Metallogenic characteristics and regularities of Hengyang Basin and its surrounding areas
LIU Xingzhong1, QIN Jinhua2, WANG Denghong2, FAN Zichun3, YANG Xiaofei3
1. Bayingolin Geological Branch, Geological Bureau of Xinjiang Uygur Autonomomous Region, Xinjiang Korla, 841000, China; 2. MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Naturals Resources, Chinese Academy of Geological Sciences, Beijing, 100037; 3. Zhicun Lithium Group Co., Ltd., Jiangxi Yichun 336000, China
Abstract：Hengyang Basin is located at the junction between Jiangxi- Hunan-Guangxi-Guangdong fold belt of South China fold system and Jiangnan platform uplift, with the development of multi-stages and multi-types metallic and non-metallic deposits. The systematic summarization of regional metallogenic regularities is deficient in current research, which hinders the establishment of metallogenic theory and ore prospecting. The authors in this paper summarized and analyzed the characteristics of magmatism and metallogenesis, temporal and spatial distribution of Hengyang Basin. The results show that multi-stage magmatism and mineralization were developed since Paleozoic, mainly in Indosinian and Yanshanian Period. Most of the main metal deposits in the basin are closely related to magmatism, and the mineralization types developed from high temperature to low temperature exist. The spatial distribution of rock mass and deposits in the basin is closely related with the deep-seated fractures, and various types of vertical zoning are developed in each deposit. Three different types of mineralized assemblage zones are developed in the basin from northwest to southeast, with mineralization temperature rising gradually. The Hengyang type basin and range structural belt are mainly controlled by the effect of lower mantle plume activities under the tectonic setting of multi-stage lithospheric extension in South China. The diagenesis and metallogenic activities are triggered by the superposition of multiple process, including partial melting and fractional crystallization in different locations of the lithosphere, upwelling of deep fertile ore fluid and the extraction of metals from surrounding rocks. The research results could provide some references for the study of metallogenic regularity and further prospecting in Meso-Cenozoic basins in South China.
[1] Gilder S A,Gill J,Coe R S,et al.Isotopic and paleomagnetic constraints on the mesozoic tectonic evolution of South China[J].Journal of Geophysical Research:Solid Earth,1996,101(B7):16137-16154. [2] 毛景文,谢桂青,郭春丽,等.南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景[J].岩石学报,2007,23(10):2329-2338. Mao J W,Xie G Q,Guo C L,et al.Large-scale tungsten-tin mineralization in the Nanling region,South China:metallogenic ages and corresponding geodynamic processes[J].Acta Petrologica Sinica,2007,23(10):2329-2338. [3] 毛景文,陈懋弘,袁顺达,等.华南地区钦杭成矿带地质特征和矿床时空分布规律[J].