吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1462-1490.doi: 10.13278/j.cnki.jjuese.20190308

• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇    下一篇

粤东莲花山地区多期岩浆锆石年代学、Hf同位素组成及其成矿作用

范飞鹏1, 肖惠良1, 陈乐柱1, 李海立1, 刘建雄2, 邓中林2, 康丛轩1, 林耿伟3, 陈凯4   

  1. 1. 中国地质调查局南京地质调查中心, 南京 210016;
    2. 广东省佛山地质局, 广东 佛山 528000;
    3. 广东省第二地质大队, 广东 汕头 515000;
    4. 中国矿业大学资源与地球科学学院, 江苏 徐州 221000
  • 收稿日期:2019-07-20 出版日期:2020-09-26 发布日期:2020-09-29
  • 作者简介:范飞鹏(1982-),男,高级工程师,主要从事金属矿产调查、评价和研究工作,E-mail:fanfp1111@163.com
  • 基金资助:
    中国地质调查局项目（12120114015701，DD20190153，DD20160037）；国家重点研发计划项目（2016YFC0600210）

Zircon U-Pb Age and Hf Isotope of Multiple-Stage Magmatism and Mineralization in Lianhuashan Region, Eastern Guangdong

Fan Feipeng1, Xiao Huiliang1, Chen Lezhu1, Li Haili1, Liu Jianxiong2, Deng Zhonglin2, Kang Congxuan1, Lin Gengwei3, Chen Kai4   

  1. 1. Nanjing Center, China Geological Survey, Nanjing 210016, China;
    2. Guangdong Foshan Geological Bureau, Foshan 528000, Guangdong, China;
    3. Guangdong Second Geological Brigade, Shantou 515000, Guangdong, China;
    4. College of Resources and Geosciences, China University of Mining and Technology, Xuzhou 221000, Jiangsu, China
  • Received:2019-07-20 Online:2020-09-26 Published:2020-09-29
  • Supported by:
    Supported by Project of China Geological Survey (12120114015701, DD20190153,DD20160037) and National Key R & D Program of China (2016YFC0600210)

PDF (PC)

229

摘要： 粤东莲花山地区位于我国东南沿海火山岩发育区，是我国重要的钨金成矿远景区。通过对该地区各类花岗岩进行LA-ICP-MS锆石U-Pb定年、岩石地球化学特征、锆石Lu-Hf同位素组成和微量元素研究，结果表明：莲花山地区的岩浆活动至少存在3期，其中石英闪长玢岩形成于中侏罗世（（168.0±2.2）Ma），黑云母二长花岗岩形成于早白垩世早期（（137.5±1.9）Ma），石英斑岩形成于早白垩世晚期（（102.0±1.5）Ma和（98.7±1.8）Ma）；岩石以钙碱性铝质-强过铝质岩浆为主，石英斑岩和流纹斑岩与成矿关系密切；各类岩浆锆石的176Lu/177Hf值均低于0.002，176Hf/177Hf值大多数小于0.282 7，εHf（t）值大多数处于-2.57~1.00之间，fLu-Hf值为-0.99~-0.95，二阶段模式年龄主要介于1.00~0.81 Ga之间，指示成岩物质来源主要来自新元古代古老下地壳变质泥岩和变质砂岩部分熔融，有少量幔源物质加入；锆石结晶温度大多处于650~750℃之间，岩石为I型花岗岩。莲花山地区不同阶段的岩浆活动和成矿作用与区域构造转换事件相关，虽缺少高精度成矿年龄对成矿时限的限制，但根据地质事实和本次研究认为该地区主要的钨金成矿时间应略晚于石英斑岩的形成时间（（102.0~98.7）Ma）。

关键词: 花岗岩, LA-ICP-MS锆石U-Pb定年, Lu-Hf同位素, 成矿作用, 莲花山钨金矿床, 粤东莲花山地区

Abstract: Lianhuashan region is located in the continental volcanic area of the southeast coast of China, which is an important prospecting area for tungsten-gold mineralization. The authors studied the zircon U-Pb age, granite geochemistry, zircon trace elements, and Hf isotope of the newly found Mesozoic intrusive rocks in Lianhuashan region in the southeast coastal areas of China, and identified three stages magmatism: Middle Jurassic quartz diorite porphyries ((168.0±2.2) Ma), early stage of Early Cretaceous biotite monzonites( (137.5±1.9)Ma), and late stage of Early Cretaceous quartz porphyries ((102.0±1.5) Ma and (98.7±1.8) Ma). The intrusive rocks belong to calc-alkaline, aluminous, strong-peraluminous magmatic rocks. The quartz porphyry and rhyolite porphyry are closely related to the mineralization. The 176Lu/177Hf values of all magmatic zircons are less than 0.002, the 176Hf/177Hf values are mostly less than 0.282 7. The zircon Hf isotope values of εHf(t) are mostly between -2.57 and 1.00, fLu-Hf values are in the range of -0.99-0.95, and their corresponding crustal model ages (TDM2) are mainly 1.00-0.81 Ga, which indicates that the source of diagenetic materials were derived from the partial melting of metamorphic mudstones and metamorphic sands of Neoproterozoic in the lower crust, and mixed with small amount of mantle material. The crystallization temperatures of zircons are mostly in the range of 650-750 ℃, which shows the characteristics of I-type granite. In combination with all these data, the magmatism and mineralization of Lianhuashan region are closely related to the tectonic transformation event. Although there is no high-precision metallogenic age to limit the time of metallogeny, the tungsten-gold mineralization time should be slightly later than the formation time of the quartz porphyry (ca. 102.0-98.7) according to the geological facts and this study results.

