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滇西点苍山-哀牢山变质岩系变质时限研究
引用本文:李宝龙,季建清,付孝悦,龚俊峰,宋彪,庆建春,张臣,马宗晋.滇西点苍山-哀牢山变质岩系变质时限研究[J].岩石学报,2009,25(3):595-608.
作者姓名:李宝龙  季建清  付孝悦  龚俊峰  宋彪  庆建春  张臣  马宗晋
作者单位:1. 北京大学地球与空间科学学院,造山带与地壳演化教育部重点实验室,北京,100871
2. 中国石化勘探南方分公司,成都,610041
3. 北京离子探针中心,中国地质科学院地质研究所,北京,100037
基金项目:国家自然科学基金项目(40472100)和自然科学基金创新群体项目(40821002)
摘    要:点苍山-哀牢山变质带沿红河-哀牢山走滑剪切带呈北西-南东向展布,其主体由下元古界苍山群和哀牢山群深变质岩系组成,是滇西最显著的带状变质带之一。点苍山-哀牢山变质带的变质时限和山脉隆升时限由于缺乏精确年代学数据制约,一直存在不同认识。本文选取点苍山花岗闪长质糜棱岩(DCS-1),哀牢山墨江-元江段黑云母花岗闪长质片麻岩(SM07-1)和其侵位的同变形花岗岩脉(SM07-3)以及元江县城西北山前花岗质片麻岩(YJ)作为研究对象,并挑选出锆石颗粒(SM07-3)、黑云母(SM07-1-Bi,SM07-3-Bi)、白云母(SM07-1-Ms)、钾长石(DCS-1-Kf, SM07-3-Kf)和斜长石(YJ-Pl)以及基质(YJ-ma)进行精确年代学测试。花岗岩脉颗粒锆石U-Pb SHRIMP 加权平均年龄为30.8±0.3Ma(SM07-3, MSWD=3.27);其它单矿物激光40Ar/39Ar等时线年龄分别为13.1±1.5Ma (DCS-1-Kf, MSWD=2.9)、22.3±0.9Ma (SM07-1-Ms, MSWD=1.7)、21.9±0.7Ma (SM07-1-Bi, MSWD=1.3)、21.3±0.7Ma (SM07-3-Kf, MSWD=1.2)、22.7±0.8Ma (SM07-3-Bi, MSWD=2.4)、19.8±1.6Ma (YJ-ma, MSWD=19)和21.57±0.38Ma (YJ-Pl, MSWD=1.5)。结合区域地质背景、地质演化、野外观察和年代学资料,本文研究认为点苍山-哀牢山变质带的峰期变质变形时间为30Ma左右,此时山脉已开始隆升,在约20Ma和13Ma山脉分别经历一期构造热事件作用,揭示山脉经历快速隆升和冷却过程。

关 键 词:渐新世  变质变形作用  地质年代学  点苍山-哀牢山
收稿时间:2008/12/19 0:00:00
修稿时间:2/6/2009 12:00:00 AM

Metamorphic time limits'study on the metamorphic rocks series of Ailao Shan-Diancang Mountain Ranges,west Yunnan
LI BaoLong,JI JianQing,FU XiaoYue,GONG JunFeng,SONG Biao,QING JianChun,ZHANG Chen and MA ZongJin.Metamorphic time limits'study on the metamorphic rocks series of Ailao Shan-Diancang Mountain Ranges,west Yunnan[J].Acta Petrologica Sinica,2009,25(3):595-608.
Authors:LI BaoLong  JI JianQing  FU XiaoYue  GONG JunFeng  SONG Biao  QING JianChun  ZHANG Chen and MA ZongJin
Institution:Laboratory of Orogenic and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Laboratory of Orogenic and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Southern Exploration Division Company, SINOPEC, Chengdu 610041, China;Laboratory of Orogenic and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Beijing SHRIMP Center, Institute of Geology, Beijing 100037, China;Laboratory of Orogenic and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Laboratory of Orogenic and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Laboratory of Orogenic and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China
Abstract:
Keywords:Oligocene  Metamorphism and deformation  Geochronology  Ailao Shan-Diancang Mountain Ranges
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