地质学报,2011,85(5):636-658. Mao J W,Chen M H,Yuan S D,et al.Geological characteristics of the Qinhang (or Shihang) metallogenic belt in South China and spatial-temporal distribution regularity of mineral deposits[J].Acta Geologica Sinica,2011,85(5):636-658. [4] 杨明桂,梅勇文.钦—杭古板块结合带与成矿带的主要特征[J].华南地质与矿产,1997,14(3):52-59. Yang M G,Mei Y W.Characteristics of geology and Metatllization in the Qinzhou-Hangzhou Paleoplate juncture[J].Geology and Mineral Resources of South China,1997,14(3):52-59. [5] 杨明桂,黄水保,楼法生,等.中国东南陆区岩石圈结构与大规模成矿作用[J].中国地质,2009,36(3):528-543. Yang M G,Huang S B,Lou F S,et al.Lithospheric structure and large-scale metallogenic process in southeast China continental area[J].Geology in China,2009,36(3):528-543. [6] 龙国中,王积廉.衡阳盆地盐类矿床地质特征与矿床成因[J].湖南地质,1994,13(1):22-24. Long G Z,Wang J L.Geologic properties and origin of salt deposits in Hengyang basin[J].Hunan Geology,1994,13(1):22-24. [7] 李福顺. 钦杭成矿带衡阳盆地找矿方向及前景分析[J].华南地质与矿产,2012,28(4):360-368. Li F S.Analysis on prospecting direction and potential of Hengyang basin in Qinzhou-Hangcheng Metallogenic belt[J].Geology and Mineral Resources of South China,2012,28(4):360-368. [8] 李竹溢.衡阳盆地Cu-Pb-Zn矿床成矿系列探讨[J].世界有色金属,2017,42(9):132,134. Li Z Y.Discussion on Metallogenic series of Cu-Pb-Zn deposit in Hengyang basin[J].World Nonferrous Metals,2017,42(9):132,134. [9] 秦锦华,王登红,陈毓川,等.试论湖南衡阳盆地与地幔柱的关系及其对关键矿产深部探测的意义[J].地质学报,2019,93(6):1501-1513. Qin J H,Wang D H,Chen Y C,et al.Discussion on the relationship between Hengyang basin and mantle plume and its implication for the deep prospecting of key minerals[J].Acta Geologica Sinica,2019,93(6):1501-1513. [10] 潘桂棠,肖庆辉,陆松年,等.中国大地构造单元划分[J].中国地质,2009,36(1):1-28. Pan G T,Xiao Q H,Lu S N,et al.Subdivision of tectonic units in China[J].Geology in China,2009,36(1):1-28. [11] 徐志刚,陈毓川,王登红,等.中国成矿区带划分方案[M].北京:地质出版社,2008:59-70. Xu Z G,Chen Y C,Wang D H,et al.The Scheme of the Classification of the Minerogenetic Units in China[M].Beijing:Geology Press,2008:59-70. [12] 孟立丰. 华南中生代构造深化特征——来自沉积盆地的研究证据[D].杭州:浙江大学,2012. Meng L F.Mesozoic Tectonic Evolution of the Southeast China Block:A Study from Mesozoic Basins[D].Hangzhou:Zhejiang University,2012. [13] 肖文舟,匡文龙,李雪宇,等.湖南衡阳清水塘矿区断裂构造控矿特征[J].地质学刊,2016,40(1):97-106. Xiao W Z,Kuang W L,Li X Y,et al.Ore-control characteristics of the fault structures in the Qingshuitang ore district of Hengyang,Hunan Province[J].Journal of Geology,2016,40(1):97-106. [14] 梁新权,郭定良.湖南深部构造活化及其浅部响应[J].地质科学,2002,37(3):332-342. Liang X Q,Guo D L.Deep tectonic activation and its shallow response in Hunan province[J].Chinese Journal of Geology,2002,37(3):332-342. [15] 张用夏. 华南地区环形构造及其成因[J].地质论评,1984,30(5):437-445. Zhang Y X.Ring structures and their genetic mechanism in the South China region[J].Geological Review,1984,30(5):437-445. [16] 王敏,王雨豪,赵亚娟,等.衡阳盆地与周边重力异常的分析[J].国土资源导刊,2015,12(4):30-34,39. Wang M,Wang Y H,Zhao Y J,et al.Analysis of gravity anomalies in Hengyang basin and its surrounding[J].Land & Resources Herald,2015,12(4):30-34,39. [17] 柏道远,周亮,王先辉,等.湘东南燕山早期钨锡与铅锌多金属矿床组合形成的构造-岩浆动力学机制[J].