Discussion on ore-controlling roles of structural system in hydrothermal metallogenic system

doi:10.13745/j.esf.sf.2023.11.65

Abstract

Abstract:

The structural system is the cornerstone of the geomechanics theory and methodology established by Prof. Li Siguang (J. S. Lee). This study begins with an exploration of the fundamental concept of the structural system, delving into its connotations to further develop and apply geomechanics theory and methodology based on the various interpretations and applications of the structural system in relevant literature, which provides a foundation for understanding the principles of crustal structure and movement, investigating the relationship between structure, diagenesis, and mineralization (reservoir formation), and guiding the exploration and evaluation of mineral resources.The study discusses the mechanical mechanisms of structural systems formed under the influence of principal compressive stress and the continuous effects of couples. Structural systems exhibit characteristics such as uniformity, regionality, hierarchy, inheritance, and complexity. It is proposed that structural types are hierarchical, while ore-forming structural systems possess distinct features, including consistency, periodicity, differentiation, diversity, and transformation. The ore-controlling rules of ore-forming structural systems are summarized and revealed. By examining the genetic relationship between ore-forming structural systems (ore-controlling structural types) and metallogenic systems, this study identifies key factors such as the regular distribution of ore-concentrated areas, ore fields, and ore deposits; the contemporaneity of structural deformation, magmatic activity, and mineralization; and the compositional consistency between ore-bearing structures and ores. These factors are used to define ore-forming structural systems and propose a research methodology for their study. This methodology provides a framework for prospecting predictions and deep exploration of ore deposits and ore bodies. To illustrate the ore-controlling roles and significance of ore-forming structural systems, this study examines two examples: the non-magmatic hydrothermal polymetallic metallogenic system (e.g., lead-zinc polymetallic deposits in the Sichuan-Yunnan-Guizhou metallogenic area) and the magmatic hydrothermal polymetallic metallogenic system (e.g., copper-tin polymetallic deposits in the Huangshaping-Baoshan ore field in southern Hunan).

Key words: ore-forming structural system, ore-controlling structural type, ore-controlling processes, orefield geomechanics, hydrothermal metallogenic system

CLC Number:

HAN Runsheng, LIU Fei, ZHANG Yan. Discussion on ore-controlling roles of structural system in hydrothermal metallogenic system[J]. Earth Science Frontiers, 2025, 32(2): 371-389.

Figures/Tables 13

Fig.1 Types of structural system. Adapted from [16].

Fig.2 Mechanical mechanism of structural system formed by the principal compressive stress effect (a) and the couple continuous effect (b). Adapted from [16].

Fig.3 Stress state and deformation process of rock stratum under continuous effect of the horizontal principal compressive stress. Adapted from [6,16].

Fig.4 Mechanical mechanism diagram of deformation process under continuous effect of the couple. Adapted from [6,16].

Fig.5 Distribution between deposits and structures in the Sichuan-Yunnan-Guizhou lead-zinc metallogenic area. Adapted from [34].

Fig.6 Fault-fold structure plan of typical deposits in the northeastern Yunnan lead-zinc metallogenic area. Adapted from [45].

Fig.7 Structural deformation period and its evolution in the Sichuan-Yunnan-Guizhou lead-zinc metallogenic area. Adapted from [36].

Fig.8 The combination type of fault-fold structure of typical deposits in the Sichuan-Yunnan-Guizhou lead-zinc metallogenic area. Adapted from [36].

Fig.9 The special chessboard structural type in the Wengkongba copper polymetallic deposit in the southwestern Yunnan. Adapted from [42].

Fig.10 Process and method of monographic study on ore-field (deposit) structure

Fig.11 The metallogenic geological model of rich-Ge lead-zinc deposit in the Sichuan-Yunnan-Guizhou lead-zinc metallogenic area. Adapted from [37].

Fig.12 The ore-field structural system and its evolution of the Huangshaping-Baoshan district. Adapted from [46].

Fig.13 The structural ore- and rock-controlling model of the Huangshaping copper-tin polymetallic deposit. Adapted from [46].

