刘兵, 李小军, 关奇, 陈棵, 陈光艳, 李维科, 胡绍斌, 张虎, 俞赛赢. 2018: 滇东南富宁地区基性侵入岩及喷出岩时代. 地质通报, 37(11): 2021-2031.
    引用本文: 刘兵, 李小军, 关奇, 陈棵, 陈光艳, 李维科, 胡绍斌, 张虎, 俞赛赢. 2018: 滇东南富宁地区基性侵入岩及喷出岩时代. 地质通报, 37(11): 2021-2031.
    LIU Bing, LI Xiaojun, GUAN Qi, CHEN Ke, CHEN Guangyan, LI Weike, HU Shaobin, ZHANG Hu, YU Saiying. 2018: The age of basic intrusive and extrusive rocks in Funing area, southeast Yunnan Province. Geological Bulletin of China, 37(11): 2021-2031.
    Citation: LIU Bing, LI Xiaojun, GUAN Qi, CHEN Ke, CHEN Guangyan, LI Weike, HU Shaobin, ZHANG Hu, YU Saiying. 2018: The age of basic intrusive and extrusive rocks in Funing area, southeast Yunnan Province. Geological Bulletin of China, 37(11): 2021-2031.

    滇东南富宁地区基性侵入岩及喷出岩时代

    The age of basic intrusive and extrusive rocks in Funing area, southeast Yunnan Province

    • 摘要: 在滇东南富宁地区基性侵入岩、喷出岩较发育,前人将其划分为"半瓦型"侵入岩、"安定型"侵入岩和"龙康型"喷出岩3类,3类岩石普遍缺乏可靠的同位素年代学资料。在对富宁地区基性侵入岩、喷出岩进行区域地质调查的基础上,应用LA-ICP-MS技术对其进行锆石U-Pb测年,在半瓦型侵入岩和安定型侵入岩中分别获得了254.0±2.0Ma和244.2±4.4Ma的加权平均年龄,在龙康型喷出岩中获得251.9±3.0Ma和255.92±0.72Ma加权平均年龄。结合野外调查和综合研究,将富宁地区"安定型"侵入岩的时代界定于中三叠世,将"半瓦型"侵入岩和"龙康型"喷出岩的时代界定于晚二叠世。

       

      Abstract: Basic rocks composed of Banwa-type intrusive rocks, Anding-type intrusive rocks and Longkang-type extrusive rocks are well outcropped in Funing area, southeast Yunnan Province, but they lacked chronological information. Based on regional geological investigation in Funing area, the authors applied LA-ICP-MS tech to determining the U-Pb age of zircons from intrusive and extrusive basic rocks. The weighted averages of 254.0±2.0Ma and 244.2±4.4Ma were obtained from Banwa-type intrusive rocks and Anding-type intrusive rocks respectively, and the weighted averages of 251.9±3.0Ma and 255.92±0.72Ma were obtained from Longkang-type extrusive rocks. Combined with field geological survey and comprehensive research, the authors hold that the age of the Anding-type intrusive rocks should be Middle Triassic, and the age of the Banwa-type intrusive rocks and the Longkang-type extrusive rocks should be Late Permian.

       

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