地质学报,2007,81(9):1238-1247. Bai D Y,Zhou L,Wang X H,et al.Tectonic-magmatic mechanisms of the two types of early Yanshanian W-Sn polymetallic and Pb-Zn-polymetallic deposit assemblages in southeast Hunan[J].Acta Geologica Sinica,2007,81(9):1238-1247. [18] 涂登峰. 湖南双江口—将军庙萤石矿床矿物中包裹体研究[J].地球化学,1987,16(3):274-279. Tu D F.Studies of inclusions in fluorite from the Shuangjiangkuo-Jiangjunmiao fluorite ore deposit in Hunan province[J].Geochimica,1987,16(3):274-279. [19] 赵增霞,徐兆文,左昌虎,等.湖南桂阳大义山南体(太坪山单元)花岗岩形成时代及物质来源探讨[J].地质论评,2017,63(2):395-412. Zhao Z X,Xu Z W,Zuo C H,et al.Emplacement time and material source of the southern Dayishan granitic batholith (Taipingshan body),Guiyang City,Hunan Province[J].Geological Review,2017,63(2):395-412. [20] Zhao Z X,Miao B H,Xu Z W,et al.2017.Petrogenesis of two types of late Triassic granite from the Guandimiao complex,southern Hunan Province,China[J].Lithos,282-283:403-419. [21] 缪柏虎,左昌虎,赵增霞,等.祁东县清水塘矿区周家岭花岗岩形成时代及物质来源[J].地质论评,2014,60(3):611-623. Miao B H,Zuo C H,Zhao Z X,et al.Forming age and material source of the Zhoujialing granite in Qingshuitang orefield,Qidong County,Hunan Province[J].Geological Review,2014,60(3):611-623. [22] 鲁玉龙,彭建堂,阳杰华,等.湘中紫云山岩体的成因:锆石U-Pb年代学、元素地球化学及Hf-O同位素制约[J].岩石学报,2017,33(6):1705-1728. Lu Y L,Peng J T,Yang J H,et al.Petrogenesis of the Ziyunshan pluton in central Hunan,South China:Constraints from zircon U-Pb dating,element geochemistry and Hf-O isotopes[J].Acta Petrologica Sinica,2017,33(6):1705-1728. [23] 陈卫锋,陈培荣,周新民,等.湖南阳明山岩体的LA-ICP-MS锆石U-Pb定年及成因研究[J].地质学报,2006,80(7):1065-1077. Chen W F,Chen P R,Zhou X M,et al.Single-zircon La-ICP-MS U-Pb dating of the Yangmingshan granitic pluton in Hunan,South China and its petrogenetic study[J].Acta Geologica Sinica,2006,80(7):1065-1077. [24] 马丽艳,刘树生,付建明,等.湖南塔山、阳明山花岗岩的岩石成因:来自锆石U-Pb年龄、地球化学及Sr-Nd同位素证据[J].地质学报,2016,90(2):284-303. Ma L Y,Liu S S,Fu J M,et al.Petrogenesis of the Tashan-Yangmingshan granitic batholiths:Constraint from zircon U-Pb age,geochemistry and Sr-Nd isotopes[J].Acta Geologica Sinica,2016,90(2):284-303. [25] 郭爱民,陈必河,陈剑锋,等.湖南塔山花岗岩SHRIMP锆石U-Pb年龄及其地质意义[J].地质通报,2017,36(2/3):459-465. Guo A M,Chen B H,Chen J F,et al.SHRIMP zircon U-Pb age of Tashan granitic pluton from Hu'nan Province and its geological significance[J].Geological Bulletin of China,2017,36(2/3):459-465. [26] 黄金川,彭建堂,阳杰华,等.湖南水口山花岗闪长岩的地球化学特征及成因[J].地球化学,2015,44(2):131-144. Huang J C,Peng J T,Yang J H,et al.Geochemistry and genesis of the Shuikoushan granodiorite in Hunan,South China[J].Geochimica,2015,44(2):131-144. [27] 左昌虎,路睿,赵增霞,等.湖南常宁水口山Pb-Zn矿区花岗闪长岩元素地球化学,LA-ICP-MS锆石U-Pb年龄和Hf同位素特征[J].地质论评,2014,60(4):811-823. Zuo C H,Lu R,Zhao Z X,et al.Characterization of element geochemistry,LA-ICP-MS zircon U-Pb age,and Hf isotope of Granodiorite in the Shuikoushan deposit,Changning,Hunan Province[J].Geological Review,2014,60(4):811-823. [28] 马铁球,李彬,陈焰明,等.湖南南岳岩体LA-ICP-MS锆石U-Pb年龄及其地球化学特征[J].中国地质,2013,40(6):1712-1724. Ma T Q,Li B,Chen Y M,et al.LA-ICP-MS zircon U-Pb age and geochemical characteristics of Nanyue granites in Hunan Province[J].Geology in China,2013,40(6):1712-1724. [29] 马铁球,闫全人,陈辉明,等.湖南攸县新市玄武岩锆石LA-ICP-MS U-Pb定年及其地球化学特征[J].