References 114

[1]	李四光. 地质力学概论[M]. 北京: 科学出版社, 1973: 1-131.
[2]	李四光. 旋扭构造[M]. 北京: 科学出版社, 1974: 1-83.
[3]	李四光. 地质力学方法[M]. 北京: 科学出版社, 1976: 1-206.
[4]	李四光. 地质力学概论[M]. 2版. 北京: 地质出版社, 1999: 1-228.
[5]	孙殿卿, 高庆华. 地质力学与地壳运动[M]. 北京: 地质出版社, 1982: 1-226.
[6]	李东旭, 周济元. 地质力学导论[M]. 北京: 地质出版社, 1986: 1-343.
[7]	马宗晋, 杜品仁. 现今地壳运动问题[M]. 北京: 地质出版社, 1995: 1-151.
[8]	高庆华. 地质力学的方法与实践: 第四篇(上) 地壳运动问题[M]. 北京: 地质出版社, 1996: 1-194.
[9]	邵云惠, 孙叶, 李成业, 等. 地质力学的方法与实践: 第五篇(下) 地质力学在环境地质中的应用[M]. 北京: 地质出版社, 1997: 1-199.
[10]	陈庆宣, 王维襄, 孙叶, 等. 地质力学的方法与实践: 第三篇岩石力学与构造应力场分析[M]. 北京: 地质出版社, 1998: 1-241.
[11]	刘迅. 地质力学的方法与实践: 第五篇(上) 地质力学在矿产资源勘查中的应用[M]. 北京: 地质出版社, 1998: 1-194.
[12]	王治顺, 朱大岗, 熊成云, 等. 地质力学的方法与实践: 第二篇构造体系各论(中国典型构造体系分论)[M]. 北京: 地质出版社, 1999: 1-194.
[13]	李东旭. 旋扭构造动力学:理论、方法及应用[M]. 北京: 地质出版社, 2003: 1-259.
[14]	王成金, 梁一鸿, 王义强. 现代地质力学[M]. 长春: 长春出版社, 2005: 1-357.
[15]	康玉柱, 赵越, 马寅生, 等. 油气地质力学[M]. 北京: 地质出版社, 2012: 1-191.
[16]	孙家骢, 韩润生. 矿田地质力学理论与方法[M]. 北京: 科学出版社, 2016: 1-356.
[17]	孙家骢. 云南省主要构造体系的成生发展及某些矿产的分布规律[J]. 云南地质, 1983, 2(1): 1-13.
[18]	翟裕生, 姚书振, 蔡克勤. 矿床学[M]. 3版. 北京: 地质出版社, 2011: 123-191.
[19]	GROVES D I, GOLDFARB R J, GEBRE-MARIAM M, et al. Orogenic gold deposits: a proposed classification in the context of their crustal distribution and relationship to other gold deposit types[J]. Ore Geology Reviews, 1998, 13(1/2/3/4/5): 7-27.
[20]	GROVES D I, SANTOSH M, GOLDFARB R J, et al. Structural geometry of orogenic gold deposits: Implications for exploration of world-class and giant deposits[J]. Geoscience Frontiers, 2018, 9(4): 1163-1177.
[21]	杨林, 王庆飞, 赵世宇, 等. 造山型金矿构造控矿作用[J]. 岩石学报, 2023, 39(2): 277-292.
[22]	LI N, YANG L Q, GROVES D I, et al. Tectonic and district to deposit-scale structural controls on the Ge’erke orogenic gold deposit within the Dashui-Zhongqu District, West Qinling Belt, China[J]. Ore Geology Reviews, 2020, 120: 103436.
[23]	DENG J, WANG Q F, LI G J, et al. Structural control and genesis of the Oligocene Zhenyuan orogenic gold deposit, SW China[J]. Ore Geology Reviews, 2015, 65: 42-54.
[24]	ALLIBONE A, BLAKEMORE H, GANE J, et al. Contrasting structural styles of orogenic gold deposits, reefton goldfield, New Zealand[J]. Economic Geology, 2018, 113(7): 1479-1497.
[25]	SAYAB M, MOLNÁR F, AERDEN D, et al. A succession of near-orthogonal horizontal tectonic shortenings in the Paleoproterozoic Central Lapland Greenstone Belt of Fennoscandia: constraints from the world-class Suurikuusikko gold deposit[J]. Mineralium Deposita, 2019, 55(8): 1605-1624.
