indicated that a nearly symmetrical strikeslip extension rift formed when extension component exists, whereas a symmetrical bending fold, which is bounded by strikeslip thrusts, was formed when compression component exists. The deformation is characterized by a typical strikeslip structure on the section, and the dimension of deformation region was related to the intensity of extension or compression component. When the stress from basement imposed on cover block, there would be rotation and internal deformation in the previous cover consisting of fault blocks, forming alternative extension and compression. When the basement faults show multiple activations or even reverse movement, some complex structures could be formed on the surface. The ChengdaoKendong buriedhill belt in the middle section of the TanchengLujiang Fault is a typical example of the structure controlled by strikesliding basement. The experiments proved that the reversal and strike sliding of the basement resulted in the rotation and torsion of the fault block, and the incomplete reversal of the cover blocks formed composite flower structure.

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     Structures of deep bed in Jiyang Sag and their control over the development of Mesozoic and Cenozoic basins.
    LIN Jian-Ye XU Jian-Guo ZHANG Dun-Xia
    2009, 16(4): 117-137. 
    Abstract ( 1867 )   PDF (6250KB) ( 1101 )  

     Based on interpretations of the 3D seismic  and well data, we have systematically elucidated the geological representations of Mesozoic and Cenozoic tectonic movements in Jiyang Sag, Bohaiwan Basin. The compressional tectonic system, the extensional tectonic system and the strike slipping tectonic system, which developed in different tectonic evolution stages, have been determined in this paper. The thrusts during Indosinian Movement consist of several arc thrusts protruding to NE or NNE direction, and negative inversion of these thrust controlled strongly the development of late Mesozoic and early Cenozoic basins. The unconformity (Tgm) indicating the main episode of Yanshan Movement has been identified clearly in seismic profiles, and the distribution pattern and the type of late Mesozoic basin in Jiyang Sag have also been determined. Combined with the analysis of regional tectonic dynamic setting, the complicated superposition structure and basinmountain conversion mechanism have been discussed. From the study of tectonic and evolution of sedimentary basin, we have revealed the Mesozoic and Cenozoic intracontinental dynamic process of eastern North China Block, which will be of benefit to the hydrocarbon exploration in the study area.

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    Discovery of compressional structure in WuerxunBeier Sag in Hailar Basin and its geological significance.
    LIU Zhi-Hong LIU Hang-Jun WANG Peng TUN Xiang-Mei SHU De-Feng MO Chuan-Biao
    2009, 16(4): 138-146. 
    Abstract ( 2202 )   PDF (2525KB) ( 910 )  

     Hailar Basin is a MesoCenozoic basin which superimposed on the Paleozoic collision orogenic belt of Inner MongoliaGreater Hinggan Mountain. The basin, trending northeast, consists of five firstorder structural units (three depressions and two uplifts), they are, from west to east, the Zhalenuoer Depression, Cuogang Uplift, Beier Lake Depression, Bayanshan Uplift and Huhe Lake Depression, respectively. Wuerxun  and Beier Sags are two secondorder structural units in the south of Beier Lake Depression. The research indicates that in the Early Cretaceous, WuerxunBeier Sag underwent two longterm compressions: NWSE trending during Damoguaihe Period to early Yimin Period, and near EW trending during late Yimin Period, respectively. The compressions led to the inversion of some depressioncontrolled normal faults in the extensional faulted depression, and formed new faultpropagation fold, faultband fold, imbricate structure, duplex structure, popup structure, triangular zone etc. Because of the differences in geometric and kinematic features and the variance in the ratio of the uplift rate of compressional structures to the deposition rate of isostructurally growing strata in space, the syncollision strata sequences show different sedimentary features in different structural positions. These structural features are very similar to those of orogenic belt. The discovery of two phases of compressional structure in WuerxunBeier Sag proved that the crust of Northeast China was not always in the state of extension and thinning in the Early Cretaceous, but showed the features of superimposition and thickening during the two compression periods, and thus formed structural framework of alternative distribution of compressiondepression basins and intracontinental (intraplate) orogenic belt in space.

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     Cenozoic tectonosedimentary characteristics and extension model of the Northwest Subbasin, South China Sea.
    DING Wei-Wei LI Meng-Bi DIAO Li-Gong RUAN Ai-Guo TUN Zhen-Li
    2009, 16(4): 147-156. 
    Abstract ( 1950 )   PDF (2361KB) ( 1062 )  

    Several seismic profiles and one oceanbottomseismic profile crossing the Northwest Subbasin, South China Sea, are introduced in this article. Based on the interpretations of these profiles and combined with structural geology, we have discussed the Cenozoic tectonosedimentary characteristics and extension model of this subbasin. The results show that the Northwest Subbasin began its seafloor spreading since 30 Ma. The extension activities mostly happened during the Oligocene. The rifts distributed symmetrically around the spreading center, which is occupied by igneous body now. Sediments in this period are characterized by chaotic and discontinuous reflectors, indicating riftfilling clastic sediments. Further to the west, the subbasin has more rifted depression characteristics. After 25 Ma the spreading center migrated to the south, the Southwest Subbasin began its spreading. The NW direction stress caused by it may have ceased the opening of the Northwest Subbasin. The Northwest Subbasin experienced thermal cooling and exhibited a broad subsidence. The ZhongXisha block may have influenced the structural distribution of the basin. The deep crustal structure showed by the velocity model of OBS profile are also symmetrical around the spreading center, which indicates that the Northwest Subbasin experienced its extension in pure shear mode.