华南地质与矿产,2012,28(4):340-349. Ma T Q,Yan Q R,Chen H M,et al.The zircon LA-ICP-MS U-Pb ages and geochemistry features of basalt at Xinshi,Youxian,Hunan Province[J].Geology and Mineral Resources of South China,2012,28(4):340-349. [30] 刘凯,毛建仁,赵希林,等.湖南紫云山岩体的地质地球化学特征及其成因意义[J].地质学报,2014,88(2):208-227. Liu K,Mao J R,Zhao X L,et al.Geological and geochemical characteristics and genetic significance of the Ziyunshan pluton in Hunan Province[J].Acta Geologica Sinica,2014,88(2):208-227. [31] 刘伟,曾佐勋,陈德立,等.湖南阳明山复式花岗岩的岩石成因:锆石U-Pb年代学、地球化学及Hf同位素约束[J].岩石学报,2014,30(5):1485-1504. Liu W,Zeng Z X,Chen D L,et al.Petrogenesis of the Yangmingshan composite granites in South Hunan Province:Constraints from geochemistry,zircon U-Pb geochronology and Hf istope[J].Acta Petrologica Sinica,2014,30(5):1485-1504. [32] 李勇,张岳桥,苏金宝,等.湖南大义山、塔山岩体锆石U-Pb年龄及其构造意义[J].地球学报,2015,36(3):303-312. Li Y,Zhang Y Q,Su J B,et al.Zircon U-Pb Dating of Dayishan and Tashan plutons in Hunan Province and its tectonic implications[J].Acta Geoscientica Sinica,2015,36(3):303-312. [33] 黄金川. 湖南水口山铅锌金矿床同位素年代学及成岩成矿机理研究[D].北京:中国科学院大学,2016. Huang J C.Isotopic Chronology and Diagenetic Metallogenic Mechanism of Lead-Zinc-Gold Deposits in Shuikoushan,Hunan[D].Beijing:University of Chinese Academy of Sciences,2016. [34] 路睿. 湖南省常宁市水口山铅锌矿床地质特征及成因机制探讨[D].南京:南京大学,2013. Lu R.Geologic Characteristic and Genesis Mechanism of the Shuikoushan Pb-Zn Deposit in Changning City,Hunan Province[D].Nanjing:Nanjing University,2013. [35] 柏道远,钟响,贾朋远,等.湘中印支期关帝庙岩体地球化学特征及成因[J].沉积与特提斯地质,2014,34(4):92-104. Bai D Y,Zhong X,Jia P Y,et al.Geochemistry and petrogenesis of the Indosinian Guandimiao granitic pluton in central Hunan[J].Sedimentary Geology and Tethyan Geology,2014,34(4):92-104. [36] 王岳军,范蔚茗,梁新权,等.湖南印支期花岗岩SHRIMP锆石U-Pb年龄及其成因启示[J].科学通报,2005,50(12):1259-1266. Wang Y J,Fan W M,Liang X Q,et al.SHRIMP Zircon U-Pb ages and it's genesis implication of Indosinian granite in Hunan Province[J].Science Bulletin,2005,50(12):1259-1266. [37] 戴方元,陈必河,刘富国.湖南关帝庙地区脉岩特征及其地质意义[J].国土资源导刊,2008,5(1):33-36. Dai F Y,Chen B H,Liu F G.Characteristics and geological significance of vein rocks in Guandimiao area in Hunan Province[J].Land & Resources Herald,2008,5(1):33-36. [38] 赵增霞,徐兆文,缪柏虎,等.湖南衡阳关帝庙花岗岩岩基形成时代及物质来源探讨[J].地质学报,2015,89(7):1219-1230. Zhao Z X,Xu Z W,Miao B H,et al.Diagenetic age and material source of the Guandimiao granitic batholith,Hengyang city,Hunan Province[J].Acta Geologica Sinica,2015,89(7):1219-1230. [39] 陈迪,刘珏懿,王先辉,等.湖南五峰仙岩体岩石地球化学、SHRIMP U-Pb年龄及Hf同位素特征[J].地质科技情报,2017,36(6):1-12. Chen D,Liu J Y,Wang X H,et al.The petrogeochemistry,SHRIMP zircon U-Pb age,and Hf isotope character of Wufengxian pluton in Hunan Province[J].Geological Science and Technology,2017,36(6):1-12. [40] 彭能立,王先辉,杨俊,等.湖南川口三角潭钨矿床中辉钼矿Re-Os同位素定年及其地质意义[J].矿床地质,2017,36(6):1402-1414. Peng N L,Wang X H,Yang J,et al.Re-Os dating of molybdenite from Sanjiaotan tungsten deposit in Chuankou area,Hunan Province,and its geological implications[J].Mineral Deposits,2017,36(6):1402-1414. [41] Qin J H,Wang D H,Li C,et al.The molybdenite Re-Os isotope chronology,in situ scheelite and wolframite trace elements and Sr isotope characteristics of the Chuankou tungsten ore field,South China[J].Ore Geology Reviews,2020,126:103756. [42] 彭冰霞,王岳军,范蔚茗,等.