东昆中构造带沟里地区浅变质地层碎屑锆石UPb年龄及其地质意义

颜全治, 裴先治, 李瑞保, 李佐臣, 裴磊, 刘成军, 陈有炘, 胡晨光, 张玉, 王兴, 彭思钟. 东昆中构造带沟里地区浅变质地层碎屑锆石UPb年龄及其地质意义[J]. 西北地质, 2017, 50(1): 165-181.
引用本文: 颜全治, 裴先治, 李瑞保, 李佐臣, 裴磊, 刘成军, 陈有炘, 胡晨光, 张玉, 王兴, 彭思钟. 东昆中构造带沟里地区浅变质地层碎屑锆石UPb年龄及其地质意义[J]. 西北地质, 2017, 50(1): 165-181.
YAN Quanzhi, PEI Xianzhi, LI Ruibao, LI Zuochen, PEI Lei, LIU Chengjun, CHEN Youxin, HU Chenguang, ZHANG Yu, WANG Xing, PENG Sizhong. Detrital Zircon U-Pb Age and Geological Significance of Metamorphic Strata at Gouli Area in the Central Tectonic Belt of East Kunlun[J]. Northwestern Geology, 2017, 50(1): 165-181.
Citation: YAN Quanzhi, PEI Xianzhi, LI Ruibao, LI Zuochen, PEI Lei, LIU Chengjun, CHEN Youxin, HU Chenguang, ZHANG Yu, WANG Xing, PENG Sizhong. Detrital Zircon U-Pb Age and Geological Significance of Metamorphic Strata at Gouli Area in the Central Tectonic Belt of East Kunlun[J]. Northwestern Geology, 2017, 50(1): 165-181.

东昆中构造带沟里地区浅变质地层碎屑锆石UPb年龄及其地质意义

  • 基金项目: 国家自然科学基金项目(41472191、41502191、41172186),中央高校基本科研业务费专项资金项目(CHD2011TD020、2013G1271091、2013G1271092、310827161002、310827161006)和青海省国土资源厅-中国铝业公司公益性区域地质矿产调查基金项目(中铝基金200801)

Detrital Zircon U-Pb Age and Geological Significance of Metamorphic Strata at Gouli Area in the Central Tectonic Belt of East Kunlun

  • 东昆中构造带具有复杂的物质组成与结构构造,其中沟里地区出露的原划石炭系浅变质沉积地层是东昆中蛇绿构造混杂岩基质岩系的重要组成部分,其形成时代和属性研究对东昆中构造带研究具有重要意义。运用LA-MC-ICP-MS锆石U-Pb年代学分析方法,对浅变质沉积地层变砂岩碎屑锆石进行详细研究,结果显示,碎屑锆石年龄谱可分为4组:①加里东期(499~565Ma)。②新元古代中期至早期(693~969Ma)。③古元古代晚期-中元古代中期(1 254~1 967Ma)。④新太古代-古元古代早期(2 348~2 776Ma)。结合前人研究资料认为浅变质沉积地层形成时间在427~499Ma,应归属于早古生代纳赤台岩群变沉积岩。其沉积物源以新元古代早期至中期响应Rodinia超大陆汇聚、裂解的物质记录及新太古代-元古代结晶基底为主,少量东昆仑地区加里东期与原特提斯洋扩张俯冲相关岩浆岩。东昆中构造带沟里地区基质地层主要是早古生代纳赤台岩群变沉积岩,而不是前人认为的石炭纪地层。东昆中构造带主要构造活动在早古生代末期就已经基本完成。
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收稿日期:  2016-08-09
修回日期:  2016-11-14
刊出日期:  2017-03-15

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