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    Genesis, stages and distribution of the fractures in H3 reservoir in Anpeng oil field, Miyang Sag.
    ZHOU Wen ZHANG Yin-De YAN Chang-Hui WANG Hong-Hui SUN Chang-Ru
    2009, 16(4): 157-165. 
    Abstract ( 2267 )   PDF (1289KB) ( 975 )  

     Based on the data of directional core drilling, FMI, routine cores and their thinsections, we have described the characteristics of H3 reservoir in Anpeng oil field, Miyang sag. By analyzing the stable isotopes of 20 fracture infillings and 5 groups of acoustic emission, combined with the studies of fracture characteristics and tectonic evolution, the fractures in H3 member were assigned to the regional fracture type which is characterized by the dominance of vertical or highangle extensional fracture, occurring in groups, relatively stable occurrences and out of the control of local nosetype folds. It has been recognized that there are 4 breaking stages, of which the 2nd one is the major stage. Based on the rock mechanical properties, the distribution of rigid rocks, the thickness of sandstones and the intensity of tectonic stress field, we have systematically discussed the geological factors controlling the fracture developments. The regional stress intensity closely related to the degree of the fracture development is the major extrinsic factor influencing the fractures, while the lithology, the density and the thickness of rocks are the major intrinsic causes. The procedures of tectonic filtering, the stress field simulation and the main curvature calculation have been employed to anticipate and evaluate the areal distribution of fractures of the reservoir groups of Ⅶ, Ⅷ and Ⅸ in the study area.

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    Development characteristics and controlling factors of reservoir fractures in Chaoyanggou Oilfield, Songliao Basin.
    ZHANG Shen BAO Zhi-Dong
    2009, 16(4): 166-172. 
    Abstract ( 2185 )   PDF (989KB) ( 946 )  

    Fractures are the main flowing channel and effective storage space for the low permeability reservoir in Chaoyanggou Oilfield, Songliao Basin. The exploitation of oil deposits in this oilfield is strongly controlled by the complex distribution of fractures. Based on regional tectonic study, core structural analysis and the data from outcrops and thin sections, we have studied the developmental characteristics, the genetic mechanism and the controlling factors of the fractures in the Chaoyanggou Oilfield. The results show that there are four sets of tectonic fractures in the reservoir,  extending in the southnorth, eastwest, northwest and northeast orientations respectively.  The fractures with low dipangle are dominant in the studied area, which are mainly the alongbedding detachment fractures formed by compressive folding, and the shear fractures related to the thrusting of faults. The fractures with high dipangle are mainly the extension fractures and oblique fractures. The tectonic fractures are mainly formed in the reversal tectonic stage at the end of Mingshui Formation, when there developed the nearly SN and nearly EW orientations fractures. The development degree of the fractures is controlled by the factors of lithology, strata thickness, the faulting, the folding, the depth, etc. The development degree of fractures is different with different lithology; there is a linear relationship between the fracture spacing and the fractured strata thickness; most fractures have a relation to the faulting; the types of fractures are different with different formation phases of the fold; and the development degree of fractures is sharply decreased with the increase in depth.

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     The geological basis of late hydrocarbon generation and accumulation in the Lower Paleozoic of Tarim Basin.
    CHEN Rui-Yin DIAO Wen-Zhi ZHANG Shui-Chang WANG Gong-Jun
    2009, 16(4): 173-181. 
    Abstract ( 2365 )   PDF (3120KB) ( 872 )  

     On special geological conditions, the late hydrocarbon generation and accumulation can take place in older formations just as those in the Mesozoic and Cenozoic. The geothermal gradient is gradually decreased in Tarim Basin. The thermal evolution of the Lower Paleozoic was suspended frequently because of multiple uplift denudations of the overlying strata. Hence the organic matter evolution in the Lower Paleozoic was suspended. The differential burial evolution led to the differential thermal evolution in different structural belts. The hydrocarbon generation potential of source rock in some areas can be preserved up to Himalayan period. In Himalayan period, the source rock was buried deeply in short time so that the hydrocarbon was generated plentifully and accumulated efficiently. The activated fault systems in Neotectonic period made the hydrocarbon migration easy. These geological conditions caused the possibility of late hydrocarbon accumulation in Tarim Basin in the Lower Paleozoic. Tazhong, Lunnan and the deeper sites of Mangar Depression are the prospective areas.

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    The reflection horizon T5 in Lufeng Sag: Its sequence stratigraphy and significance in petroleum exploration.
    DAO Zong-Pu DING Fang HE Shi-Bin HAO Jian-Rong GAO Lei XU Kai-Beng QIN Chang-Wen HE Yu-Beng
    2009, 16(4): 182-189. 
    Abstract ( 1894 )   PDF (3082KB) ( 766 )  

    The composite seismic wave of the reflection horizon T5 includes three positive and two negative highamplitude events. The middle positive one is the seismic event of T5 interpreted in this study; it is the best stratigraphic correlation marker and seismic interpretation horizon because of its stability, continuity, and extensive distribution;it is a surface of downlap termination in the deepsag area and a surface of onlap termination in the alongshore and highlandform area. Corresponding to T5, the middle stratum is composed of limestone, and limestone interbedded with sandstone or mudstone; and it is only composed of sandy mudstone in the northwest of Lufeng Sag. It was formed in the first transgression stage of sedimentation during the transition of the Lufeng Sag from a shore zone to a neritic shelf under the long transgression background after the Nanhai movement, with the age of 185 Ma and formed around the maximum flood stage of thirdorder sequence TB21. Above the middle stratum, a set of sandstone strata lies locally, formed as the falling system tract of TB21 and another stage of transgression sedimentation. Under the middle stratum, an interbedded stratum of sandstone and mudstone lies as a fourthorder sequence of TB21. Assemblages of petroleum reservoir and seal rock developed in and about the reflection horizon T5, which was controlled mainly by the sequence cyclicity and successive landform.