湖南中部和广东西部3个典型花岗质岩体的LA-ICP-MS锆石U-Pb定年及其成岩意义[J].地质学报,2006,80(10):1597. Peng B X,Wang Y J,Fan W M,et al.U-Pb ages of three typical granitic bodies in the middle of Hunan Province and the western Guangdong Province[J]. Acta Geologica Sinica,2006,80(10):1597. [43] 张晓军,罗华,吴志华,等.湖南大义山矿田白沙子岭锡矿床Rb-Sr同位素等时线年龄及其地质意义[J].中国地质大学学报:地球科学版,2014,39(10):1322-1332. Zhang X J,Luo H,Wu Z H,et al.Rb-Sr Isochron age and its geological significance of Baishaziling Tin deposit in Dayishan ore field,Hunan Province[J].Journal of China University of Geosciences(Earth Science),2014,39(10):1322-1332. [44] 刘耀荣,邝军,马铁球,等.湖南大义山花岗岩南体黑云母40Ar-39Ar定年及地质意义[J].资源调查与环境,2005,26(4):244-249. Liu Y R,Kuang J,Ma T Q,et al.40Ar-39Ar dating of biotitie in south Dayishan granite and its geological significance[J].Resources Survey & Environment,2005,26(4):244-249. [45] Meng L F,Li Z X,Chen H L,et al.Geochronological and geochemical results from Mesozoic basalts in southern South China block support the flat-slab subduction model[J].Lithos,2012,132-133:127-140. [46] 赵振华,包志伟,张伯友.湘南中生代玄武岩类地球化学特征[J].中国科学:D辑,1998,28(S2):7-14. Zhao Z H,Bao Z W,Zhang B Y.Geochemical characteristics of Mesozoic basalts in the Southern Guangxi[J]. Science in China Series D,1998,28(S2):7-14. [47] 谢桂青,彭建堂,胡瑞忠,等.湖南锡矿山锑矿矿区煌斑岩的地球化学特征[J].岩石学报,2001,17(4):629-636. Xie G Q,Peng J T,Hu R Z,et al.Geochemical characteristics of lamprophres in the Xikuangshan antimony ore deposits,Hunan Province[J].Acta Petrologica Sinica,2001,17(4):629-636. [48] 史国伟,欧阳志强,李先灿.湖南邵东县石桥铺矿区铅锌矿地质特征及找矿前景探讨[J].国土资源导刊,2015,12(3):9-15. Shi G W,Ouyang Z Q,Li X C.Geological characteristics and exploration prospect of the lead-zinc deposit in the Shiqiaopu,Shaodong County,Hunan[J].Land & Resources Herald,2015,12(3):9-15. [49] 吴志华,魏绍六.留书塘铅锌矿床成矿特征与找矿方向[J].华南地质与矿产,2009,25(4):17-21. Wu Z H,Wei Z L.Metallogenic characteristics and Pospecting direction of Liushutang lead-zinc deposit[J].Geology and Mineral Resources of South China,2009,25(4):17-21. [50] 欧阳玉飞,黄满湘,郑平.湖南川口杨林坳钨矿床控矿因素与成矿规律研究[J].矿产与地质,2008,22(4):285-288. Ouyang Y F,Huang M X,Zheng P.Research on the ore-controlling factors and ore-forming rules of the Yanglin'ao W deposit in Chuankou,Hunan[J].Mineral Resources and Geology,2008,22(4):285-288. [51] 郑平. 湖南衡南杨林坳白钨矿床控矿构造研究[D].长沙:中南大学,2008. Zheng P.Study on the Ore-controlling Structure of Yanglin'ao Scheelite Deposit in East Hengyang,Hunan Province[D].Changsha:Central South University,2008. [52] 公凡影. 湖南省康家湾铅锌金银矿床地质特征及矿床成因探讨[D].北京:中国地质大学(北京),2012. Gong F Y.Discussion on the Characteristics and Genesis of Kangjiawan Pb-Zn-Au-Ag Deposit,Hunan[D].Beijing:China University of Geosciences Beijing,2012. [53] 王宾海,王诗潮,周倩,等.衡阳盆地北缘盐田桥铜矿床成矿构造地质地球化学特征[J].地质科技情报,2017,36(6):232-238. Wang B H,Wang S C,Zhou Q,et al.Geological and geochemical characteristics of ore controlling structure of the Yantianqiao copper deposit in the northern margin of Hengyang basin[J].Geological Science and Technology Information,2017,36(6):232-238. [54] 刘晓敏,杨亮.