[26]	陈衍景. 造山型矿床、成矿模式及找矿潜力[J]. 中国地质, 2006, 33(6): 1181-1196.
[27]	李华健, 王庆飞, 杨林, 等. 青藏高原碰撞造山背景造山型金矿床: 构造背景、地质及地球化学特征[J]. 岩石学报, 2017, 33(7): 2189-2201.
[28]	吕古贤, 郭涛, 舒斌, 等. 胶东金矿集中区构造体系多层次控矿规律研究[J]. 大地构造与成矿学, 2007, 31(2): 193-204.
[29]	刘迅. 关于构造体系控矿的若干地球化学问题[J]. 中国地质科学院院报, 1988, 9: 33-47.
[30]	韩润生, 马德云, 刘丛强, 等. 陕西铜厂矿田构造成矿动力学[M]. 昆明: 云南科技出版社, 2003: 105-109.
[31]	HAN R S, WANG L, MA D Y, et al. “Giant pressure shadow” structure and ore-finding method of tectonic stress field in the Tongchang Cu-Au polymetallic orefield, Shaanxi, China: II. Dynamics of tectonic ore-forming processes and prognosis of concealed ores[J]. Chinese Journal of Geochemistry, 2010, 29(4): 455-463.
[32]	翟裕生, 林新多. 矿田构造学[M]. 北京: 地质出版社, 1993: 1-214.
[33]	陈宣华, 陈正乐, 杨农. 区域成矿与矿田构造研究: 构建成矿构造体系[J]. 地质力学学报, 2009, 15(1): 1-19.
[34]	柳贺昌, 林文达. 滇东北铅锌银矿床规律研究[M]. 昆明: 云南大学出版社, 1999: 1-468.
[35]	韩润生, 王峰, 胡煜昭, 等. 会泽型(HZT)富锗银铅锌矿床成矿构造动力学研究及年代学约束[J]. 大地构造与成矿学, 2014, 38(4): 758-771.
[36]	韩润生, 张艳, 王峰, 等. 滇东北矿集区富锗铅锌矿床成矿机制与隐伏矿定位预测[M]. 北京: 科学出版社, 2019: 1-510.
[37]	韩润生, 吴鹏, 张艳, 等. 西南特提斯川滇黔成矿区富锗铅锌矿床成矿理论研究新进展[J]. 地质学报, 2022, 96(2): 554-573.
[38]	韩润生, 陈进, 黄智龙, 等. 构造成矿动力学及隐伏矿定位预测:以云南会泽超大型铅锌(银、锗)矿床为例[M]. 北京: 科学出版社, 2006: 1-200.
[39]	韩润生, 刘丛强, 黄智龙, 等. 论云南会泽富铅锌矿床成矿模式[J]. 矿物学报, 2001, 21(4): 674-680.
[40]	韩润生, 孙家骢, 李俊, 等. 易门铜矿“镜面对称” 成矿及意义[J]. 地质力学学报, 1999, 5(2): 77-82.
[41]	韩润生, 赵冻. 初论岩浆热液成矿系统控岩控矿构造深延格局研究方法[J]. 地学前缘, 2022, 29(5): 420-437. DOI
[42]	田映天, 韩润生, 刘飞, 等. 滇西南翁孔坝铜多金属矿床构造控矿模式[J]. 昆明理工大学学报(自然科学版), 2023, 48 (5): 50-65.
[43]	孙岩, 徐士进, 刘德良, 等. 断裂构造地球化学导论[M]. 北京: 科学出版社, 1998: 171-176.
[44]	韩润生, 刘丛强, 黄智龙, 等. 云南会泽铅锌矿床构造控矿及断裂构造岩稀土元素组成特征[J]. 矿物岩石, 2000, 20(4): 11-18.
[45]	韩润生, 胡煜昭, 王学琨, 等. 滇东北富锗银铅锌多金属矿集区矿床模型[J]. 地质学报, 2012, 86(2): 280-294.
[46]	韩润生, 赵冻, 吴鹏, 等. 湘南黄沙坪铜锡多金属矿床构造控岩控矿机制及深部找矿勘查启示[J]. 地学前缘, 2020, 27(4): 199-218. DOI
[47]	PIQUER J, SKARMETA J, COOKE D R. Structural evolution of the Rio Blanco-Los Bronces district, Andes of central Chile: controls on stratigraphy, magmatism, and mineralization[J]. Economic Geology, 2015, 110(8): 1995-2023.
[48]	翟裕生. 关于构造-流体-成矿作用研究的几个问题[J]. 地学前缘, 1996, 3(4): 230-236.
[49]	邓军, 杨立强, 翟裕生, 等. 构造-流体-成矿系统及其动力学的理论格架与方法体系[J]. 地球科学, 2000, 25(1): 71-78.