Key words: granites, LA-ICP-MS zircon U-Pb dating, Lu-Hf isotope, mineralization, Lianhuashan tungsten-gold deposit, Lianhuashan region,eastern Guangdong

中图分类号: 

  • P588.12
[1] 徐晓春,岳书仓.粤东地区中生代火山岩与侵入岩的成因关系及成因类型[J].合肥工业大学学报(自然科学版),1994,17(4):184-192. Xu Xiaochun,Yue Shucang. Genetic Relationship and Type of the Mesozoic Volcanic and Intrusive Rocks in Eastern Guangdong,China[J]. Journal of Hefei University of Technology(Natural Sciences), 1994, 17(4):184-192.
[2] 徐晓春,岳书仓.粤东地区中生代岩浆作用的大地构造背景及构造-岩浆演化[J].合肥工业大学学报(自然科学版),1996, 19(1):127-134. Xu Xiaochun,Yue Shucang. Tectonic Background and Evolution of Mesozoic Magmatism,Eastern Guangdong[J].Journal of Hefei University of Technology(Natural Sciences),1996,19(1):127-134.
[3] 周新民.南岭地区晚中生代花岗岩成因与岩石圈动力学演化[M].北京:科学出版社, 2007:1-691. Zhou Xinmin. Petrogenesis and Geodynamic Evolution of Late Mesozoic Granites in Nanling Region[M]. Beijing:Science Press, 2007:1-691.
[4] 李献华,李武显,李正祥.再论南岭燕山早期花岗岩的成因类型与构造意义[J].科学通报, 2007,52(9):981-991. Li Xianhua,Li Wuxian,Li Zhengxiang. Discussed Again on the Genetic Types and Tectonic Significance of Early Yanshanion Granite in Nanling[J]. Chinese Science Bulletin, 2007,52(9):981-991.
[5] 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 Jingwen,Xie Guiqing,Guo Chunli,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.
[6] 毛景文,谢桂青,郭春丽,等.华南地区中生代主要金属矿床时空分布规律和成矿环境[J].高校地质学报, 2008,14(4):510-526. Mao Jingwen,Xie Guiqing,Guo Chunli,et al. Spatial-Temporral Distribution of Mesozoic Ore Deposits in South China and Their Metallogenic Setting[J]. Geological Journal of China Universities, 2008,14(4):510-526.
[7] 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 Liangshu. An Analysis of Principal Features of Tectonic Evolution in South China Block[J]. Geological Bulletin of China, 2012,31(7):1035-1053.
[8] 阳杰华,刘亮,刘佳.华南中生代大花岗岩省成岩成矿作用研究进展与展望[J].矿物学报,2017,37(6):791-800. Yang Jiehua, Liu Liang, Liu Jia. Research Progress and Prospects of Diagenesis and Mineralization in Mesozoic Granite Province of South China[J]. Acta Mineralogica Sinica, 2017,37(6):791-800.
[9] 王文宝,李建华,辛宇佳,等.华南大容山-十万大山花岗岩体LA-ICP-MS锆石U-Pb定年、地球化学特征及地质意义[J].地球学报,2018,39(2):179-188. Wang Wenbao, Li Jianhua, Xin Yujia,et al. LA-ICP-MS Zircon U-Pb Dating, Geochemical Characteristics and Geological Significance of the Darongshan-Shiwandashan Granite Body in Yingqi, South China[J]. Acta Geoscientica Sinica, 2018,39(2):179-188.
[10] 王帅,陶继华,李武显,等.赣西北麦斜岩体锆石U-Pb年代学、地球化学以及Sr-Nd同位素研究及其岩石成因[J].地质学报,2018,92(4):747-768. Wang Shuai, Tao Jihua, Li Wuxian,et al. Zircon U-Pb Geochronology, Geochemistry and Sr-Nd Isotope Studies and Their Petrogenesis of the Mai Clinolith in Northwestern Jiangxi Province[J]. Acta Geologica Sinica, 2018, 92(4):747-768.
[11] 陈毓川,王登红,徐志刚,等. 华南区域成矿和中生代岩浆成矿规律概要[J]. 大地构造与成矿学,2014,38(2):219-229. Chen Yuchuan, Wang Denghong, Xu Zhigang,et al. Summary of Regional Metallogenic and Mesozoic Magmatic Metallogenic Laws in South China[J]. Geotectonica et Metallogenia, 2014, 38(2):219-229.
[12] 朱志刚.广东省黄金矿床的地质特征及找矿方向[J].南方金属, 2001(6):5-9. Zhu Zhigang. Geological Characteristics and Prospecting Direction of Gold Deposits in Guangdong[J]. Southern Metals, 2001(6):5-9.
[13] 毛景文,李晓峰,张作衡,等.中国东部中生代浅成热液金矿的类型、特征及其地球动力学背景[J]. 高校地质学报, 2003, 9(4):620-637. Mao Jingwen, Li Xiaofeng, Zhang Zuoheng,et al. Types, Characteristics and Geodynamic Background of Mesozoic Epithermal Gold Deposits in Eastern China[J]. Geological Journal of China Universities, 2003, 9(4):620-637.