湖南谭子山探山岭矿段铜、重晶石矿成矿地质条件分析[J].地球,2016(3):88-89. Liu X M,Yang L.Mineralized geological conditions of copper and barite in Tanshanling section of Tanzishan in Hunan Province[J].Earth,2016(3):88-89. [55] 王银茹. 湖南省川口三角潭钨矿床成因及成矿模式研究[D].长沙:中南大学,2012. Wang Y R.Research on Ore Genesis and Metallogenic Model of the Sanjiaotan Tungsten Deposit in Chuankou,Huan[D].Changsha:Central South University,2012. [56] 缪柏虎. 湖南祁东县清水塘铅锌矿床地质特征及形成机制[D].南京:南京大学,2014. Miao B H.Geologic Characteristic and Genesis Mechanism of the Qingshuitang Pb-Zn Deposit in Qidong County,Hunan Pro-vince[D].Nanjing:Nanjing University,2014. [57] Qin J H,Huang F,Zhong S H,et al.Unraveling evolution histories of large hydrothermal systems via garnet U-Pb dating,sulfide trace element and isotopic analyses:A case study of Shuikoushan polymetallic ore field,South China[J].Ore Geology Reviews,2022,149:105063. [58] 程顺波,吴志华,刘重芃,等.湖南省留书塘铅锌矿床S、Pb同位素特征及意义[J].地质通报,2017,36(5):846-856. Cheng S B,Wu Z H,Liu Z P,et al.Sulfur and lead isotope geochemistry of the Liushutang lead-zinc deposit in Hunan Province and its significance[J].Geological Bulletin of China,2017,36(5):846-856. [59] 毛景文,谢桂青,李晓峰,等.大陆动力学演化与成矿研究:历史与现状——兼论华南地区在地质历史演化期间大陆增生与成矿作用[J].矿床地质,2005,24(3):193-205. Mao J W,Xie G Q,Li X F,et al.Geodynamic process and metallogeny:History and present research trend,with a special discussion on continental accretion and related metallogeny throughout geological history in South China[J].Mineral Deposits,2005,24(3):193-205. [60] Zartman R E,Doe B R.Plumbotectonics-the model[J].Tectonophysics,1981,75(1/2):135-162. [61] 曾志方. 湖南大义山锡矿田构造控矿作用与成矿机理研究[D].武汉:中国地质大学,2013:1-100. Zeng Z F.Research on Tectonic Ore-controlling and Metallogenic Mechanism of the Dayishan Tin Field,Hunan,China[D].Wuhan:China University of Geosciences,2013:1-100. [62] Greentree M R,Li Z X,Li X H,et al.Late mesoproterozoic to earliest neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia[J].Precambrian Research,2006,151(1-2):79-100. [63] 李献华,王选策,李武显,等.华南新元古代玄武质岩石成因与构造意义:从造山运动到陆内裂谷[J].地球化学,2008,37(4):382-398. Li X H,Wang X C,Li W X,et al.Petrogenesis and tectonic significance of Neoproterozoic basaltic rocks in South China:From orogenesis to intracontinental rifting[J].Geochimica,2008,37(4):382-398. [64] Li W X,Li X H,Li Z X,et al.Obduction-type granites within the ne jiangxi ophiolite:implications for the final amalgamation between the Yangtze and cathaysia blocks[J].Gondwana Research,2008,13(3):288-301. [65] Li X H.U-Pb zircon ages of granites from the southern margin of the Yangtze Block:Timing of Neoproterozoic Jinning:Orogeny in SE China and implications for Rodinia assembly[J].Precambrian Research,1999,97(1-2):43-57. [66] 李献华,周汉文,李正祥,等.扬子块体西缘新元古代双峰式火山岩的锆石U-Pb年龄和岩石化学特征[J].地球化学,2001,30(4):315-322. Li X H,Zhou H W,Li Z X,et al.Zircon U-Pb age and petrochemical characteristics of the Neoproterozoic bimodal volcanics from western Yangtze block[J].Geochimica,2001,30(4):315-322. [67] 舒良树. 