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    Some key tectonics characteristics of Chinese foreland basins and their petroleum exploration.
    LI Ben-Liang WEI Guo-Ji GU Cheng-Cao
    2009, 16(4): 190-202. 
    Abstract ( 2197 )   PDF (3034KB) ( 1068 )  

    Chinese foreland basins show many special tectonic characteristics resulting from their tectonic settings and evolution. We have concluded five key tectonics geologic characteristics of Chinese foreland basins based on the study of the sedimentary infill, tectonics evolution, tectonic dynamics, spatial location distribution and structural deformation geometry. (1) The foreland basin is the superimposition of the compression sedimentary stratigraphic sequence with the extension basin, and the foreland basin includes underlying rift basin and upper dustpan flexure deposited basin. (2) The foreland thrustfold structural deformation has occurred four times since the Protozoic, in the Late Caledonian, Late Hercynian, Indosinan and Late Himalayan, respectively. (3) The foreland basin developed based on the control of two factors that are the basin basement collaged by many small plates or terrains and the rejuvenation of ancient orogenic belt, so the foreland basins or foreland thrusts are located in front of ancient orogenic belt. (4) The foreland basins and the rejuvenation of ancient orogenic belt make up a giant basinmountains system resulting from the distant effect of IndiaEurasia collision, which is located on the outer circle of Tibet Plateau, so the thrust deformation intensity, basin deposition range and coupling between orogenic belt and basin changed from strong to weak as from interior to outer circle of Tibet Plateau. (5) There are many structural styles of the thrust and fold belt in different basins, such as brittle behavior faultrelated fold, ductile behavior basementinvolved structure, basementinvolved faultrelated fold, and salt structure. Above tectonics characteristics result in the regularity and complexity of oil pooling. We have put forward some suggestions on the study of tectonics of foreland basin for petroleum exploration.

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     Selected tectonic topics in the investigation of geodynamic process of destruction of North China craton.
    ZHANG Chang-Hou
    2009, 16(4): 203-214. 
    Abstract ( 2026 )   PDF (1500KB) ( 1564 )  

    The destruction of the North China craton is a key problem in the continental geodynamics, which was realized from the comparison research of the lithosphere thickness, thermal gradient, age and components of the underneath mantle lithosphere between the Paleozoic and the Cenozic in eastern North China craton. As the huge amount of thinning of the lithosphere is regarded as one of the most important indicators of the destruction of the North China craton, several geodynamic models were proposed to account for the process of lithosphere thinning in last two decades. Meanwhile, since many other geological records formed during the destruction of the North China craton could not be explained reasonably by these geodynamic models, they could not be naturally treated as geodynamic models for the destruction of North China craton yet so far. Several important tectonic topics are supposed to be taken into consideration before an integrated geodynamic model for the destruction of North China craton is established, they are that (1) the active versus passive rifting model and the roles they played during the destruction of North China craton are supposed to be reevaluated based on detailed identifications of geological events sequences of tectonic deformation, sedimentation and volcanism, and the combination of the thermalchemical erosion model with aforementioned rifting model is expected to form an integrated candidate geodynamic model for the destruction of North China craton; that (2) in addition to the geochemical constraints, the spatial and temporal evolution of the plutonism and volcanism associated with delamination, rapid uplift of the crustal surface and related sedimentation and tectonic deformation should be systematically investigated to evaluate, revise and extend current lithosphere delamination model, and identification of high thermal anomaly expected from inferred delamination and the tectonic deformation responses of the thermal weakened crust caused by delamination to regional tectonic stress field, and the variations of stress derived from delamination as well, are supposed to be carried out toward a better construction of a delamination related geodynamic model; that (3) whether the destruction of North China craton was following an old stabilized craton or a mobile orogenic belt is a key to a better understanding of the process and mechanism of the destruction of North China craton, which require integrations of researches in regional tectonic deformation, syntectonic sedimentation and associated plutonism and volcanism; if the predestruction tectonics of eastern North China craton are of mobile orogenic belt characters, the extensional collapse of orogen should be taken into account during reconstructing the geodynamic process of the destruction of North China craton. 

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    Tectonic division of the upper crust of the North China Block.
    LI Chao WANG Zong-Xiu
    2009, 16(4): 215-224. 
    Abstract ( 2198 )   PDF (4120KB) ( 1512 )  

    By the analysis of natural earthquakes, we obtained the depth, the style of activation, and the strength of the detachment layer in the middle crust. Based on above study and combined with the interpretation of the gravity and magnetic anomalies of the basement of the study region, we propose that there is a regional detachment layer formed in the middle crust in the North China Block, and its depth determines the transition between the shallow and deep deformation in the study region. The detachment layer is the floor boundary of the deformation during the extension of the North China Block. When units of upper crust of the region slip along the detachment layer, owing to different velocities and boundary conditions, the derived cutoff lines, transverse faults and minor related highs and depressions are formed; all these are the basal tectonic units consisting of the upper crust of the North China Block, and they controlled the distribution of the basins and ranges and tectonic landforms basically in the study region. The division scheme of the upper crust in the North China Block is brought forward: there are 9 firstscale units (ⅠⅨ) and 23 secondscale units. Among them, the firstscale units are: Ⅰ EWtrending faulted block of the regional depression in the northern Yinshan; Ⅱ faulted block of YanshanYinshan regional high; Ⅲ faulted block of regional Taihangshan high; Ⅳ faulted block of regional Dabieshan high; Ⅴ faulted sags and uplifts in the Bohai Bay basin; Ⅵ faulted sags and uplifts of southern North China basin; Ⅶ regional faulted uplifts in west Shangdong; Ⅷ regional faulted sags and uplifts in the Lower Yangtze; Ⅸ regional faulted sag of the Ordos.