[14] 王成辉,刘善宝,郭春丽,等.南岭地区与金矿有关岩浆岩成矿专属性初探[J].大地构造与成矿学, 2014, 38(2):276-288. Wang Chenghui,Liu Shanbao,Guo Chunli,et al. Metallogenic Specialization of the Magmatic Rocks Associated with Gold Deposits in the Nanling Region[J]. Geotectonica et Metallogenia, 2014, 38(2):276-288.
[15] 王成辉,徐珏,黄凡,等.中国金矿资源特征及成矿规律概要[J].地质学报, 2014, 88(12):2315-2325. Wang Chenghui,Xu Jue,Huang Fan,et al. Resources Characteristics and Outline of Regional Metallogeny of Gold Deposits in China[J]. Acta Geologica Sinica, 2014, 88(12):2315-2325.
[16] 范飞鹏,肖惠良,陈乐柱,等.粤东鸿沟山金矿区流纹斑岩锆石SHRIMP U-Pb定年、Lu-Hf同位素组成及其地质意义[J].地质论评,2018,64(1):213-226. Fan Feipeng,Xiao Huiliang,Chen Lezhu,et al. SHRIMP Zircon U-Pb Dating, Lu Hf Isotopic Composition of Rhyolitic Porphyry in Honggoushan Gold Deposit, Eastern Guangdong, and Their Geological Significance[J].Geological Review, 2018, 64(1):213-226.
[17] Qiu Zengwang, Yan Qinghe, Li Shasha, et al. Highly Fractionated Early Cretaceous I-Type Granites and Related Sn Polymetallic Mineralization in the Jinkeng Deposit, Eastern Guangdong, SE China:Constraints from Geochronology, Geochemistry, and Hf Isotopes[J]. Ore Geology Reviews,2017,88:718-738.
[18] Yan Qinghe, Wang He, Qiu Zengwang, et al. Origin of Early Cretaceous A-Type Granite and Related Sn Mineralization in the Sanjiaowo Deposit, Eastern Guangdong, SE China and Its Tectonic Implication[J]. Ore Geology Reviews,2018,93:60-80.
[19] Zhang Lipeng, Zhang Rongqing, Chen Yuxiao, et al. Geochronology and Geochemistry of the Late Cretaceous Xinpeng Granitic Intrusion, South China:Implication for Sn-W Mineralization[J]. Ore Geology Reviews, 2019, 113:103.
[20] 满发胜,白玉珍,倪守斌,等.莲花山钨矿床同位素地质学初步研究[J].矿床地质, 1983, 2(4):35-42. Man Fasheng, Bai Yuzhen, Ni Shoubin, et al. Preliminary Isotope Studies of the Lianhuashan Tungsten Ore Deposit[J]. Mineral Deposits, 1983, 2(4):35-42.
[21] 陈惜华, 胡祥昭, 丛献东.西岭锡矿床岩体含矿性与成因类型的研究[J]. 地球化学, 1986(1):50-57. Chen Xihua, Hu Xiangzhao, Cong Xiandong. Genesis and Mineralization of Subgranitic Porphyry, Xiling Tin Deposit, Guangdong[J]. Geochimica, 1986(1):50-57.
[22] 地质矿产部书刊编辑室.全国同位素年龄汇编(3)[M].北京:地质出版社,1983. Editorial Office of the Ministry of Geology and Mineral Resources. Compilation of National Isotope Age (3)[M]. Beijing:Geological Publishing House,1983.
[23] 尹家衡,黄光昭,徐明华.粤东中生代火山旋回划分及对比[J].中国地质科学院南京地质矿产研究所所刊, 1989, 10(4):16-28. Yin Jiaheng, Huang Guangzhao, Xu Minghua. Contrasting and Divission of Mesozoic Volcanic Cycles in East Guangdong[J]. Nanjing Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, 1989, 10(4):16-28.
[24] 李坤英,沈加林,王小平,等.东南沿海火山、侵入杂岩同位素年代学[J].中国地质科学院南京地质矿产研究所所刊, 1990,11(4):45-57. Li Kunying, Shen Jialin, Wang Xiaoping, et al. The Isotopic Geochronology of Volcano and Intrusive Rocks in Southeast Coastal of China[J]. Nanjing Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, 1990,11(4):45-57.
[25] 徐晓春.粤东中生代火山-侵入杂岩的稀土元素地球化学研究[J].合肥工业大学学报(自然科学版), 1993,16(2):121-127. Xu Xiaochun. REE Geochemistry of Mesozoic Volcanic Intrusive Complexes in Eastern Guangdong[J]. Journal of Hefei University of Technology(Natural Sciences), 1993, 16(2):121-127.
[26] 谢芳忠.广东莲花山钨金矿地质特征及其找矿意义[J].黄金地质科技, 1993(3):19-21. Xie Fangzhong. Geological Characteristics and Prospecting Significance of Lianhuashan Tungsten-Gold Deposit in Guangdong[J]. Gold Geology, 1993(3):19-21.