[50]	谭凯旋, 谢焱石, 郭定良. 构造-流体-成矿体系的耦合动力学: 以湘西金矿为例[J]. 矿物岩石地球化学通报, 2000, 19(4): 241-243.
[51]	谢焱石, 谭凯旋, 郝涛. 构造-流体-成矿作用的分形与混沌动力学[J]. 大地构造与成矿学, 2010, 34(3): 378-385.
[52]	和中华, 周云满, 和文言, 等. 滇西北衙超大型金多金属矿床成因类型及成矿规律[J]. 矿床地质, 2013, 32(2): 244-258.
[53]	刘飞, 王雷, 韩润生, 等. 滇西北北衙斑岩型金多金属矿田构造体系及其控矿作用[J]. 地学前缘, 2017, 24(6): 208-224. DOI
[54]	刘飞, 韩润生, 王雷, 等. 滇西北北衙斑岩型金多金属矿床万硐山矿段构造控岩控矿作用机制[J]. 大地构造与成矿学, 2016, 40(2): 266-280.
[55]	周云满, 张长青, 和中华, 等. 滇西北衙金多金属矿床成矿作用特征标志[J]. 地质找矿论丛, 2018, 33(1): 1-14.
[56]	周云满, 周癸武, 张长青, 等. 滇西北衙金多金属矿床成矿构造特征及地质勘查意义[J]. 大地构造与成矿学, 2021, 45(2): 308-326.
[57]	HE W Y, YANG L Q, BRUGGER J, et al. Hydrothermal evolution and ore genesis of the Beiya giant Au polymetallic deposit, western Yunnan, China: evidence from fluid inclusions and H-O-S-Pb isotopes[J]. Ore Geology Reviews, 2017, 90: 847-862.
[58]	MAO J W, ZHOU Y M, LIU H, et al. Metallogenic setting and ore genetic model for the Beiya porphyry-skarn polymetallic Au orefield, Western Yunnan, China[J]. Ore Geology Reviews, 2017, 86: 21-34.
[59]	汪礼明, 郭兰萱, 王涌泉, 等. 广东凡口铅锌矿床逆冲推覆构造体系: 地质特征、演化序列及控矿作用[J]. 大地构造与成矿学, 2022, 46(6): 1218-1228.
[60]	朱恩异, 王雷, 任涛, 等. 湘南长城岭矿区塘下垄花岗斑岩地球化学、锆石U-Pb年代学及Hf同位素特征[J]. 大地构造与成矿学, 2022, 46(6): 1200-1217.
[61]	李厚民, 李立兴, 余金杰, 等. 湘南地区钨锡多金属矿床矿石矿物组合、矿化蚀变特征及成矿流体组成[J]. 地质学报, 2021, 95(10): 3127-3145.
[62]	赵冻, 韩润生, 刘飞, 等. 湘南多金属矿集区岩浆热液成矿作用研究进展[J]. 大地构造与成矿学, 2023, 47(2): 337-360.
[63]	HOU Z Q, MA H W, ZAW K, et al. The Himalayan Yulong porphyry copper belt: product of large-scale strike-slip faulting in Eastern Tibet[J]. Economic Geology, 2003, 98(1): 125-145.
[64]	RICHARDS J P, BOYCE A J, PRINGLE M S. Geologic evolution of the Escondida area, Northern Chile: a model for spatial and temporal localization of porphyry Cu mineralization[J]. Economic Geology, 2001, 96(2): 271-305.
[65]	RICHARDS J P. Tectono-magmatic precursors for porphyry Cu-(Mo-Au) deposit formation[J]. Economic Geology, 2003, 98(8): 1515-1533.
[66]	SIRON C R, RHYS D, THOMPSON J F H, et al. Structural controls on porphyry Au-Cu and Au-rich polymetallic carbonate-hosted replacement deposits of the Kassandra mining district, Northern Greece[J]. Economic Geology, 2018, 113(2): 309-345.
[67]	TOSDAL R M, RICHARDS J P. Magmatic and structural controls on the development of porphyry Cu ± Mo ± Au deposits[M]. Society of Economic Geologists Reviews, Chapter 6, Littleton: Society of Economic Geologists, 2001, 14: 157-181.
