Receiver function structures beneath the Haiyuan fault on the northeastern margin of the Tibetan plateau  

作　　者：Yutao Shi Yuan Gao Laiyu Lu 

机构地区：[1]Institute of Earthquake Forecasting,China Earthquake Administration,Beijing 100036,China [2]Institute of Geophysics,China Earthquake Administration,Beijing 100081,China

出　　处：《Earthquake Science》2021年第4期367-377,共11页地震学报（英文版）

基　　金：supported by National Natural Science foundation of China(Nos.41474032 and U1839209);the Basic Research Project of the Institute of Earthquake Forecasting,China Earthquake Administration(Nos.2019CSES0102 and 2012IES010101).

摘　　要：We performed a receiver function analysis on teleseismic data recorded along two dense seismic profiles and from 4 broadband regional seismic stations across the northeastern Tibetan plateau.The crustal thickness and vP/vS ratio were measured by the H-κdomain search algorithm.The Moho discontinuity across the Haiyuan arc fault zone was also revealed by common conversion point(CCP)imaging.Our study results show that the crustal thickness and the vP/vS ratio were 42–56 km and 1.60–1.88,respectively.The crustal thickening on the northeastern margin indicates that the crust is shortening or that there was a superimposition of crusts during the collision of the Tibetan plateau with Eurasian block.Our results suggest that Haiyuan fault likely resulted from the interactions of high temperature and pressure conditions during the collision of the Indian and Asian continents.The Moho beneath the Haiyuan tectonic region exhibits an obvious offset and a vague discontinuity according to CCP imaging.This study suggests that the Haiyuan arc fault zone is a trans-crustal fault that cuts through the Moho in the northeastern Tibetan Plateau.Moreover,there are indications of strong deformation in the intensive crustal extrusion from the interior of the Tibetan Plateau to its northeastern margin.

关 键 词：Haiyuan fault Receiver function Crustal thickness vP/vS ratio 

分 类 号：P315.2[天文地球—地震学] P542.3[天文地球—固体地球物理学]