[27] 赵希林,毛建仁,陈荣,等.闽西南地区紫金山岩体锆石SHRIMP定年及其地质意义[J].中国地质, 2008,35(4):590-597. Zhao Xilin, Mao Jianren, Chen Rong, et al. SHRIMP Zircon Dating of the Zijinshan Pluton in Southwestern Fujian and Its Implications[J]. Geology in China, 2008, 35(4):590-597.
[28] 王小雨.粤东新寮岽铜多金属矿床地质特征及成因初步研究[D].北京:中国地质大学(北京), 2015:1-99. Wang Xiaoyu. Preliminary Study on Geological Characteristics and Genesis of the Xinliaodong Cu Polymetallic Deposit in Eastern Guangdong Province[D]. Beijing:China University of Geosciences(Beijing), 2015:1-99.
[29] 王小雨,毛景文,程彦博,等.粤东新寮岽铜多金属矿区石英闪长岩锆石U-Pb年龄、地球化学及Hf同位素组成[J]. 地质通报, 2016,35(8):1357-1375. Wang Xiaoyu, Mao Jingwen, Cheng Yanbo, et al. Zircon U-Pb Age, Geochemistry and Hf Isotopic Compositions of Quartzdiorite from the Xinliaodong Cu Polymetallic Deposit in Eastern Guangdong Province[J]. Geological Bulletin, 2016, 35(8):1357-1375.
[30] 刘鹏,程彦博,毛景文,等.粤东田东钨锡多金属矿床花岗岩锆石U-Pb年龄、Hf同位素特征及其意义[J].地质学报, 2015, 89(5):1244-1257. Liu Peng, Cheng Yanbo, Mao Jingwen, et al. Zircon U-Pb Age and Hf Iostopic Characteristics of Granite from the Tiandong Tungsten-Sn Polymetallic Deposit in Eastern Guangdong Province and Its Significance[J]. Acta Geologica Sinica, 2015, 89(5):1244-1257.
[31] 李海立,肖惠良,范飞鹏,等.广东潮安飞鹅山钨钼多金属矿床辉钼矿Re-Os同位素定年[J]. 地质学报, 2016, 90(2):231-239. Li Haili, Xiao Huiliang, Fan Feipeng, et al. Molybdenite Re-Os Isotopic Age of Fei'eshan Tungsten and Molybdenum Polymetallic Deposit in Chao'an Guangdong[J]. Acta Geologica Sinica, 2016, 90(2):231-239.
[32] 梁敦杰,谢佑才.广东莲花山断裂带西南段地质构造特征[J].中国区域地质,1988(2):30-35. Liang Dunjie, Xie Youcai. Geological Structural Characteristics of the Southwestern Segment of Lianhuashan Fault Zone in Guangdong[J]. Regional Geology of China, 1988(2):30-35.
[33] 雷新勇,岳书仓.广东莲花山钨矿床成岩-成矿稀土元素地球化学研究[J].地质与勘探,1989(3):15-20. Lei Xinyong, Yue Shucang. Geochemistry of Diagenesis-Metallogenesis REE of Lianhuashan Tungsten Deposit, Guangdong[J]. Geology and Exploration, 1989(3):15-20.
[34] 李建超,丘元禧.广东莲花山燕山早期断裂动热变质带的基本特征及形成机制的探讨[J].长春地质学院学报,1990,20(1):11-20,123. Li Jianchao, Qiu Yuanxi. Basic Characteristics and Formation Mechanism of the Early Yanshan Fault Dynamic-Thermal Metamorphic Belt in Lianhuashan, Guangdong[J]. Journal of Changchun Institute of Geology, 1990,20(1):11-20,123.
[35] 何双梅,曹芬元,刘燕忠.广东莲花山钨矿床中发现自然铝[J].地质与勘探,1990(9):32-34. He Shuangmei, Cao Fenyuan, Liu Yanzhong. Natural Aluminium Found in Lianhuashan Tungsten Deposit, Guangdong[J]. Geology and Exploration, 1990(9):32-34.
[36] 黄玉昆,张珂.广东莲花山断裂带的新构造运动特征[J].华南地震,1990(2):25-34. Huang Yukun,Zhang Ke. Neotectonic Movement Characteristics of the Lianhuashan Fault Zone in Huangyukun, Zhangke, Guangdong[J]. South China of Seismology, 1990(2):25-34.
[37] 周立功.广东莲花山断裂带的现今活动研究[J].中国地质科学院562综合大队集刊,1991(增刊):107-122. Zhou Ligong. Study on the Present Activities of Lianhuashan Fault Zone in Guangdong[J]. Collection of 562 Comprehensive Brigades, Chinese Academy of Geological Sciences, 1991(Sup.):107-122.
[38] 邱元禧,邱津松,李建超,等.广东莲花山断裂带中、新生代多期复合变形变质带的基本特征及其形成机制的探讨[J].中国地质科学院地质力学研究所所刊,1991(增刊):93-106. Qiu Yuanxi, Qiu Jinsong, Li Jianchao,et al. Basic Characteristics and Formation Mechanism of Mesozoic-Cenozoic Composite Deformation Metamorphic Belt in Lianhuashan Fault Zone, Guangdong[J]. Journal of Institute of Geomechanics, Chinese Academy of Geological Sciences, 1991(Sup.):93-106.
