华南晚中生代陆弧迁移与海域盆地演化

doi:10.13745/j.esf.sf.2022.8.5

地学前缘 ›› 2022, Vol. 29 ›› Issue (6): 277-290.DOI: 10.13745/j.esf.sf.2022.8.5

• 原型盆地复原理论与方法 • 上一篇下一篇

华南晚中生代陆弧迁移与海域盆地演化

朱伟林¹(), 徐旭辉², 王斌³, 曹倩³, 陈春峰⁴, 高顺莉⁴, 冯凯龙¹, 付晓伟¹^,^*()

1.同济大学海洋地质国家重点实验室, 上海 200092
2.中国石化石油物探技术研究院, 江苏南京 211103
3.中国石油化工股份有限公司石油勘探开发研究院无锡石油地质研究所, 江苏无锡 214131
4.中海石油(中国)有限公司上海分公司, 上海 200030

收稿日期:2022-07-07 修回日期:2022-08-01 出版日期:2022-11-25 发布日期:2022-10-20
通信作者: 付晓伟
作者简介:朱伟林(1956—),男,教授,博士生导师,主要从事海域构造地质及石油地质研究。E-mail: zhuwl@tongji.edu.cn
基金资助:
国家自然科学基金项目(41702228);中国石油化工股份有限公司资助项目(P20027)

Late Mesozoic continental arc migration in southern China and its effects on the evolution of offshore forearc basins

ZHU Weilin¹(), XU Xuhui², WANG Bin³, CAO Qian³, CHEN Chunfeng⁴, GAO Shunli⁴, FENG Kailong¹, FU Xiaowei¹^,^*()

1. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
2. Sinopec Geophysical Research institute, Nanjing 211103, China
3. Wuxi Research Institute of Petroleum Geology, Sinopec, Wuxi 214131, China
4. CNOOC China Limited (Shanghai), Shanghai 200030, China

Received:2022-07-07 Revised:2022-08-01 Online:2022-11-25 Published:2022-10-20
Contact: FU Xiaowei

摘要/Abstract

摘要：

陆弧和弧前盆地是俯冲体系中具有密切联系的构造单元。中生代以来,华南受多期板块俯冲的控制,发育大规模岩浆岩带及海域广泛分布的弧前盆地。但陆域弧岩浆岩较少,海域又缺乏足够钻井,各时期陆弧的位置存在较大争议,同时,南海北部至东海一带弧前盆地也缺乏系统认识,因此,亟须新的研究思路深化对华南晚中生代俯冲体系和俯冲过程的认识。本文以前人研究为基础,对海域钻遇中生界的典型钻井进行了详细分析,系统开展了海域盆地区域构造和沉积对比,将弧前盆地发育与岛弧变迁相结合综合分析。结果表明早侏罗世—早白垩世陆弧位于南海北部—东海靠近陆域一侧,经历了早侏罗世局限陆弧、中晚侏罗世沿海陆弧带、早白垩世向海沟方向的迁移。在此过程中,华南海域弧前盆地群于中侏罗世正式形成,早白垩世发育盆缘角度不整合,粗碎屑相带向海沟方向迁移,晚白垩南海北部与东海各自进入新的构造体制,结束弧前盆地的发育。华南沿海海域中生代盆地的发育可为陆弧的展布提供重要约束,弧岩浆岩带的迁移控制了弧前盆地的演化。

关键词: 华南, 中生代, 弧前盆地, 陆弧, 俯冲体系

Abstract:

Forearc basins are closely linked to continental arcs in a subduction system. In southern China, widespread onshore magmatic belt and offshore forearc basins developed under multi-stage subduction since the Mesozoic. However, the arc migration pattern has been under hot debate, and the related forearc basins are little known because of limited offshore drilling and lack of access to onshore magmatic arc rock. Thus, new research designs are needed to observe the Late-Mesozoic subduction system/processes of southern China based on available data. In this paper, typical offshore wells containing Mesozoic layers are analyzed in detail; tectonics and sedimentation characteristics of offshore basins are systematically compared; and the development of forearc basins is analyzed in combination with the arc migration. Results show that the arc system extends roughly along the present-day coast of southern China from the Early Jurassic to Early Cretaceous: It mainly distributes in the southern East China Sea and extends to the northeastern South China Sea region in the Early Jurassic, then spreads widely southwards to the South China Sea in the Middle-Late Jurassic; since the Early Cretaceous it migrates eastward due to rollback of the subducted Paleo-Pacific slab. During this arc migration process, forearc basins are finally formed in the Middle Jurassic. And in response to the trenchward arc migration, angular unconformities in all forearc basins are formed and coarse clastic facies migrate trenchward in the Early Cretaceous. In the Late Cretaceous, the northern China Sea region is no longer in the subduction system and the forearc basin is replaced by regional unconformity; meanwhile, the East China Sea Basin becomes a backarc basin. Forearc basin evolution is primarily controlled by the migrating arc system, thus Mesozoic basins in the offshore South China Sea can provide important constraint on the regional arc migration pattern.

Key words: South China block, Mesozoic, forearc basin, continental arc, subduction system

中图分类号:

朱伟林, 徐旭辉, 王斌, 曹倩, 陈春峰, 高顺莉, 冯凯龙, 付晓伟. 华南晚中生代陆弧迁移与海域盆地演化[J]. 地学前缘, 2022, 29(6): 277-290.

ZHU Weilin, XU Xuhui, WANG Bin, CAO Qian, CHEN Chunfeng, GAO Shunli, FENG Kailong, FU Xiaowei. Late Mesozoic continental arc migration in southern China and its effects on the evolution of offshore forearc basins[J]. Earth Science Frontiers, 2022, 29(6): 277-290.

图/表 8

图1 区域位置及已发表岩浆岩数据(区域断裂据文献[11]修改;岩浆岩数据来源于文献[7,10,12⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓-30])

Fig.1 Simplified map showing regional faults and compiled ages of magmatic rocks. Adapted from [7,10⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓⇓-30].

图2 华南陆域及东海—南海北部海域中生代盆地综合对比图

Fig.2 Comparison of the onshore and offshore Mesozoic basins (blue shaded area) in southern China

图3 南海—台湾—东海—浙江中生代地层及沉积对比图 (石浦柱状图据文献[42]修改;MZ-1-1井据文献[40]修改;台湾地区柱状图据文献[39]修改;Sampaguita-1井据文献[43]修改)

Fig.3 Stratigraphic and sedimentary comparisons between wells for Mesozoic strata of the South China Sea-Taiwan-East China Sea-Zhejiang regions (well locations see insert map). Modified from [39-40,42-43].

图4 华南及沿海海域早侏罗世岛弧展布及岩相古地理图 (粤闽浙陆域岩相古地理据文献[50]修改)

Fig.4 Lithofacies paleogeographic sketch map of southern China showing the arc distribution pattern in the Early Jurassic. Basemap modified from [50].

图5 华南及沿海海域中晚侏罗世陆弧展布及岩相古地理图 (粤闽浙陆域内陆湖盆据文献[55]修改)

Fig.5 Lithofacies paleogeographic sketch map of southern China showing the arc distribution pattern in the Middle-Late Jurassic (onshore basin data from [55])

图6 华南及沿海海域早白垩世岛弧展布及岩相古地理图 (粤闽浙陆域内陆湖盆据文献[55]修改)

Fig.6 Lithofacies paleogeographic sketch map of southern China showing the arc distribution pattern in the Early Cretaceous (onshore basin data from [55])

图7 南海北部晚中生代构造-沉积演化模式图

Fig.7 Schematic diagrams showing the Late Mesozoic tectono-sedimentary evolution in the northern South China Sea