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    Mesozoic asthenosphere upwelling of Eastern China and its effects on structuremagma mineralizationconcentrated region.
    GENG Ji-Shan YANG Wei-Ran GENG Zuo-Yun LIU Jian-Hua SHAO Jian-She
    2009, 16(4): 225-239. 
    Abstract ( 1745 )   PDF (2412KB) ( 1064 )  

    Based on the detailed study of seismic tomography image in South China, and according to the geotectonic environment and shape and heat  of asthenosphere upwelling, we divided the structure of lithosphereasthenosphere at the Mesozoic upper mantle of Eastern China into three types. (1)Continental platform area (North China platform and Yangtze platform): asthenosphere upwelled along paleorift; over the plume head, the granitic rocks of crust and mantle mixed and correspondingly, Au, Cu, Mo, PbZn, etc. mineralizationconcentrated regions were formed; and at the steep contact belt of asthenosphere and the thick area of lithosphere, mediatebasic complex was formed. (2)Central area of fold zone (Nanling and its extension zone): asthenosphere was “recumbent” at suitable depth, with adequate heat and in a great extent; by heat conduction, the interior of partial crust remelted, and the crustsource granitic rocks, and correspondingly, W, Sn and rare elements mineralizationconcentrated regions were formed. (3)Marginal area of fold zone (Southern Daxinganling and southern margin of South China): the mantlesource or crustmantle mixed granitic rocks, and correspondingly, Cu, Au, PbZn, Mo, Ag mineralizationconcentrated regions were formed. In conclusion, asthenosphere upwelling is the origin of the formation of Mesozoic structures, magma, and mineralizationconcentrated regions.

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     Distribution and activity of Tanlu fault belt in Cenozoic shown by  seismic data.
    YANG Ke-Min HU Beng DANG Xiao-Chun
    2009, 16(4): 240-251. 
    Abstract ( 2010 )   PDF (5257KB) ( 981 )  

    The Tanlu fault belt, being a preNeogene giant fault belt located in the marginal Pacific area of East China, can be divided into southern, central and northern segments, and seven subsegments based on the geologic contexture shown in seismic data. In petroleum industry, there are two different views on the belt in terms of effective extension of the belt, i.e. the broad sense of Tanlu fault belt and the narrow sense of Tanlu fault belt. The geological contexture of the broad sense of preNeogene Tanlu fault belt includes two basins separated by the central uplift, and the geological contexture of the narrow sense of Tanlu fault belt consists of a central horst belt and the faults on its both sides. The broad sense of Tanlu fault belt is unacceptable because of its broadening the limitation of Tanlu fault belt and the existence of inversion and flower structures developed both inside and outside of the belt. The general extension of the narrow sense of Tanlu fault belt is NNE, and changes to NE on the south of Jiashan. The preNeogene faults (extending EW, NE and NEE) on both sides of the belt intersect the belt with acute angles. The boundary faults of all Paleogene halfgrabens developed on both sides of the belt from north to south are growth faults. It indicates that the Paleogene basins are extension basins rather than the pullapart basin. The dextral strikeslip stress superimposed on the paleogene structural layer was caused by the underthrusting of Pacific plate beneath the Eurasian plate. The left translational movement of the belt resulted from the north underthrusting of Kula plate beneath the Eurasian plate during the Mesozoic. The intersection position of Tanlu NE translational strikeslipping fault and the subtle faults extending NW is the structural position for earthquake generation. So, we should pay more attention to supervise the earthquake activity in the intersection position of Gaoliying growth fault (extending NE) and the subtle fault of BozhongSunheNankou which extending NW.

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    P wave velocity structure in the crust and upper mantle beneath northeastern South China Sea and surrounding regions.
    LI Zhi-Wei XU Yi HAO Tian-Yao XU E LIU Jin-Song
    2009, 16(4): 252-260. 
    Abstract ( 1805 )   PDF (2248KB) ( 1420 )  

    With the Pwave arrival times from Chinese and ISC stations, we conducted the tomographic inversion for the 3D velocity structure in the crust and mantle beneath the northeastern South China Sea (SCS) and surrounding regions by using spherical finite difference technique. We analyzed the tectonic differences and deep geodynamic characteristics based on the tomographic results, which show high velocity anomalies at the uppermost mantle beneath the northeast SCS, and depict the lithospheric mantle extension from South China continent to marginal sea. Because of the low temperature and thick lithosphere beneath the northeast SCS, it seems no magma intruded from mantle, so we inferred that the rift may only occur in the crust rather than extend to the upper mantle, which shows the nature of nonvolcanic continental margin. The low velocity anomalies at the central subbasin suggest the uplift of hot materials in the mantle. The high velocities at South China continent and Taiwan region, and the low velocities at Okinawa Trough depict the different tectonics of the crust: the former ones belong to the normal crust of Eurasia continent or thickened crust caused by the collision between Philippine Sea Plate and Eurasia Plate, while the latter one belongs to the thinned crust caused by backarc spreading. Between the high velocities of South China continent and northeast SCS, the Binhai fault belt depicts the suture of South China block and SCS block, and the low velocities at upper mantle suggest the deepdriven magma process beneath the marine of South China continent. The velocity anomalies at Luzon, Manila Trench and East Luzon Trench relate to their tectonics natures. The low velocities at the upper mantle from southern Taiwan to northern Luzon depict two volcanic chains: western volcanic chain (WVC) and eastern volcanic chain (EVC). The high velocity belt at north Luzon ridge depicts the subducted continental slab.
    Key words: Northeastern South China Sea; P wave velocity structure; lithospheric mantle; seismic tomography

