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北京昌平地区基底片麻岩和中-新元古代盖层锆石U-Pb年龄和Hf同位素研究及其地质意义
引用本文:任荣,韩宝福,张志诚,李建锋,杨岳衡,张艳斌.北京昌平地区基底片麻岩和中-新元古代盖层锆石U-Pb年龄和Hf同位素研究及其地质意义[J].岩石学报,2011,27(6):1721-1745.
作者姓名:任荣  韩宝福  张志诚  李建锋  杨岳衡  张艳斌
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. 中国科学院地质与地球物理研究所岩石圈演化国家重点实验室,北京,100029
基金项目:本文受国家自然科学基金项目(J0730533)资助.
摘    要:本文通过对北京昌平地区燕辽裂陷槽内出露的基底密云群片麻岩及其上覆沉积盖层底部长城系常州沟组和顶部青白口系长龙山组砂岩的锆石LA-ICP-MS U-Pb年龄和Hf同位素组成的研究,对华北克拉通新太古代-元古宙期间的沉积与地壳演化进行探讨.锆石的LA-ICP-MS U-Pb年代学研究表明,密云群含辉石角闪斜长片麻岩的原岩形...

关 键 词:华北克拉通  前寒武纪  燕辽裂陷槽  碎屑锆石  沉积与地壳演化
收稿时间:2010/7/14 0:00:00
修稿时间:2011/3/11 0:00:00

Zircon U-Pb and Hf isotopic studies of basement gneiss and overlying Meso-Neoproterozoic sedimentary rocks from the Changping area, Beijing, and their geological implications
REN Rong,HAN BaoFu,ZHANG ZhiCheng,LI JianFeng,YANG YueHeng and ZHANG YanBin.Zircon U-Pb and Hf isotopic studies of basement gneiss and overlying Meso-Neoproterozoic sedimentary rocks from the Changping area, Beijing, and their geological implications[J].Acta Petrologica Sinica,2011,27(6):1721-1745.
Authors:REN Rong  HAN BaoFu  ZHANG ZhiCheng  LI JianFeng  YANG YueHeng and ZHANG YanBin
Institution:Key Laboratory of Orogenic belts and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic belts and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic belts and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic belts and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing 100871, China;State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Abstract:Zircon LA-ICP-MS U-Pb and Hf isotopic studies of the Neoarchean basement gneiss of the Miyun Group and overlying Meso-Neoproterozoic sandstones of the Changzhougou Formation of the Changcheng System and Changlongshan Formation of the Qingbaikou System from the Yan-Liao aulacogen in the Changping area,Beijing,are carried out in order to investigate the sedimentary and crustal evolution of the North China Craton (NCC).Zircon U-Pb dating on a pyroxene-bearing hornblende-plagioclase gneiss yields a protolith ag...
Keywords:North China Craton  Precambrian  Yan-Liao aulacogen  Detrital zircon  Sedimentary and crustal evolution
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