图8 东海南部晚中生代构造-沉积演化模式图

Fig.8 Schematic diagrams showing the Late Mesozoic tectono-sedimentary evolution in the southern East China Sea

参考文献 66

[1]	NODA A. Forearc basins: types, geometries, and relationships to subduction zone dynamics[J]. Geological Society of America Bulletin, 2016, 128(5/6): 879-895. DOI URL
[2]	LI Z X, LI X H. Formation of the 1 300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China: a flat-slab subduction model[J]. Geology, 2007, 35(2): 179-182. DOI URL
[3]	LI Z X, LI X H, CHUNG S L, et al. Magmatic switch-on and switch-off along the South China continental margin since the Permian: transition from an Andean-type to a western Pacific-type plate boundary[J]. Tectonophysics, 2012, 532/533/534/535: 271-290.
[4]	SUO Y, LI S, JIN C, et al. Eastward tectonic migration and transition of the Jurassic-Cretaceous Andean-type continental margin along Southeast China[J]. Earth-Science Reviews, 2019, 196: 102884. DOI URL
[5]	LI J, DONG S, CAWOOD P A, et al. An Andean-type retro-arc foreland system beneath Northwest South China revealed by sinoprobe profiling[J]. Earth and Planetary Science Letters, 2018, 490: 170-179. DOI URL
[6]	LI J, ZHANG Y, DONG S, et al. Cretaceous tectonic evolution of South China: a preliminary synthesis[J]. Earth-Science Reviews, 2014, 134: 98-136. DOI URL
[7]	WANG G C, JIANG Y H, LIU Z, et al. Multiple origins for the middle Jurassic to early Cretaceous high-K calc-alkaline I-type granites in northwestern Fujian province, SE China and tectonic implications[J]. Lithos, 2016, 246/247: 197-211. DOI URL
[8]	刘潜, 于津海, 苏斌, 等. 福建锦城187 Ma花岗岩的发现: 对华南沿海早侏罗世构造演化的制约[J]. 岩石学报, 2011, 27(12): 3575-3589.
[9]	ZHAO L, GUO F, ZHANG X, et al. Cretaceous crustal melting records of tectonic transition from subduction to slab rollback of the paleo-Pacific plate in SE China[J]. Lithos, 2021, 384/385: 105985. DOI URL
[10]	XU C, ZHANG L, SHI H, et al. Tracing an Early Jurassic magmatic arc from South to East China seas[J]. Tectonics, 2017, 36: 466-492. DOI URL
[11]	LIN S, XING G, DAVIS D W, et al. Appalachian-style multi-terrane Wilson cycle model for the assembly of South China[J]. Geology, 2018, 46: 319-322. DOI URL
[12]	XU C, SHI H, BARNES C G, et al. Tracing a Late Mesozoic magmatic arc along the Southeast Asian margin from the granitoids drilled from the northern South China Sea[J]. International Geology Review, 2016, 58: 71-94. DOI URL
[13]	LIU L, XU X, XIA Y. Asynchronizing paleo-Pacific slab rollback beneath SE China: insights from the episodic Late Mesozoic volcanism[J]. Gondwana Research, 2016, 37: 397-407. DOI URL
[14]	GUO C, CHEN Y, ZENG Z, et al. Petrogenesis of the Xihuashan granites in southeastern China: constraints from geochemistry and in-situ analyses of zircon U-Pb-Hf-O isotopes[J]. Lithos, 2012, 148: 209-227. DOI URL