[39] 邹和平,王建华,丘元禧.广东南澳和莲花山韧性剪切带40Ar/39Ar年龄及其地质意义[J].地球学报,2000,21(4):356-364. Zou Ping, Wang Jianhua, Qiu Yuanxi.40Ar/39Ar Age of Nanao and Lianhuashan Ductile Shear Zones in Guangdong and Its Geological Significance[J]. Acta Geoscientica Sinica, 2000, 21(4):356-364.
[40] 杜继宇. 莲花山断裂带和长乐-南澳断裂带构造特征及活动时代[D].长春:吉林大学,2012. Du Jiyu. Structural Characteristics and Active Ages of Lianhuashan Fault Zone and Changle-Nan'ao Fault Zone[D]. Changchun:Jilin University, 2012.
[41] 汪礼明,王军,王核,等.粤东莲花山断裂带动力变质作用与动力变质热液成矿[J].大地构造与成矿学,2018,42(5):908-917. Wang Liming, Wang Jun, Wang He,et al. Dynamic Metamorphism and Hydrothermal Metallogenesis of Lianhuashan Fault Zone in Eastern Guangdong[J]. Geotectonica et Metallogenia, 2018,42(5):908-917.
[42] 陈叙涛.广东莲花山钨矿地质特征及成矿模式分析[J].西部资源,2017(4):91-92. Chen Xutao. Analysis of Geological Characteristics and Metallogenic Model of Lianhuashan Tungsten Deposit in Guangdong[J]. Western Resources, 2017(4):91-92.
[43] 贾黎黎.广东莲花山地区成矿规律研究[J].西部资源,2017(3):28-30. Jia Lili. Study on Metallogenic Regularity of Lianhuashan Area in Guangdong[J]. Western Resources, 2017(3):28-30.
[44] 张均红. 广东莲花山斑岩型钨-金矿蚀变矿化特征及其找矿意义[C]//四川省地质学会2015年资料汇编:I. 成都:四川省地质学会,2015:3. Zhang Junhong. Alteration and Mineralization Characteristics of Lianhuashan Porphyry Tungsten-Gold Deposit in Guangdong Province and its Prospecting Significance[C]//Data Compilation of Sichuan Geological Society in 2015:I. Chengdu:Sichuan Geological Society, 2015:3.
[45] 李晓蕾. 中国典型钨矿床地质找矿模型研究[D].北京:中国地质大学(北京),2014:1-74. Li Xiaolei. Study on Geological Prospecting Model of Typical Tungsten Deposits in China[D].Beijing:China University of Geosciences (Beijing), 2014:1-74.
[46] 柳少波,王联魁.广东莲花山斑岩型钨-金矿床蚀变矿化特征及分带模式[J].长春地质学院学报,1997, 27(3):57-64. Liu Shaobo, Wang Liankui. Alteration Mineralization Characteristics and Zoning Patterns of Lianhuashan Porphyry Tungsten-Gold Deposit, Guangdong[J]. Journal of Changchun Institute of Geology, 1997,27(3):57-64.
[47] 柳少波,王联魁.莲花山斑岩型W-Au矿床成矿流体来源及其演化[J].世界地质,1996,15(2):55-60. Liu Shaobo, Wang Liankui. Origin and Evolution of Ore-Forming Fluids in Lianhuashan Porphyry W-Au Deposit[J]. Global Geology, 1996,15(2):55-60.
[48] 李兆麟,杨忠芳.广东莲花山钨矿成岩成矿温度研究[J].矿床地质,1995, 14(3):252-260. Li Zhaolin, Yang Zhongfang. Study on Diagenetic and Metallogenic Temperature of Lianhuashan Tungsten Deposit, Guangdong[J]. Mineral Deposits,1995, 14(3):252-260.
[49] 谢芳忠.广东莲花山钨金矿地质特征及其找矿意义[J].黄金地质科技,1993(3):19-21. Xie Fangzhong. Geological Characteristics and Prospecting Significance of Lianhuashan Tungsten-Gold Deposit in Guangdong[J]. Gold Geology, 1993(3):19-21.
[50] 李兆麟,杨忠芳.广东莲花山钨矿成矿机制探讨[J].地质找矿论丛,1992(1):63-70. Li Zhaolin, Yang Zhongfang. Discussion on the Metallogenic Mechanism of Lianhuashan Tungsten Deposit in Guangdong[J]. Contributions to Geology and Mineral Resources Research, 1992(1):63-70.
[51] 曾玖吾,王曼祉,陈森煌,等.广东莲花山斑岩型钨矿床钴金银碲铋矿物的研究[J].矿物岩石,1987(4):12-18. Zeng Jiuwu, Wang Manzhi, Chen Senhuang,et al. Study on Cobalt, Gold, Silver, Tellurium Bismuth Minerals in Lianhuashan Porphyry Tungsten Deposit, Guangdong[J]. Journal of Mineralogy and Petrology, 1987(4):12-18.
[52] 曾玖吾,王曼祉,曲维政,等.广东莲花山钨矿床中分散钨赋存情况及有用元素综合利用的研究[J].地质找矿论丛,1986(2):36-45. Zeng Jiuwu, Wang Manzhi, Qu Weizheng, et al. A Study on the Occurrence of Dispersed Tungsten and the Comprehensive Utilization of Useful Elements in Lianhuashan Tungsten Deposit, Guangdong[J]. Contributions to Geology and Mineral Resources Research, 1986(2):36-45.