[68]	JOSE P, PABLO S A, PAMELA P F. A new model for the optimal structural context for giant porphyry copper deposit formation[J]. Geology, 2021, 49(5): 597-601.
[69]	陈华勇, 吴超. 俯冲带斑岩铜矿系统成矿机理与主要挑战[J]. 中国科学: 地球科学, 2020, 50(7): 865-886.
[70]	陈国达. 成矿构造研究法[M]. 北京: 地质出版社, 1985: 1-413.
[71]	韩润生, 张艳, 任涛, 等. 碳酸盐岩容矿的非岩浆后生热液型铅锌矿床研究综述[J]. 昆明理工大学学报(自然科学版), 2020, 45(4): 29-40.
[72]	黄智龙, 陈进, 韩润生, 等. 云南会泽超大型铅锌矿床地球化学及成因: 兼论峨眉山玄武岩与铅锌成矿的关系[M]. 北京: 地质出版社, 2004: 1-187.
[73]	李文博, 黄智龙, 陈进, 等. 云南会泽超大型铅锌矿床硫同位素和稀土元素地球化学研究[J]. 地质学报, 2004, 78(4): 507-518.
[74]	张长青, 毛景文, 吴锁平, 等. 川滇黔地区MVT铅锌矿床分布、特征及成因[J]. 矿床地质, 2005, 24(3): 336-348.
[75]	许典葵, 黄智龙, 邓红, 等. 云南会泽超大型铅锌矿床的矿床模型[J]. 矿物学报, 2009, 29(2): 235-242.
[76]	张艳, 韩润生, 魏平堂, 等. 云南会泽矿山厂铅锌矿床流体包裹体特征及成矿物理化学条件[J]. 吉林大学学报(地球科学版), 2017, 47(3): 719-733.
[77]	HAN R S, LIU C Q, HUANG Z L, et al. Geological features and origin of the Huize carbonate-hosted Zn-Pb-(Ag)district, Yunnan, South China[J]. Ore Geology Reviews, 2007, 31(1/2/3/4): 360-383.
[78]	陈进. 麒麟厂铅锌硫化矿矿床成因及成矿模式探讨[J]. 有色金属矿产与勘查, 1993(2): 85-90.
[79]	廖文. 滇东、黔西铅锌金属区硫、铅同位素组成特征与成矿模式探讨[J]. 地质与勘探, 1984, 20(1): 2-6.
[80]	陈士杰. 黔西滇东北铅锌矿成因探讨[J]. 贵州地质, 1986, 3(3): 211-222.
[81]	张位及. 试论滇东北铅锌矿床的沉积成因和成矿规律[J]. 地质与勘探, 1984, 20(7): 11-16.
[82]	赵准. 滇东、滇东北地区铅锌矿床的成矿模式[J]. 云南地质, 1995, 14(4): 350-354.
[83]	柳贺昌. 滇、川、黔铅锌成矿区的构造控矿[J]. 云南地质, 1995, 14(3): 173-189.
[84]	周朝宪, 魏春生, 叶造军. 密西西比河谷型铅锌矿床[J]. 地质地球化学, 1997(1): 65-75.
[85]	崔峻豪, 韩润生, 王加昇, 等. 滇东北乐红铅锌矿床构造成生发展及其控矿作用[J]. 大地构造与成矿学, 2018, 42(4): 664-680.
[86]	韩润生, 王明志, 金中国, 等. 黔西北铅锌多金属矿集区成矿构造体系及其控矿机制[J]. 地质学报, 2020, 94(3): 850-868.
[87]	何志威, 李泽琴, 陈军, 等. 黔西北铅锌矿床成矿岩性组合与构造控矿样式[J]. 矿物学报, 2020, 40(4): 367-375.
[88]	金中国, 黄智龙, 郑明泓, 等. 贵州碳酸盐岩型铅锌矿床地质特征与容矿机理[J]. 矿物学报, 2020, 40(4): 346-355.
[89]	李波, 杨懿霆, 韩润生, 等. 黔西北小河边铁多金属矿床构造特征与找矿预测[J]. 矿物学报, 2020, 40(4): 483-501.
[90]	吕豫辉, 韩润生, 任涛, 等. 滇东北矿集区云南富乐厂铅锌矿区断裂构造控矿特征及其与成矿的关系[J]. 现代地质, 2015, 29(3): 563-575.
[91]	宋丹辉, 韩润生, 王峰, 等. 黔西北青山铅锌矿床构造控矿机理及其对深部找矿的启示[J]. 中国地质, 2024, 51(2): 399-425.
[92]	王健, 张均, 张晓军, 等. 四川天宝山矿床闪锌矿Rb-Sr年代学、稳定同位素及地质意义[J]. 地球科学, 2019, 44(9): 3026-3041.
[93]	王亮, 张嘉玮, 向坤鹏, 等. 黔西北地区地球物理特征与铅锌矿控矿构造分析[J]. 现代地质, 2019, 33(2): 325-336.
[94]	王明志, 韩润生, 周威, 等. 黔西北矿集区亮岩铅锌矿区成矿构造解析[J]. 地质力学学报, 2019, 25(2): 187-197.
[95]	王明志, 韩润生, 张艳. 成矿构造体系对铅锌成矿系统的控制作用: 以会泽富锗铅锌矿床为例[J]. 地质学报, 2020, 94(10): 3008-3023.
[96]	吴建标, 韩润生, 冯志兴, 等. 川西南大梁子铅锌矿区F15主控断裂及其控矿作用机制[J]. 地质通报, 2022, 41(10): 1869-1886.