[15]	CHEN J Y, YANG J H, ZHANG J H, et al. Geochemical transition shown by Cretaceous granitoids in southeastern China: implications for continental crustal reworking and growth[J]. Lithos, 2014, 196/197: 115-130. DOI URL
[16]	GUO F, FAN W, LI C, et al. Multi-stage crust-mantle interaction in SE China: temporal, thermal and compositional constraints from the Mesozoic felsic volcanic rocks in eastern Guangdong-Fujian provinces[J]. Lithos, 2012, 150: 62-84. DOI URL
[17]	CHEN J Y, YANG J H, ZHANG J H, et al. Petrogenesis of the Cretaceous Zhangzhou batholith in southeastern Vhina: zircon U-Pb age and Sr-Nd-Hf-O isotopic evidence[J]. Lithos, 2013, 162/163: 140-156. DOI URL
[18]	CHEN J Y, YANG J H, ZHANG J H. Origin of Cretaceous aluminous and peralkaline A-type granitoids in northeastern Fujian, coastal region of southeastern China[J]. Lithos, 2019, 340/341: 223-238. DOI URL
[19]	ZHU K Y, LI Z X, XU X S, et al. Early Mesozoic ferroan (A-type) and magnesian granitoids in eastern South China: tracing the influence of flat-slab subduction at the western Pacific margin[J]. Lithos, 2016, 240/241/242/243: 371-381.
[20]	LIU L, XU X, ZOU H. Episodic eruptions of the Late Mesozoic volcanic sequences in southeastern Zhejiang, SE China: petrogenesis and implications for the geodynamics of paleo-Pacific subduction[J]. Lithos, 2012, 154: 166-180. DOI URL
[21]	XIA Y, XU X S, ZHU K Y. Paleoproterozoic S- and A-type granites in southwestern Zhejiang: magmatism, metamorphism and implications for the crustal evolution of the Cathaysia basement[J]. Precambrian Research, 2012, 216/217/218/219: 177-207.
[22]	LIN J W, LEE C Y, CHEN C H, et al. Exotic origin of Pingtan island in the Pingtan-Dongshan metamorphic belt (SE China): zircon U-Pb age and Hf isotope evidences[J]. Lithos, 2020, 374/375: 105701. DOI URL
[23]	CHEN J Y, YANG J H, JI W Q. Ages and petrogenesis of Jurassic and Cretaceous intrusive rocks in the Matsu islands: implications for lower crust modification beneath southeastern China[J]. Journal of Asian Earth Sciences, 2017, 150: 14-24. DOI URL
[24]	YAN L L, HE Z Y, JAHN B M, et al. Formation of the Yandangshan volcanic-plutonic complex (SE China) by melt extraction and crystal accumulation[J]. Lithos, 2016, 266/267: 287-308. DOI URL
[25]	HE Z Y, XU X S, NIU Y. Petrogenesis and tectonic significance of a Mesozoic granite-syenite-gabbro association from inland South China[J]. Lithos, 2010, 119: 621-641. DOI URL
[26]	HUANG H Q, LI X H, LI Z X, et al. Intraplate crustal remelting as the genesis of Jurassic high-K granites in the coastal region of the Guangdong province, SE China[J]. Journal of Asian Earth Sciences, 2013, 74: 280-302. DOI URL
[27]	HUANG H Q, LI X H, LI Z X, et al. Formation of the Jurassic South China large granitic province: insights from the genesis of the Jiufeng pluton[J]. Chemical Geology, 2015, 401: 43-58. DOI URL
