刘巍^1,,
郭震^2,3,
陈永顺^2,3,,,
张安琪²
1. 北京大学地球与空间科学学院理论与应用地球物理研究所, 北京 100871
2. 南方科技大学海洋科学与工程系, 深圳 518055
3. 上海佘山地球物理国家野外科学观测研究站, 上海 201602

基金项目: 国家自然科学基金委重点项目（41890814，U1901602），国土资源部行业调查项目子课题"秦岭及周边地区三维地壳和岩石圈结构探测"（1212011220261）和深圳市海外高层次人才创新创业专项资金团队资助项目（KQTD20170810111725321）资助


详细信息

作者简介: 刘巍, 男, 1990年生, 北京大学博士研究生, 主要研究方向为地球动力学、地震学成像.E-mail: 1701110588@pku.edu.cn

通讯作者: 陈永顺, 男, 教授, 博士生导师, 主要从事全球板块构造、海洋地球物理学和地球动力学方面的研究.E-mail: johnyc@sustech.edu.cn

中图分类号: P313

收稿日期:2020-10-27
修回日期:2021-07-08
上线日期:2021-09-10

The crustal and uppermost mantle structure of the Qinling-Tongbai-Dabie orogenic belt from integrated geophysical observations

LIU Wei^1,,
GUO Zhen^2,3,
CHEN YongShun^2,3,,,
ZHANG AnQi²
1. Institute of Theoretical and Applied Geophysics, School of Earth and Space Sciences, Peking University, Beijing 100871, China
2. Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China
3. Shanghai Sheshan National Geophysical Observatory, Shanghai 201602, China


More Information

Corresponding author: CHEN YongShun,E-mail:johnyc@sustech.edu.cn

MSC: P313

--> Received Date: 27 October 2020
Revised Date: 08 July 2021
Available Online: 10 September 2021


摘要
摘要:秦岭—桐柏—大别复合造山带（以下称为秦岭大别造山带）属于中国中央造山带的一部分，由华北克拉通与扬子克拉通汇聚形成.对于秦岭大别造山带及其周缘地区的研究，可以为这一大陆碰撞造山带的形成与演化过程提供重要信息.本文整合研究区域的接收函数与背景噪声数据，采用H-κ叠加分析、接收函数与背景噪声联合反演、克希霍夫偏移成像等方法，得到了沿秦岭东西方向具有高分辨率的地壳及上地幔结构.研究结果显示：（1）莫霍面深度由西向东逐步抬升，由剖面西侧最深约55 km上升至剖面东侧最浅约30 km；莫霍面于东西秦岭之间起伏明显；桐柏以及东大别下方莫霍面局部加深.（2）西秦岭中下地壳观测到的高速异常阻隔了青藏高原东北缘地壳低速异常的向东扩张，反映了青藏高原东北缘的中下地壳流没有通过西秦岭继续向东流动.（3）西秦岭岩石圈地幔顶部高速异常延伸至100 km深度（剖面底部），桐柏—西大别岩石圈地幔顶部高速延伸至70 km深度，东大别、东秦岭岩石圈地幔顶部未见较大深度范围的高速异常.
关键词: 秦岭大别造山带/
接收函数/
克希霍夫偏移成像/
H-κ叠加/
联合反演/
地壳以及上地幔结构

Abstract:The Qinling-Tongbai-Dabie orogenic belt (QD)is the important element of the China Central Orogenic Systems, which was formed by the convergence of the North China Craton and the Yangtze Craton. Due to its key position in the Central Orogenic Systems, the QD is an ideal place to study the orogenic processes between collided continents. To reveal the fine crustal and uppermost mantle structure with high resolution beneath the QD and surrounding areas, this work integrates seismic data available around the QD, which consist of raw seismic data, ambient noise data, and receiver function data. We adopted the Kirchhoff migration method to obtain a preliminary image of the Moho, used the H-κ analysis to calculate the crustal thickness and V_P/V_S, and utilized a joint inversion of ambient noise and receiver functions to construct a high resolution V_S velocity model beneath the QD. Finally, we obtained a profile crossing the QD from west to east with detailed structures in the crust and uppermost mantle. The results reveal that: (1) Moho depth gradually becomes shallower from west to east, from the deepest about 55 km in the west to the shallowest about 30 km in the east of the profile.(2) The high velocity anomaly in the middle and lower crust of the West Qinling blocks the eastward expansion of the low velocity anomaly in the crust of the Northeast Tibetan Plateau, which provides unambiguous evidence that the crustal ductile flow within the Northeast Tibetan Plateau does not continue to flow eastward through the West Qinling.(3) In the uppermost mantle, the West Qinling is underlain by high velocity down to at least 100 km depth, the Tongbai and East Dabie are underlain by high velocity down to 70 km depth, however, the high velocity is not shown beneath East Qinling or East Dabie.
Key words:Qinling-Dabie orogenic belt/
Receiver function/
Kirchhoff migration imaging/
H-κ stacking/
Joint inversion/
Crustal and uppermost mantle structure



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