[53] 余纪能.广东莲花山断裂带中段锡矿床成矿地质特征[J].矿产与地质,1985(3):13-21. Yu Jineng. Metallogenic Geological Characteristics of Tin Deposits in the Middle Section of Lianhuashan Fault Zone, Guangdong[J]. Mineral Resources and Geology, 1985(3):13-21.
[54] 汪礼明,卜安,王核,等.广东莲花山断裂带南西段整装勘查区勘查找矿新进展[J].矿床地质,2014,33(增刊1):965-966. Wang Liming, Bu An, Wang He, et al. New Progress in Prospecting and Prospecting in the Whole Exploration Area of the South-West Segment of Lianhuashan Fault Zone in Guangdong[J]. Mineral Deposits, 2014, 33(Sup.1):965-966.
[55] 钱龙兵,郭丽荣,余庆亮.广东莲花山断裂带南西段整装勘查区矿床预测模型[J].地质学刊,2017,41(3):468-473. Qian Longbing, Guo Lirong, Yu Qingliang. Prediction Model of Mineral Deposits in the Whole Prospecting Area in the South-West Segment of Lianhuashan Fault Zone, Guangdong[J]. Journal of Geology, 2017,41(3):468-473.
[56] 王军.广东莲花山断裂带南西段锡铜多金属矿整装勘查区基础地质与综合研究新进展[J].资源环境与工程,2018,32(2):209-211. Wang Jun. New Advances in Basic Geology and Comprehensive Research in the Integrated Prospecting Area for Tin-Copper Polymetallic Deposits in the South-West Segment of Lianhuashan Fault Zone, Guangdong[J]. Resources Environment & Engineering, 2018,32(2):209-211.
[57] 徐晓春,岳书仓.粤东中生代火山-侵入杂岩的地壳深熔成因:Pb-Nd-Sr多元同位素体系制约[J].地质论评, 1999, 45(增刊1):829-835. Xu Xiaochun,Yue Shucang. The Origin of Deep Crustal Melting of Mesozoic Volcanic Intrusive Complex in Eastern Guangdong Province:Constraints of Pb-Nd-Sr Multiple Isotope System[J]. Geological Review, 1999, 45(Sup.1):829-835.
[58] Liu Y S, Hu Z C, Gao S, et al. In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS Without Applying an Internal Standard[J]. Chemical Geology, 2008, 257(1):34-43.
[59] Liu Y, Gao S, Hu Z, et al. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons of Mantle Xenoliths[J]. Journal of Petrology,2010, 51(1/2):537-571.
[60] Liu Y, Hu Z,Zong K, et al. Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010, 55(15):1535-1546.
[61] Wiedenbeck M, Alle P, Corfu F, et al. Three Natural Zircon Standards for U-Th-Pb, Lu-Hf, Trace Element and REE Analyses[J]. Geostandards and Geoanalytical Research,1995, 19:1-23.
[62] Sláma J, Kosler J, Condon D J, et al. Plesovice Zircon:A New Natural Reference Material for U-Pb and Hf Isotopic Microanalysis[J]. Chemical Geology, 2008, 249:1-35.
[63] Ludwig K R. ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel[C]//US Geol Surp.Open File Rep. Berkeley:Berkeley Geochronology Center Special Publication, 2003:91-445.
[64] Alain Cocherie, Michèle Robert. Laser Ablation Coupled with ICP-MS Applied to U-Pb Zircon Geochronology:A Review of Recent Advances[J]. Gondwana Research,2008, 14(4):597-608.
[65] Wu F Y, Yang Y H, Xie L W, et al. Hf Isotopic Compositions of the Standard Zircons and Baddeleyites Used in U-Pb Geochronology[J]. Chemical Geology, 2008, 234(1/2):105-126.
[66] 谭运金.广东莲花山斑岩钨矿床地质地球化学特征及矿床成因[J]. 地球化学,1983(2):121-132. Tan Yunjin. Geological and Geochemical Characteristics and Genesis of Lianhuashan Porphyry Tungsten Deposit, Guangdong[J]. Geochimica, 1983(2):121-132.
[67] Sun S S, McDonough W F. Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[C]//Saunders A D, ChNorry M J. Magmatism in the Ocean Basins. London:Geological Society of Special Publications, 1989:313-345.