[28]	JIANG S H, BAGAS L, LIANG Q L. New insights into the petrogenesis of volcanic rocks in the Shanghang Basin in the Fujian province, China[J]. Journal of Asian Earth Sciences, 2015, 105: 48-67. DOI URL
[29]	LI B, JIANG S Y, ZHANG Q, et al. Geochemistry, geochronology and Sr-Nd-Pb-Hf isotopic compositions of Middle to Late Jurassic syenite-granodiorites-dacite in South China: petrogenesis and tectonic implications[J]. Gondwana Research, 2016, 35: 217-237. DOI URL
[30]	YUAN W, YANG Z, ZHAO X, et al. Early Jurassic granitoids from deep drill holes in the East China Sea Basin: implications for the initiation of palaeo-Pacific tectono-magmatic cycle[J]. International Geology Review, 2018, 60: 813-824. DOI URL
[31]	ZHU W, CUI Y, SHAO L, et al. Reinterpretation of the northern South China Sea pre-Cenozoic basement and geodynamic implications of the South China continent: constraints from combined geological and geophysical records[J]. Acta Oceanologica Sinica, 2021, 40: 13-28.
[32]	林鹤鸣, 张青林, 张向涛, 等. 南海北部潮汕坳陷mz-1井硅质岩放射虫组合、地球化学特征及构造古地理意义[J]. 石油学报, 2019, 40(S1): 188-196. DOI
[33]	张青林, 张航飞, 张向涛, 等. 南海北部潮汕坳陷上白垩统盆地原型及其大地构造背景分析[J]. 地球物理学报, 2018, 61(10): 4308-4321.
[34]	冯晓杰, 蔡东升, 王春修, 等. 东海陆架盆地中新生代构造演化特征[J]. 中国海上油气地质, 2003: 35-39.
[35]	杨长清, 杨传胜, 孙晶, 等. 东海陆架盆地南部中生代演化与动力学转换过程[J]. 吉林大学学报(地球科学版), 2019, 49(1): 139-153.
[36]	张勇, 姚永坚, 李学杰, 等. 中生代以来东亚洋陆汇聚带多圈层动力下的中国海及邻区构造演化及资源环境效应[J]. 中国地质, 2020, 47(5): 1271-1309.
[37]	YANG C, SUN J, YANG Y, et al. Key factors controlling Mesozoic hydrocarbon accumulation in the southern East China Sea basin[J]. Marine and Petroleum Geology, 2020, 118: 104436. DOI URL
[38]	王可德, 王建平, 徐国庆, 等. 东海陆架盆地西南部中生代地层的发现[J]. 地层学杂志, 2000, 24(2): 129-131.
[39]	周蒂. 台西南盆地和北港隆起的中生界及其沉积环境[J]. 热带海洋学报, 2002, 2: 50-57.
[40]	吴国瑄, 王汝建, 郝沪军, 等. 南海北部海相中生界发育的微体化石证据[J]. 海洋地质与第四纪地质, 2007, 27(1): 79-85.
[41]	张素芳, 张向涛, 张青林, 等. 南海北部白垩系发育特征及构造意义[J]. 海洋地质与第四纪地质, 2015, 35(6): 81-86.
[42]	王学寅, 胡文瑄, 胡广, 等. 浙江石浦下白垩统灰岩微相分析与锆石U-Pb年代学研究[J]. 地质论评, 2012, 58(4): 614-626.
[43]	TAYLOR B, HAYES D E. The tectonic evolution of the South China Basin. The tectonic and geologic evolution of Southeast Asian seas and islands[J]. Geophysical Monograph, 1980: 89-104.
[44]	胡文博. 东海陆架盆地南部中生界沉积体系研究[D]. 北京: 中国地质大学(北京), 2012.
[45]	邵磊, 尤洪庆, 郝沪军, 等. 南海东北部中生界岩石学特征及沉积环境[J]. 地质论评, 2007, 53(2): 164-169.
[46]	张金虎, 金春爽, 徐立明, 等. 福建黄塘晚侏罗世长林组硅质岩地球化学特征及其沉积环境意义[J]. 地学前缘, 2019, 12(3): 190-201.
[47]	SCHLÜTER H, HINZ K, BLOCK M J M G. Tectono-stratigraphic terranes and detachment faulting of the South China Sea and Sulu sea[J]. Marine Geology, 1996, 130: 39-78. DOI URL
[48]	HU G, HU W, CAO J, et al. Fluctuation of organic carbon isotopes of the Lower Cretaceous in coastal southeastern China: terrestrial response to the oceanic anoxic events (oae1b)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2014, 399: 352-362. DOI URL