[97]	HAN R S, WU J B, ZHANG Y, et al. Oblique distribution patterns and the underlying mechanical model of orebody groups controlled by structures at different scales[J]. Scientific reports, 2024, 14: 4591. DOI PMID
[98]	赵冻, 韩润生, 王加昇, 等. 滇东北矿集区小河铅锌矿床构造解析及其控矿模式[J]. 地质力学学报, 2020, 26(3): 345-362.
[99]	HAN R S, LIU C Q, CARRANZA E J M, et al. REE geochemistry of altered tectonites in the Huize base-metal district, Yunnan, China[J]. Geochemistry: Exploration, Environment, Analysis, 2012, 12(2): 127-146.
[100]	HAN R S, CHEN J, WANG F, et al. Analysis of metal-element association halos within fault zones for the exploration of concealed ore-bodies: a case study of the Qilinchang Zn-Pb-(Ag-Ge) deposit in the Huize mine district, Northeastern Yunnan, China[J]. Journal of Geochemical Exploration, 2015, 159: 62-78.
[101]	高妍, 郑声宇. 韩润生: 10年磨一剑, 向地球深部去[J]. 科技创新与品牌, 2019(7): 52-56.
[102]	马丽艳, 路远发, 屈文俊, 等. 湖南黄沙坪铅锌多金属矿床的Re-Os同位素等时线年龄及其地质意义[J]. 矿床地质, 2007, 26(4): 425-431.
[103]	姚军明, 华仁民, 屈文俊, 等. 湘南黄沙坪铅锌钨钼多金属矿床辉钼矿的Re-Os同位素定年及其意义[J]. 中国科学(D辑: 地球科学), 2007, 37(4): 471-477.
[104]	LI H, WATANABE K, YONEZU K. Zircon morphology, geochronology and trace element geochemistry of the granites from the Huangshaping polymetallic deposit, South China: implications for the magmatic evolution and mineralization processes[J]. Ore Geology Reviews, 2014, 60: 14-35.
[105]	LI D F, TAN C Y, MIAO F Y, et al. Initiation of Zn-Pb mineralization in the Pingbao Pb-Zn skarn district, South China: constraints from U-Pb dating of grossular-rich garnet[J]. Ore Geology Reviews, 2019, 107: 587-599.
[106]	李石锦. 湖南黄沙坪铅锌矿多金属矿床构造控矿特征及成矿浅析[J]. 大地构造与成矿学, 1997, 21(4): 339-346.
[107]	舒良树, 周新民, 邓平, 等. 南岭构造带的基本地质特征[J]. 地质论评, 2006, 52(2): 251-265.
[108]	柏道远, 马铁球, 王先辉, 等. 南岭中段中生代构造-岩浆活动与成矿作用研究进展[J]. 中国地质, 2008, 35(3): 436-455.
[109]	祝新友, 王京彬, 张志, 等. 湖南黄沙坪铅锌矿NNW向构造的识别及其找矿意义[J]. 地质与勘探, 2010, 46(4): 609-615.
[110]	周永章, 李兴远, 郑义, 等. 钦杭结合带成矿地质背景及成矿规律[J]. 岩石学报, 2017, 33(3): 667-681.
[111]	付雨昕, 赵冻, 韩润生. 湘南黄沙坪—宝山矿田构造应力场控矿规律及找矿方向分析[J]. 有色金属(矿山部分), 2022, 74(5): 173-188.
[112]	雷镇, 陶思源, 李波, 等. 湘南黄沙坪铜多金属矿床-256 m中段构造地球化学特征及找矿预测[J]. 中国有色金属学报, 2022, 32(9): 2835-2855.
[113]	文一卓, 孟雨红, 许以明, 等. 湖南首个固体矿产勘查3000 m科学深钻选址研究[J]. 地质与勘探, 2022, 58(5): 975-988.
[114]	沈宏飞, 李厚民, 余金杰, 等. 湘南地区钨锡多金属矿床浆液过渡态熔体类型成因联系及其成矿意义[J]. 地质学报, 2023, 97(1): 109-123.