[68] 黄道袤,万渝生,张德会,等.华北克拉通南缘下汤地区古元古代构造热事件:地球化学特征、锆石SHRIMP U-Pb定年和Hf同位素研究[J].地质论评, 2016, 62(6):1439-1461. Huang Daomao, Wan Yusheng, Zhang Dehui, et al. Paleoproterozoic Tectono-Thermal Events in the Xiatang Area,Lushan County,Southern Margin of the North China Craton:Evidence from Geochemical Features,Zircon SHRIMP Dating and Hf Isotopic Analysis[J]. Geological Review, 2016, 62(6):1439-1461.
[69] Blichert-Toft,Albarede F. The Lu-Hf Isotope Geochemistry of Chondrites and the Evolution of the Mantle-Crust System[J]. Earth Planet Science Letter, 1997, 148:243-258.
[70] Grifin W L, Wang Xiang, Jackson S E, et al. Zircon Chemistry and Magma Genesis, SE China:In-situ Analysis of Hf Isotopes, Tonglu and Pingtan Igneous Complexes[J]. Lithos, 2002, 61:237-269.
[71] Scherer E. Calibration of the Lutetium-Hafnium Clock[J]. Science, 2001, 293:683-687.
[72] Amelin Y,Lee D C,Halliday A N, et al. Nature of the Earth's Earliest Crust from Hafnium Isotopes in Single Detrital Zircons[J]. Nature, 1999, 399:252-255.
[73] Vervoorta J D,Patchetta P J,Blichert T J, et al. Relationships Between Lu-Hf and Sm-Nd Isotopic Systems in the Global Sedimentary System[J]. Earth and Planetary Science Letters, 1999, 168(1/2):79-99.
[74] 白玉珍,满发胜,倪守斌,等.莲花山钨矿区K-Ar同位素地质年龄[J].地球化学, 1983(2):133-139. Bai Yuzhen, Man Fasheng, Ni Shoubin, et al. K-Ar Dating of Lianhuashan Tungsten Ore Deposit[J]. Geochimica, 1983(2):133-139.
[75] 吴福元,李献华,郑永飞,等. Lu-Hf同位素体系及其岩石学应用[J].岩石学报, 2007, 20(2):185-220. Wu Fuyuan, Li Xianhua, Zheng Yongfei,et al. Lu-Hf Isotopic System and Its Petrological Application[J]. Acta Petrologica Sinica, 2007, 20(2):185-220.
[76] King P L, White A J R, Chappell B W, et al. Characterization and Origin of Aluminous A-Type Granites from the Lachlan Fold Belt, Southeastern Australia[J]. Journal of Petrology, 1997(3):371-391.
[77] 王涛,刘燊. 胶南花岗岩锆石饱和温度及其地质意义[J].矿物岩石地球化学通报,2013, 32(5):619-624. Wang Tao, Liu Shen. Zircon Saturation Temperature of Jiaonan Granite and Its Geological Significance[J]. Bulletin of Mineralogy,Petrology and Geochemistry, 2013, 32(5):619-624.
[78] Watson E B,Harrison T M. Zircon Saturation Revisited:Temperature and Composition Effect in Avariety of Crustal Magmas Types[J]. Earth and Planetary Science Letters, 1983, 64(2):295-304.
[79] Watson E B, Wark D A T,Homas J B. Crystallization Thermometers for Zircon and Rutile[J]. Contrib Mineral Petrol, 2006, 151(4):413-433.
[80] Ferry J M,Watson E B. New Thermodynamic Models and Revised Calibrations for the Ti-In-Zircon and Zr-In-Rutile Thermometers[J]. Contrib Mineral Petrol, 2007, 154(4):429-437.
[81] 周金胜,孟祥金,臧文栓,等. 西藏青草山斑岩铜金矿含矿斑岩锆石U-Pb年代学、微量元素地球化学及地质意义[J]. 岩石学报,2013,29(11):3755-3766. Zhou Jinsheng, Meng Xiangjin, Zang Wenshuan,et al. Zircon U-Pb Geochronology, Trace Element Geochemistry and Geological Significance of Ore-Bearing Porphyry Porphyry in Qingcaoshan Porphyry Copper-Gold Deposit, Tibet[J]. Acta Petrologica Sinica,2013, 29(11):3755-3766.
[82] Clemens J D,Vielzeuf D. Constraints on Melting and Magma Production in the Crust[J]. Earthand Planetary Science Letters, 1987, 86(2/3/4):287-306.
[83] Vielzeuf,Holloway. Experimental Determination of the Fluid-Absent Melting Relations in the Pelitic System[J]. Contributions to Mineralogy and Petrology, 1988, 98(3):257-276.