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    Nanning Cenozoic asthenosphere upwelling plume and its influence on the shallow surface structure.
    LI Xi-Guang YAN Xiao-Min LIANG Ji
    2009, 16(4): 261. 
    Abstract ( 1794 )   PDF (1964KB) ( 905 )  

    Based on the integrated research of intermediate structure, regional faults, Cenozoic basins and threedimensional numerical simulation, we further analyze the impact of the Nanning Cenozoic asthenosphere upwelling plume tectonics on the shallow surface structure of the study area. A series of transitional structures, generated at the margin of the asthenosphere upwelling plume, affect the activities of NEtrending and NWtrending regional faults near the central of plume. Simultaneously, during the asthenosphere upwelling and flowing to southeast, the plume caused the movement of the upper crust mass, which led to the following events: the extension of the center, the west and the north of the plume; the formation of fault basins on the shallow surface; the enhancement of the activity of NEtrending and NWtrending regional faults in the southeast; the generation of the Lingshan midstrong seismic active region. The conclusion has further been tested by the threedimensional numerical simulation.

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     Sintering reaction of pseudoleucite syenite: Thermodynamic analysis and process evaluation.
    TAN Dan-Jun MA Hong-Wen LI Ge LIU Gao JU Dan
    2009, 16(4): 269-276. 
    Abstract ( 1492 )   PDF (920KB) ( 930 )  

     Based on comprehensive analysis of the modal composition of a pseudoleucite syenite ore collected from the Zijin Hill of Lin County, Shanxi Province, we carried out a thermodynamic analysis of pseudoleucite syenite sintering process with sodium carbonate as the additive. It indicates that when the pseudoleucite syenite was sintered at 760880 ℃ for 1015 h, with the sodium carbonate as the additive, the decomposition rate of minerals in the pseudoleucite syenite could reach 971%. The thermodynamic calculation shows that it needs to consume 065 t of Na2CO3 in treating pseudoleucite syenite ore per ton, and about 95% Na2CO3 could be recycled. This process consumed (229248)×10-6 kJ of heat energy, corresponding to 1909720682 kg of standard coal and the thermal efficiency was 40%; the CO2 emission is 077081 t. Compared with the Russian limestonesintering technique, the consumption of natural mineral resources and energy, and greenhouse gas emissions in sodasintering technique could be reduced by 65%, 63% and 65%, respectively. Therefore, the procedure suggested in this paper has broad prospects in industrial applications for its economic benefits and environmentalfriendliness.

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     Characteristics and evolution of sedimentary microfacies of Chang 64+5 layer in the northern area of western Mahuangshan.
    LIU Yu-Mei XU Xin-He LI Qing-Li DU Wei-Wei LI Mei LI Shun-Li
    2009, 16(4): 277-286. 
    Abstract ( 1861 )   PDF (2251KB) ( 750 )  

     There are widespread indications of oil and gas in the Chang 64+5 layer of western Mahuangshan, while it proves that there is more water and less oil by well test. Furthermore, the distribution and continuity of sand arent clear. To understand the distribution and evolution of sedimentary microfacies in the area, six kinds of sedimentary microfacies and eight kinds of sedimentary structures were identified and ten kinds of microcontact patterns and five kinds of sedimentary sequence models were summarized by detailed core observation and description and logging data. Each model represents different sedimentary facies.  Reverse cycle is dominant and normal shortterm cycle also exists in the vertical direction; distributary mouth bar and subaqueous distributary channel are developed alternately in the lateral direction. The lower channel sands are “many but small, narrow and thin”, while the upper channel sands are “a few but large, wide and thick”. The “singlefactor analysis and multifactor comprehensive” research method was used to divide this area into three phase beltsdelta inner front, delta outer front and predelta. Subaqueous distributary channel, distributary mouth bar and interdistributary deposits are prevailing in the delta inner front. Distal bar and sand sheet are dominant in the delta outer front and predelta mud is dominant in the predelta. According to modern sedimentary facies model, the area is a constructive braided riverlake delta. Its evolution shows three stages: the initial development period (Chang 63), the main facies belts are the predelta and the delta outer front; the earlymiddle development period (Chang 62Chang 61), the main facies belts are the inner delta front and the delta outer front and each microfacies is a single phase and is deposited alternately; the middlelate development period  (Chang 4+52Chang 4+51), the main facies belt is the delta inner front and the subaqueous distributary channel shows a multiphase stacking pattern.

