武振波^1,,
唐国彬²,
徐涛^2,3,,,
梁春涛^1,4,
翁雪飞¹
1. 成都理工大学地球物理学院, 成都 610059
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
3. 中国科学院青藏高原地球科学卓越创新中心, 北京 100101
4. 成都理工大学, 地球勘探与信息技术教育部重点实验室, 成都 610059

基金项目: 国家自然科学基金（41704042，91755215，41674064）资助


详细信息

作者简介: 武振波, 女, 1988年生, 副教授, 主要从事地震学研究.E-mail:wuzhenbo@cdut.edu.cn

通讯作者: 徐涛, 男, 1978年生, 研究员, 主要从事地震学研究.E-mail:xutao@mail.iggcas.ac.cn

中图分类号: P315;P541

收稿日期:2020-07-04
修回日期:2020-10-09
上线日期:2020-11-05

Eclogitization of Indian lower crust during its northward subduction revealed by receiver function depth migration images

WU ZhenBo^1,,
TANG GuoBin²,
XU Tao^2,3,,,
LIANG ChunTao^1,4,
WENG XueFei¹
1. College of Geophysics, Chengdu University of Technology, Chengdu 610059, China
2. State key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
3. CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China
4. Chengdu University of Technology, Key Laboratory of Earth Exploration and Information Techniques of the China Ministry of Education, Chengdu 610059, China


More Information

Corresponding author: XU Tao,E-mail:xutao@mail.iggcas.ac.cn

MSC: P315;P541

--> Received Date: 04 July 2020
Revised Date: 09 October 2020
Available Online: 05 November 2020


摘要
摘要:印度地壳与岩石圈地幔的俯冲前缘和俯冲形态，对认识高原构造变形、隆升机制有重要意义.本文基于青藏高原西缘分布的流动宽频带地震台站（TW-80测线和Y2台网）记录的远震波形数据，通过接收函数H-κ网格搜索与CCP叠加方法，对研究区地壳结构进行成像.结果显示：（1）研究区西侧北西—南东向剖面（剖面1，2），狮泉河逆冲断裂带以南，深度67~80 km范围内均观测到连续的Moho界面；40~55 km范围内存在另一组横向上可连续追踪的界面，其形态与之下Moho面横向变化趋势近乎平行；（2）研究区东侧剖面3下方，Moho面从南端喀喇昆仑断裂带下方向北逐渐加深，在雅鲁藏布江缝合带附近增至大约67 km，进入拉萨块体至台站WT20和WT03下方至最深75~80 km，然后向北有所抬升.基于成像结果和岩石学研究成果推测藏南块体下方，自西向东均存在俯冲印度板块下地壳的榴辉岩化现象，可以用来指示印度板块地壳尺度的俯冲前缘，其在青藏高原西部（约80°E）位于班公湖—怒江缝合带附近，向东逐步递减至拉萨块体中部.
关键词: 青藏高原/
接收函数/
印度板块俯冲/
榴辉岩化

Abstract:The receiver functions calculated at the broadband seismic stations of TW-80 and Y2 array are used to reveal the main subduction features of the Indian plate beneath western Tibet. The H-κ grid-searching results and CCP depth migration image show that the observed Moho structure at depth 67~80 km is laterally traceable from south to north on the west profiles in the study area, while there is another discontinuity interface at depth 40~55 km almost parallel to the Moho up to the station SQAT nearby the Shiquanhe thrust fault. This feature also can be seen on the CCP migration image on the east profile of the study area. Based on the evidence derived from this and previous petrology studies, we infer that the Indian lower crust front beneath western Tibet is located at Bangonghu-Nujiang suture, while it gradually reduces southward to the internal Lhasa block beneath central and east Tibet.
Key words:Tibetan plateau/
Receiver function/
Northward subducting Indian plate/
Eclogitization



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