[49]	王长势, 朱伟林, 钟锴, 等. 南海北部陆坡晚白垩世构造逆冲及其成因[J]. 地球科学: 中国地质大学学报, 2015, 40(9): 1505-1516.
[50]	马永生, 陈洪德, 王国力. 中国南方构造-层序岩相古地理图集[M]. 北京: 科学出版社, 2009.
[51]	CUI Y, SHAO L, LI Z X, et al. A Mesozoic Andean-type active continental margin along coastal South China: new geological records from the basement of the northern South China Sea[J]. Gondwana Research, 2021, 99: 36-52. DOI URL
[52]	刘凯, 徐维光, 叶海敏, 等. 华南中生代岩浆岩时空分布和迁移与古太平洋板块俯冲过程[J]. 矿物岩石地球化学通报, 2016, 35(6): 1141-1155.
[53]	杨宗永, 何斌. 华南侏罗纪构造体制转换: 碎屑锆石U-Pb年代学证据[J]. 大地构造与成矿学, 2013, 37(4): 580-591.
[54]	CUI J, ZHANG Y, DONG S, et al. Zircon U-Pb geochronology of the Mesozoic metamorphic rocks and granitoids in the coastal tectonic zone of SE China: constraints on the timing of late Mesozoic orogeny[J]. Journal of Asian Earth Sciences, 2013, 62: 237-252. DOI URL
[55]	ZHOU Z, MA C, XIE C, et al. Genesis of highly fractionated I-type granites from Fengshun complex: implications to tectonic evolutions of South China[J]. Journal of Earth Science, 2016, 27: 444-460. DOI URL
[56]	YUI T F, OKAMOTO K, USUKI T, et al. Late Triassic-Late Cretaceous accretion/subduction in the Taiwan region along the eastern margin of South China: evidence from zircon SHRIMP dating[J]. International Geology Review, 2009, 51: 304-328. DOI URL
[57]	付晓伟, 朱伟林, 陈春峰, 等. 丽水—椒江凹陷西斜坡明月峰组上段碎屑锆石物源[J]. 地球科学: 中国地质大学学报, 2015, 40(12): 1987-2001.
[58]	WEILIN Z, KAI Z, XIAOWEI F, et al. The formation and evolution of the East China Sea shelf basin: a new view[J]. Earth-Science Reviews, 2019, 190: 89-111. DOI URL
[59]	LI C F, ZHOU Z, GE H, et al. Rifting process of the Xihu Depression, East China Sea basin[J]. Tectonophysics, 2009, 472: 135-147. DOI URL
[60]	XU G Q, WU S H, ZHANG L, et al. Stratigraphic division and depositional processes for the Mesozoic basin in northern South China Sea[J]. Marine Geophysical Research, 2013, 34: 175-194. DOI URL
[61]	陈虹宇, 胡广, 胡文瑄, 等. 浙江石浦下白垩统石浦群沉积相、层序及相对海平面变化[J]. 沉积学报, 2018, 36(2): 243-256.
[62]	MÜLLER D R, SDROLIAS M, GAINA C, et al. Long-term sea-level fluctuations driven by ocean basin dynamics[J]. Science, 2008, 319(5868): 1357-1362. DOI PMID
[63]	NIU Y, LIU Y, XUE Q, et al. Exotic origin of the Chinese continental shelf: new insights into the tectonic evolution of the western Pacific and eastern China since the Mesozoic[J]. Science Bulletin, 2015, 60: 1598-1616. DOI URL
[64]	LI Y, MA C Q, XING G F, et al. The Early Cretaceous evolution of SE China: insights from the Changle-Nan'ao metamorphic belt[J]. Lithos, 2015, 230: 94-104. DOI URL
[65]	WEI X, DING W, CHRISTESON G L, et al. Mesozoic suture zone in the East China Sea: evidence from wide-angle seismic profiles[J]. Tectonophysics, 2021, 820: 229116. DOI URL
[66]	HALL R. Late Jurassic-Cenozoic reconstructions of the Indonesian region and the Indian ocean[J]. Tectonophysics, 2012, 570/571: 1-41. DOI URL