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    Geochemical natures of copper, nickel and PGE and their significance for the study of origin and evolution of mantlederived magmas and magmatic sulfide deposits.
    SONG Xie-Tan HU Rui-Zhong CHEN Li-Meng
    2009, 16(4): 287-305. 
    Abstract ( 2025 )   PDF (2791KB) ( 25135 )  

    Ni, Cu and PGE are very important in the study of origin and evolution of mantle derived magmas and the formation of the related magmatic sulfide deposits, because their geochemical natures are different from other trace elements. Ni, Os, Ir and Ru are compatible elements, and Cu and Pd are incompatible in sulfur undersaturated magmas. Thus, they may be differentiated during fractional crystallization of the sulfur undersaturated basaltic magma. In contrast, all of these metals will be concentrated in sulfide liquid while sulfur saturation is reached. Particularly, minor sulfide removal will result in PGEdepletion in the basaltic magma because PGE have very high sulfide liquid/silicate melt partition coefficients. Therefore, PGE are the most sensitive tracers for sulfide segregation. Ni, Cu and PGE are also very important in the studies of key factors of the formation of magmatic sulfide deposits, which resulted from the evolution of mantle derived magmas. They are also significant for revealing fractionation of sulfide melts because Ni, Cu and PGE have different sulfide solid solution/sulfide liquid partition coefficients. In this article, the significances of Ni, Cu and PGE in the studies of origin and evolution of mantle derived magmas and the formation of magmatic sulfide deposits are presented systemically, based on the introduction of natures of these elements.

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    Sedimentary facies analysis based on the spatial information and its application.
    SUN Jing XUE Lin-Fu DIAO Yu-Ting
    2009, 16(4): 306-312. 
    Abstract ( 1712 )   PDF (1192KB) ( 1044 )  

    In this paper, the sedimentary facies are grouped into fanshaped sedimentary facies, sheet sedimentary facies and banded sedimentary facies based on the plane distribution patterns of sedimentary facies, and different buffer zone methods are used for different types of sedimentary facies. Based on the Walther’s law of facies, we have analyzed the wells of known sedimentary facies types. Moreover, we have carried out the automatic analysis of the plane sedimentary facies for the wells with known sedimentary facies types by using computeraided programming and replacement of manual works. The feasibility of this method was proved by the study of the sedimentary facies of K2 member in the Kongnan area of Dagang Oilfield.

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    The enlightenment from  thermoelectricity of a few natural semiconductor minerals for seismic electric field change.
    SHEN Dun-Feng SHEN Xu-Hui LIU Qian
    2009, 16(4): 313-319. 
    Abstract ( 1650 )   PDF (966KB) ( 877 )  

     Under different active temperature, the thermovoltage of four kinds of typical minerals, such as magnetite, arsenopyrite, pyrite, and chalcopyrite, were tested by thermoelectricity equipment BHTE06. All the minerals showed that the absolute value of the thermovoltage rose with active temperature increasing. Based on the theory of thermoelectricity and the analysis of genetic environment of natural minerals, we assume that the semiconductor minerals widely exist in crust and most of them have the thermoelectric property. Because the isogenetic electronmagnetic field and thermal field can interact with each other while the earthquake is generated and occurred, we propose that the thermal field can excite the semiconductor minerals to produce thermoelectric effects and a new additional thermoelectric field. The additional thermoelectric field may provide precursory information for earthquake prediction. The thermoelectricity produced by widely existing natural semiconductor minerals in crust may play an important role in the abnormal change of geoelectric field during the gestation and occurrence of an earthquake. Therefore, the indepth study of thermoelectric effects of natural semiconductor minerals is of revelatory significance for understanding the general mechanism of abnormal change of geoelectric field before an earthquake.

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    Complexity of ore controlling fractures of Dajishan tungsten deposit.
    LIU Ning-Jiang WU Chong-Wen
    2009, 16(4): 320-325. 
    Abstract ( 1620 )   PDF (965KB) ( 997 )  

    To understand the complexity of the development and evolution of orecontrolling fracture system in Dajishan tungsten deposit, Quannan County, Jiangxi Province, we collected rock samples at different depth of deposit, and performed experiments on rock acoustic emission. The results showed that the sequence of rock acoustic emission events has a distinctive feature, and generally goes through three processes of occurrence, quiescence and burst. The onset and development of fracture system has a cascade of avalanchespunctuated equilibrium hierarchic fractal structure. The breaking process is extremely discontinuous in time, and the energy release in the process is also discontinuous and decreasing with depth, which reflects the development of mineralization. The author applies the theory of complexity to studying the orecontrolling fractures of the veintype tungsten ore deposits in Dajishan. The following conclusions were drawn. The dynamics of the onset and development of fracture system is similar to that of the oreforming system; that is, it consists of the selforganization arising from the coupling of random motion, the coherent behavior produced by interaction between subsystems, the realization of cooperative synchronization, the occurrence of critical transition point, and the attainment of selforganized criticality. All of them result from the coupling and interaction of physical movement of minerals, time and space. The formation of veintype tungsten ore deposit in Dajishan is closely related to critical rupture of orecontrolling fracture system and its avalanchespunctuated equilibrium cascade fractal growth, i.e., the metallogenic model of veintype tungsten ore deposit in Dajishan follows the generalized “fivestoreyed type” metallogenic model.