华南构造演化的基本特征[J].地质通报,2012,31(7):1035-1053. Shu L S.An analysis of principal features of tectonic evolution in South China block[J].Geological Bulletin of China,2012,31(7):1035-1053. [68] Gilder S A,Keller G R,Luo M,et al.Eastern Asia and the Western Pacific timing and spatial distribution of rifting in China[J].Tectonophysics,1991,197(2-4):225-243. [69] Li X H.Cretaceous magmatism and lithospheric extension in southeast China[J].Journal of Asian Earth Sciences,2000,18(3):293-305. [70] 夏文臣. 中国东部中、新生代断陷盆地的成因地层格架及其与油气的关系[J].地质科技情报,1991,10(1):41-48. Xia W C.Genetic stratigraphic framework and its genetic relationship to oil and gas in mesozoic and Cenozoic Faultcontrolled basins of eastern China[J].Geological Science and Technology Information,1991,10(1):41-48. [71] 华仁民,陈培荣,张文兰,等.华南中、新生代与花岗岩类有关的成矿系统[J].中国科学(D辑),2003,33(4):335-343. Hua R M,Chen P R,Zhang W L,et al.Metallogenic systems related to Mesozoic and Cenozoic granitoids in South China[J].Science in China Series D:Earth Sciences,2003,46(8):816-829. [72] Wernicke B,Axen G J,Snow J K.Basin and Range extensional tectonics at the latitude of Las Vegas,Nevada[J].GSA Bulletin,1988,100(11):1738-1757. [73] Zhou X M,Li W X.Origin of Late Mesozoic igneous rocks in Southeastern China:implications for lithosphere subduction and underplating of mafic magmas[J].Tectonophysics,2000,326(3-4):269-287. [74] 舒良树,王德滋.北美西部与中国东南部盆岭构造对比研究[J].高校地质学报,2006,12(1):1-13. Shu L S,Wang D Z.A comparison study of basin and range tectonics in the western North America and southeastern China[J].Geological Journal of China Universities,2006,12(1):1-13. [75] 张进业. 衡山变质核杂岩体西缘构造特征[J].华东地质学院学报,1994,17(1):18-22. Zhang J Y.Tectonic feature of the western edge in the metamorphic nucleus complex of Hengshan[J].Journal of East China Geological Institute,1994,17(1):18-22. [76] Hill R I,Campbell I H,Davies G F,et al.Mantle plumes and continental tectonics[J].Science,1992,256(5054):186-193. [77] Parsons T,Thompson G A,Smith R P.More than one way to stretch:A tectonic model for extension along the plume track of the Yellowstone hotspot and adjacent Basin and Range Province[J].Tectonics,1998,17(2):221-234. [78] 王五力,郭胜哲.中国东北古亚洲与古太平洋构造域演化与转换[J].地质与资源,2012,21(1):27-34. Wang W L,Guo S Z.The evolution and transformation of Paleo-Asia and Paleo-Pacific tectonic domain of northeast China[J].Geology and Resources,2012,21(1):27-34. [79] 童航寿. 华南地幔柱构造与成矿[J].铀矿地质,2010,26(2):65-72,94. Tong H S.Mantle plume structure and metallogenesis in South China[J].Uranium Geology,2010,26(2):65-72,94. [80] 华仁民,陈培荣,张文兰,等.论华南地区中生代3次大规模成矿作用[J].矿床地质,2005,24(2):99-107. Hua R M,Chen P R,Zhang W L,et al.Three major metallogenic events in Mesozoic in South China[J].Mineral Deposits,2005,24(2):99-107. [81] 陈毓川,裴荣富,张宏良.南岭地区与中生代花岗岩类有关的有色、稀有金属矿床地质[J].地球学报,1990,17(1):79-85. Chen Y C,Pei R F,Zhang H L.The geology of nonferrous and rare metal deposits related to Mesozoic Granitoids in the Nanling region,China[J].Acta Geoscientica Sinica,1990,17(1):79-85.
2024, Vol. 11 
