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)

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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
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