藏北羌塘早古生代岩浆作用及其地质意义

解超明, 李才, 翟庆国, 刘一鸣, 王明, 胡培远, 范建军. 2021. 藏北羌塘早古生代岩浆作用及其地质意义. 沉积与特提斯地质, 41(2): 340-350. doi: 10.19826/j.cnki.1009-3850.2021.01004
引用本文: 解超明, 李才, 翟庆国, 刘一鸣, 王明, 胡培远, 范建军. 2021. 藏北羌塘早古生代岩浆作用及其地质意义. 沉积与特提斯地质, 41(2): 340-350. doi: 10.19826/j.cnki.1009-3850.2021.01004
XIE Chao-ming, LI Cai, ZHAI Qing-guo, LIU Yi-ming, WANG Ming, HU Pei-yuan, FAN Jian-jun. 2021. The Early Paleozoic magmatism in Qiangtang, northern Tibet and its geological significance. Sedimentary Geology and Tethyan Geology, 41(2): 340-350. doi: 10.19826/j.cnki.1009-3850.2021.01004
Citation: XIE Chao-ming, LI Cai, ZHAI Qing-guo, LIU Yi-ming, WANG Ming, HU Pei-yuan, FAN Jian-jun. 2021. The Early Paleozoic magmatism in Qiangtang, northern Tibet and its geological significance. Sedimentary Geology and Tethyan Geology, 41(2): 340-350. doi: 10.19826/j.cnki.1009-3850.2021.01004

藏北羌塘早古生代岩浆作用及其地质意义

  • 基金项目:

    国家自然科学基金项目(批准号:41872231,41972236);自然资源部东北亚矿产资源评价重点实验室自主课题基金资助(编号:DBY-ZZ-18-06)

详细信息
    作者简介: 解超明(1983—),男,教授,主要从事青藏高原基础地质研究。E-mail:xcmxcm1983@jlu.edu.cn
  • 中图分类号: P588.11+5;P542.5

The Early Paleozoic magmatism in Qiangtang, northern Tibet and its geological significance

  • 藏北羌塘早古生代岩浆作用及其构造演化对研究青藏高原早期演化历史以及羌塘盆地基底性质结构等具有重要科学意义。本文在综述前人研究基础上,系统总结了藏北羌塘地区早古生代岩浆岩的时空分布特征及年代学格架,初步探讨了青藏高原早古生代构造-岩浆事件对冈瓦纳大陆北缘构造演化以及羌塘盆地基底属性的约束。羌塘地区早古生代岩浆岩主要分布在日湾茶卡、都古尔、戈木日、本松错等地区,岩性以变质辉长岩、变质玄武岩、安山岩、花岗岩、变质流纹岩以及花岗片麻岩等为主。基于区域地质调查和年代学研究结果,羌塘地区早古生代发生了多期岩浆作用,分别为~500 Ma、~482 Ma、~474 Ma、~455 Ma、~438 Ma。这些岩浆岩可能是泛非造山运动结束后,冈瓦纳大陆北缘岩石圈伸展减薄的产物,并构成了羌南-保山板块早古生代的结晶基底,但有关伸展减薄的机制问题仍需开展进一步的研究工作,这些地质记录对恢复和反演青藏高原冈瓦纳大陆北缘的陆缘性质具有重要约束意义。
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收稿日期:  2020-12-30
修回日期:  2021-01-18

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