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    Application of prognostication from comprehensive information based on GIS to ores prospecting in crisis mines—A case from Yinan gold mine.
    XIANG Zhong-Lin GU Xue-Xiang DONG Shu-Xi WANG Yan
    2009, 16(4): 326-334. 
    Abstract ( 1552 )   PDF (9273KB) ( 1135 )  

    In the 21st century, with the fast development of industry, there is much need for the mineral resources; however, a few mines face serious resource crisis. Looking for ore in the outside and in the depth of the mine is a basic and main way that solves the crisis mine problems. Additionally, with the development of geosciences and the continuing progress of mineral exploration, mass geoscience data have been accumulated,  and the mineral exploration has entered a new era that is marked by the heavy dependence of ore finding on comprehensive information.  In this article, under the guidance of metallogenic forecasting theories such as the Analogy Comparison and the Anomalycaused Mineralization, the authors utilized GIS technology, applied analytic hierarchy process (AHP) method, through building, quantifying and operating in fuzzy logic on the prospecting model of synthetic information, acquired and interpreted the target area in the Yinan gold mine, and discussed the method and process in multiinformation metallogenic prediction based on GIS. The engineering testing and verification results indicated that the prognostication from comprehensive information based on GIS greatly improved the efficiency of metallogenic information extraction and integration. This method provides a kind of effective method and means for the prognostication for periphery and deep sites of resources crisis mine, and also promotes sustainable development of mine.

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    The study of metallogenic anomaly identification based on deep soil data with multifractal method—A case study of Cu element in Tongling ore clustering area.
    YUAN Feng LI Xiao-Hui BAI Xiao-Yu LI Xiu-Yu ZHANG Chen-Ye ZHOU Chao-Fa
    2009, 16(4): 335-343. 
    Abstract ( 1845 )   PDF (1627KB) ( 1246 )  

     In this paper, we take Cu element of Tongling ore clustering area as an example, and carry out the research on metallogenic anomaly identification with multifractal method, based on deep soil data. The results show that the Krigemultifractal interpolation method has tremendous advantage compared with the krige interpolation method when soil sampling density is relatively lower and spatial distribution of element content has little difference. For the kind of old ore clustering area, such as Tongling ore clustering area, which has a higher level of ore mining, and the spatial distribution of surface soil elements is mainly controlled by external pollution sources, the multifractal method that is based on deep soil data can identify anomalies efficiently and provide special services for deep and peripheral concealed ore prospecting in old ore clustering area. Moreover, for the blank researching area, multifractal method works the same way whether it is based on surface or deep soil data. For the multifractal method, there is still no standard being set up to determine the threshold anomaly of metallogenic prognosis by the soil elements. This paper presents a calculation method using the cumulative frequency of elemental contentsnumber of deposits. The anomaly area obtained by this method can well identify the most of known deposits. Meanwhile, by this method some blank abnormal areas which are worthwhile to do further anomaly inspection have been identified.

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    A study of the stable isotopes of the disperse elements(Ge, Cd, Tl).
    FAN Hai-Feng WEN Han-Cha HU Rui-Zhong ZHANG Hu-Xu
    2009, 16(4): 344-353. 
    Abstract ( 2398 )   PDF (1286KB) ( 1488 )  

    Recently, the nontraditional stable isotopic geochemistry has achieved great advancement in the study of the evolution of paleooceanic environment, in which the stable isotopes of redoxsensitive elements (Se,Mo,Fe,etc.) have played an important role. In comparison, the use of stable isotopes of some disperse elements (Ge,Cd,Tl) in tracing the paleooceanic environment was overlooked for years. But these elements have their own special recycling mechanism in the marine system, and thus, the trace of the stable isotopes of these elements may provide potential geological implications for the paleooceanic environment. Their sources and sinks are simple in the marine system; moreover, both inorganic and organic adsorption could control their isotopic fractionations. On the other hand, Ge, Cd and Tl are easily evaporated at high temperature, and their major isotopic fractionation may have occurred during the formation of the primary nebula. There are large scale lowtemperature deposit field in South China, which would provide the best chance to the improvement of Ge,Cd,Tl stable isotopes. In addition, Cd and Tl are the potential toxic elements in the supergene environment; therefore, their isotopic composition could be used to trace the source of contamination.

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    Analysis of soil physical and chemical properties by reflectance spectroscopy.
    JIA Hua-Ji JI Jun-Feng CHEN Jun LIAO Qi-Lin YANG Zhong-Fang
    2009, 16(4): 354-362. 
    Abstract ( 2472 )   PDF (1794KB) ( 1110 )  

     Soil reflectance spectroscopy within the visiblenearinfrared (VNIR) region (0.382.5 μm) contains much information of soil composition and their physical and chemical parameters. The determination of a soil reflectance spectrum is not only rapid, inexpensive but also nondestructive and environmental friendly, and moreover, the spatial distribution of soil reflectance information can be mapped by hyperspectral remote sensing. Based on the large quantities of soil samples acquired in the ecogeochemical survey of Jiangsu Province, we have related the soil ecogeochemical parameters, such as cation exchange capacity (CEC), organic matter, pH, ferric oxide, and contents of Al, Fe and Si, to the reflectance parameters of soil samples. The results indicate that the CEC of soil can be accurately predicted by first derivative (FD) values of soil reflectance spectra at 1400, 1900 and 2200 nm or by reflectance values directly at the shorter wavelengths (~400 nm). Soil organic matter, types of iron oxides, and contents of Al, Fe and Si can also be determined by their respective relevant wavelengths on the reflectance or FD spectra. Soil pH in Jiangsu was found to be highly correlated to FD values near 656 nm; however, this relationship showed a regional dependence, which may account for the nonlinear relationship between soil pH and reflectance parameters. The more complicated mechanisms relating to the relationship between soil pH and their reflectance parameters need to be further clarified.