华南晚中生代陆弧迁移与海域盆地演化

Late Mesozoic continental arc migration in southern China and its effects on the evolution of offshore forearc basins

RichHTML

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

图/表 8

参考文献 66

相关文章 15

编辑推荐

Metrics

本文评价

[1]	张进江, 郑剑磊, 王海滨, 郭磊, 刘江, 戚国伟. 内蒙古大青山-盘羊山晚中生代-早新生代构造事件及其对华北北缘构造演化的启示[J]. 地学前缘, 2024, 31(1): 127-141.
[2]	任纪舜, 刘建辉, 朱俊宾. 中国东部中生代上叠造山系[J]. 地学前缘, 2024, 31(1): 142-153.
[3]	胡瑞忠, 高伟, 付山岭, 苏文超, 彭建堂, 毕献武. 华南中生代陆内成矿作用[J]. 地学前缘, 2024, 31(1): 226-238.
[4]	杨风丽, 徐铭辰, 庄圆, 赵西西, 胡虞杨, 杨瑞青. 古生代中国中西部三大陆块古地理位置重建与演变[J]. 地学前缘, 2022, 29(6): 265-276.
[5]	叶涛, 牛成民, 王德英, 王清斌, 代黎明, 陈安清. 渤海西南海域中生代构造演化、动力学机制及其对华北克拉通破坏的启示[J]. 地学前缘, 2022, 29(5): 133-146.
[6]	杨雅军, 杨晓平, 江斌, 汪岩, 庞雪娇. 大兴安岭中生代火山岩地层时空分布与蒙古—鄂霍茨克洋、古太平洋板块俯冲作用响应[J]. 地学前缘, 2022, 29(2): 115-131.
[7]	谢桂青, 毛景文, 张长青, 李伟, 宋世伟, 章荣清. 华南地区三叠纪矿床地质特征、成矿规律和矿床模型[J]. 地学前缘, 2021, 28(3): 252-270.
[8]	张志亮, 陈飞扬, 张志飞. 华南寒武纪碳酸盐岩中最早腕足动物的辐射、发育与分布[J]. 地学前缘, 2020, 27(6): 79-103.
[9]	沈阳, 王训练, 李玉坤, 杨志华, 岑武轩, 王雪兵. 黔南上司地区石炭系有孔虫:兼论华南维宪阶有孔虫生物地层序列[J]. 地学前缘, 2020, 27(6): 213-233.
[10]	陈国超, 裴先治, 李瑞保, 李佐臣, 裴磊, 刘成军, 陈有炘, 王盟, 高峰, 魏均启. 东昆仑造山带东段晚古生代—早中生代构造岩浆演化与成矿作用[J]. 地学前缘, 2020, 27(4): 33-48.
[11]	胡瑞忠, 陈伟, 毕献武, 付山岭, 尹润生, 肖加飞. 扬子克拉通前寒武纪基底对中生代大面积低温成矿的制约[J]. 地学前缘, 2020, 27(2): 137-150.
[12]	杜杨松, 曹毅, 秦新龙, 庞振山, 杜轶伦, 王功文. 皖赣沿江地区中生代壳幔相互作用与多成因夕卡岩成矿过程研究综述[J]. 地学前缘, 2020, 27(2): 165-181.
[13]	李刚, 蒋职权, 邵学峰, 高万里, 刘正宏. 医巫闾山中—晚侏罗世构造变形与同构造花岗岩的耦合关系[J]. 地学前缘, 2019, 26(2): 72-91.
[14]	朱弟成，王青，赵志丹，牛耀龄，侯增谦，潘桂棠，莫宣学. 大陆边缘弧岩浆成因与大陆地壳形成[J]. 地学前缘, 2018, 25(6): 67-77.
[15]	李细光，潘黎黎，李冰溯，聂冠军，吴教兵，陆俊宏，黎峻良，严小敏. 广西灵山断裂北段古地震事件初步研究[J]. 地学前缘, 2018, 25(4): 268-275.