青藏高原新特提斯蛇绿岩的地质特征及其构造演化

刘飞, 杨经绥, 连东洋, 李观龙. 2020. 青藏高原新特提斯蛇绿岩的地质特征及其构造演化. 岩石学报, 36(10): 2913-2945. doi: 10.18654/1000-0569/2020.10.01
引用本文: 刘飞, 杨经绥, 连东洋, 李观龙. 2020. 青藏高原新特提斯蛇绿岩的地质特征及其构造演化. 岩石学报, 36(10): 2913-2945. doi: 10.18654/1000-0569/2020.10.01
LIU Fei, YANG JingSui, LIAN DongYang, LI GuanLong. 2020. Geological features of Neothyan ophiolites in Tibetan Plateau and its tectonic evolution. Acta Petrologica Sinica, 36(10): 2913-2945. doi: 10.18654/1000-0569/2020.10.01
Citation: LIU Fei, YANG JingSui, LIAN DongYang, LI GuanLong. 2020. Geological features of Neothyan ophiolites in Tibetan Plateau and its tectonic evolution. Acta Petrologica Sinica, 36(10): 2913-2945. doi: 10.18654/1000-0569/2020.10.01

青藏高原新特提斯蛇绿岩的地质特征及其构造演化

  • 基金项目:

    本文受南方海洋科学与工程广东省实验室(广州)人才团队引进重大专项(GML2019ZD0201)、中国地质调查局地质调查项目(DD20190060)、国家自然科学基金项目(41720104009)、山东地勘局七队合作项目(QDKY202007)和深地动力学自然资源部重点实验室自主基金项目(J1901-15)联合资助

详细信息
    作者简介:

    刘飞, 男, 1982年生, 博士, 构造地质学专业, E-mail:lfhy112@126.com

  • 中图分类号: P541

Geological features of Neothyan ophiolites in Tibetan Plateau and its tectonic evolution

  • 西藏雅鲁藏布江缝合带(YZSZ)和班公湖-怒江缝合带(BNSZ)蛇绿岩代表了新特提斯洋壳和岩石圈地幔残余,是我国铬铁矿和蛇绿岩型金刚石的重要原产地,目前这两条蛇绿岩带的成因和相互关系还存在着争论。本文总结了YZSZ、BNSZ、狮泉河-纳木错蛇绿混杂岩带(SNMZ)和松多缝合带蛇绿岩的时空分布、组成和构造背景,归纳了拉萨地块晚古生以来的岩浆岩分布,获得以下主要认识:(1)Panjal地幔柱活动可能促使怒江洋和雅江西洋在早二叠世空谷期(283~272Ma)打开;(2)雅江东洋由于松多洋的南向俯冲在晚三叠世打开,与雅江西洋以萨嘎-措勤为界,并形成冈底斯东部245~200Ma岩浆热事件;(3)~140Ma班怒洋闭合以及南羌塘与北拉萨地块碰撞,导致雅江洋扩张速率加快而引发了北向拉萨地块的平板俯冲,进而导致班怒洋的再次裂解形成133~104Ma"红海型"小洋盆;(4)YZSZ缝合带西段南带蛇绿岩为北带的逆冲推覆体;(5)BNSZ和SNMZ蛇绿岩隶属于一个洋盆,后者代表了班怒洋成熟洋盆扩张脊的残余。

  • 加载中
  • 图 1 

    特提斯造山带中已发现蛇绿岩型金刚石的位置分布图

    Figure 1. 

    Distribution map of ophiolite-type diamonds discovered from chromitite and peridotite along Tethyan orogenic belt

    图 2 

    雅鲁藏布江缝合带、班公湖-怒江缝合带和狮泉河-纳木错混杂岩带中蛇绿岩分布简图

    Figure 2. 

    Tectonic outline of the Tibetan Plateau showing the distribution of ophiolites in Yarlung Zangbo Suture Zone (YZSZ), Bangong-Nujiang Suture Zone (BNSZ) and Shiquan River-Namtso Mélange Zone (SNMZ)

    图 3 

    西藏南部雅鲁藏布江缝合带、班公湖-怒江缝合带、狮泉河-纳木错蛇绿混杂岩带和松多缝合带分布简图(a)及雅鲁藏布江缝合带西段区域地质图(b)

    Figure 3. 

    Ophiolites distribution along the YZSZ, BNSZ, SNMZ and SS (a) and simplified geological map of the western part of the YZSZ (b) in South Tibet

    图 4 

    雅鲁藏布江缝合带主要蛇绿岩的岩性柱状图

    Figure 4. 

    Synthetic stratigraphic-lithological columnar sections of ophiolites in the YZSZ

    图 5 

    雅鲁藏布江缝合带、班公湖-怒江缝合带、狮泉河-纳木错蛇绿混杂岩带和松多缝合带蛇绿岩年龄分布简图

    Figure 5. 

    Geological sketches of the YZSZ, BNSZ, SNMZ and SS showing ages of the ophiolitic massifs

    图 6 

    班公湖-怒江缝合带、狮泉河-纳木错混杂带和松多缝合带中主要蛇绿岩的岩性柱状图

    Figure 6. 

    Synthetic stratigraphic-lithological columnar sections of main ophiolites in the BN, SN and SS

    图 7 

    拉萨地块及两侧岩浆岩分布简图(据Liu et al., 2017c修改)

    Figure 7. 

    Schematic geological map showing the distribution of magmatic rocks within and both sides of the Lhasa block (modified after Liu et al., 2017c)

    图 8 

    青藏高原新特提斯洋构造演化模式图

    Figure 8. 

    Tectonic reconstruction of the Neotethyan ocean evolution in Tibetan Plateau

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出版历程
收稿日期:  2020-05-20
修回日期:  2020-08-14
刊出日期:  2020-10-01

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