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    Theory of accuracy assessment and methods for error correction in 3D geological structure models.
    SHU Liang-Feng TUN Shen-Cai BO Shen
    2009, 16(4): 363-371. 
    Abstract ( 2364 )   PDF (1269KB) ( 1120 )  

     Accuracy assessment and error correction of 3D geological models has become a bottleneck that restricted the development and application of 3D geological modeling. Based on the review of the present situation and development trends in 3D geological modeling, we introduced a general research framework for the accuracy assessment, error detection and dynamic correction in 3D geological structure modeling. To evaluate the accuracy of 3D geological structure models, we proposed to establish the general theoretical model, the practical operating model oriented to the given geologic body and the 3D distribution model of spatial uncertainty for geologic structure, respectively. The research should focus on the influence of geologic features and 3D modeling approaches on the accuracy of 3D geological models, should solve the accuracy assessment problem that induced by the interpolation error of the popular geologic surface and the extrapolation error of special geologic entity. Two approaches for error correction of 3D geological structure models, called the originaldatabased method and interimmodelbased method, are presented. To implement those approaches, the visual interactive technique of modeling data and 3D model was adopted. This research laid a foundation to build the theory and method system for accuracy assessment and error correction in 3D geological models, and also is helpful in improving the 3D modeling techniques under complicated geologic conditions.

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    A study of the outburst form of the endmoraine lake in Tibet.
    LIU Jing-Jing CHENG Zun-Lan LI Yong LUO Xi
    2009, 16(4): 372-380. 
    Abstract ( 1640 )   PDF (1890KB) ( 935 )  

    Many endmoraine lakes are distributed in Tibet. Once any of theses lakes outbursts, this region will undergo a huge loss. So studying the outburst mechanism is essential for forecast and assessment of the disaster. In this paper, the endmoraine dam is considered as a natural dam and the outburst of endmoraine lake is researched in terms of hydraulics and soil mechanics. According to field observations and previous researches, our study focuses on the overflow and pipingbreak types of outburst. It is found that the dyke breach in the overflow type usually has the shape of an arc or a trapezoid. From the field observations, we have found a relationship between the height and the open width of the breach. Almost all endmoraine lakes collapse partially. Based on field surveys and sampling analysis, we have determined the possible ways of collapse of the Guangxieco endmoraine lake by infiltration.

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    Integrity of debrisflow surge sequence.
    LI Yong LIU Jing-Jing SU Feng-Huan SU Feng-Cheng
    2009, 16(4): 381-388. 
    Abstract ( 1860 )   PDF (1177KB) ( 883 )  

    Debris flow, which is usually  of high density and viscosity, is conspicuous for its composition of successive surges of various properties. A debris flow is equal to a surge sequence and thus the surge sequence is believed to convey the information about the integrated properties of a system underlying debris flow. Based on observations in Jiangjia Gully, in this paper we focus on the integrity of surge sequence by considering the autocorrelation and tempospatial interval. The Hurst exponent is employed to express the autocorrelation. Results show that the Hurst exponents are exclusively bigger than 05, the value for random series without longrun aftereffects, suggesting the longrange correlation of the surge sequences. Furthermore, an eventspace is introduced by taking each surge as a point assigned with a parameter set. Three parameters, the discharge, velocity, and time interval are chosen to define a surge point. Then a debris flow event appears as a group of points clustered in a small range in the eventspace. This visualizes the concentration of surges in temporal and spatial dimensions, and further illustrates the tempospatial correlation of the surges. The integrity and autocorrelation of the surge sequence can be taken as the sign of an underlying dynamics of debris flow.

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     Bacterial molecular ecology in the groundwater contaminated by oil.
    HAO Chun-Bo WANG An-Cai DONG Jian-Nan ZHANG Qian CA Wu-Tian
    2009, 16(4): 389-400. 
    Abstract ( 2196 )   PDF (2142KB) ( 582 )  

    An oilcontaminated groundwater sample was collected at an abandoned petrochemical factory. Bacterial genome DNA was extracted for the 16S rDNA gene amplification, and then a bacterial 16S rDNA gene clone library was constructed. After the phylogenetic analysis of 16S rDNA sequences, bacterial diversity and community structure of the groundwater were studied. The results showed the bacteria in the groundwater could be divided into 11 groups, which were as follows:Betaproteobacteria(381%),Alphaproteobacteria(353%),Gamaproteobacteria(51%),Deltaroteobacteria(52%),Bacteroidetes(40%),Verrucomicrobia(25%),Epsilonproteobacteria(19%),Nitrospira(13%),Planctomycetes(13%),Candidate Division OD1(13%),Unclassified Bacteria(38%)。Betaproteobacteria and Alphaproteobacteria were predominant in the ecosystem, each of which accounted for over onethird of total clones. Hydrogenophaga and Sphingomonas are the most abundant degrading bacteria in the sample, which accounted for 381% and 353% of all bacteria respectively. Many clones also affiliated with other degrading bacteria, such as Sulfuricurvum kujiense, Trichlorobacter thiogenes, Rhodoferax ferrireducens and bacteria of genus Rhodobacter, Methylomonas, Nevskia. Besides, a lot of 16S rDNA sequences in the clone library had high similarity to the ones originated from similar polluted environments, such as groundwater contaminated with tar oil, groundwater contaminated with benzene, soil contaminated with crude oil, soil contaminated with methyl bromide and methyl chloride, antibiotics production wastewater and activated sludge, which proved that there were lots of degrading bacteria population in the oilcontaminated water. The components of petroleum contaminant have an important effect on community structure of degrading bacteria.

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