[84] 龙天祥, 何小虎, 刘飞, 等. 长安金矿区碱性岩锆石U-Pb年代学、微量元素、Hf同位素特征及其地质意义[J]. 吉林大学学报(地球科学版), 2019, 49(6):1607-1627. Long Tianxiang, He Xiaohu, Liu Fei, et al. Zircon U-Pb Geochronology, Trace Element, Hf Isotope of Alkaline Rocks from Chang'an Gold Deposit and Its Geological Implication[J]. Journal of Jilin University(Earth Science Edition), 2019, 49(6):1607-1627.
[85] 王德滋,刘昌实,沈渭洲,等.桐庐I和相山S型两类碎斑熔岩对比[J].岩石学报,1993,9(1):44-54. Wang Dezi, Liu Changshi, Shen Weizhou, et al. The Contrast Between Tonglu I-Type and Xiangshan S-Type Clastoporphyritic Lava[J]. Acta Petrologica Sinica, 1993, 9(1):44-54.
[86] 任纪舜.论中国南部的大地构造[J].地质学报, 1990,64(4):275-288. Ren Jishun. On the Geotectonics of Southern China[J]. Acta Geologica Sinica, 1990, 64(4):275-288.
[87] 舒良树.华南前泥盆纪构造演化:从华夏地块到加里东期造山带[J].高校地质学报, 2006, 12(4):418-431. Shu Liangshu. Predevonian Tectonic Evolution of South China:From Cathaysian Block to Caledonian Period Folded Orogenic Belt[J]. Geological Journal of China Universities, 2006, 12(4):418-431.
[88] Li Zhengxiang, Li Xianhua, Wartho J A, et al. Magmatic and Metamorphic Events During the Early Paleozoic Wuyi-Yunkai Orogeny, Southeastern South China:New Age Constraints and Pressure-Temperature Conditions[J]. Geological Society of America Bulletin, 2010, 122(5/6):772-793.
[89] 张岳桥,董树文,李建华,等.华南中生代大地构造研究新进展[J].地球学报,2012, 33(3):257-279. Zhang Yueqiao, Dong Shuwen, Li Jianhua,et al. New Advances in Mesozoic Tectonic Studies in South China[J]. Acta Geoscientica Sinica, 2012, 33(3):257-279.
[1] 赵亚云, 刘晓峰, 刘远超, 次琼, 郑常云, 杨春四, 李莉, 付海龙. 西藏昂仁县多仁则—桑阿卡地区铜多金属矿点含矿岩体成因及成矿意义[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1323-1339.
[2] 孙海瑞, 吕志成, 于晓飞, 李永胜, 杜泽忠, 吕鑫, 公凡影. 甘肃柳园地区早二叠世正长花岗斑岩脉锆石U-Pb年代学、岩石地球化学特征——对北山造山带晚古生代构造背景的指示[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1433-1449.
[3] 程家龙, 崔子良, 李俊. 云南省保山市西邑大型铅锌隐伏矿床找矿预测地质模型[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1450-1461.
[4] 贺根文, 路思明, 彭琳琳, 于长琦, 李伟, 刘翠辉. 赣南狮吼山硫铁多金属矿区花岗岩地球化学、年代学特征及其成因[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1491-1504.
[5] 余振东, 项新葵, 谭荣, 孙德明, 张斯. 赣北大湖塘平苗矿段白云母花岗岩锆石U-Pb年代学、地球化学及地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1505-1517.
[6] 翁望飞, 王德恩, 胡召齐, 朱强, 汪启年, 吴冀明, 唐国强, 张鹏飞. 安徽省休宁—歙县整装勘查区晚侏罗世逆冲推覆构造特征及其与成矿作用关系[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1518-1538.
[7] 余长胜, 杨言辰, 韩世炯, 杨昆林, 宋朝阳, 张易航, 王旺. 大兴安岭下嘎来奥伊铅锌矿床钾长花岗岩的岩石成因及地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(4): 1042-1058.
[8] 蔡永丰, 刘风雷, 冯佐海, 周云, 曾长育. 桂东北姑婆山岩体矿物学和年代学特征及其成岩成矿意义[J]. 吉林大学学报(地球科学版), 2020, 50(3): 842-856.
[9] 陈会军, 于宏斌, 马永非, 陈井胜, 钱程, 刘世伟, 崔天日, 钟辉. 吉东南地区五女峰岩体锆石U-Pb年代学、岩石地球化学特征及其构造意义[J]. 吉林大学学报(地球科学版), 2020, 50(2): 531-541.
[10] 周传芳, 杨华本, 李向文, 刘玉, 刘涛, 陈卓, 蔡艳龙, 刘宁波, 王博超, 王大可. 大兴安岭北段新林地区晚石炭世花岗岩的岩石成因及地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(1): 97-111.
[11] 杨小鹏, 王长兵, 李文庆. 大兴安岭北段索图罕地区碱长花岗岩成因及形成构造背景[J]. 吉林大学学报(地球科学版), 2019, 49(5): 1338-1349.
[12] 鲁倩, 孙景贵, 安久海, 韩吉龙, 褚小磊. 吉林敦化松江河地区中生代似斑状花岗岩成因和形成环境:元素、Hf同位素和锆石U-Pb年代学证据[J]. 吉林大学学报(地球科学版), 2019, 49(3): 673-689.
[13] 尹志刚, 李海娜, 张海, 郝科, 庞学昌, 宫兆民, 李敏, 张圣听. 大兴安岭加格达奇东北部花岗岩类形成时代、地球化学特征及成因[J]. 吉林大学学报(地球科学版), 2018, 48(6): 1741-1755.
[14] 梁生贤. 互相关系数自约束的重力三维反演与高效求解[J]. 吉林大学学报(地球科学版), 2018, 48(5): 1473-1482.
[15] 高飞, 刘永江, 温泉波, 李伟民, 冯志强, 范文亮, 汤超. 内蒙古突泉—科尔沁右翼中旗地区中生代花岗岩锆石U-Pb年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2018, 48(3): 769-783.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发