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李孟奎博士一篇论文获被引次数最多奖

时间:2019-03-21 来源:未知 点击:

李孟奎博士的论文奖

日前,李孟奎博士的一篇论文“Crustal and upper-mantle structure of the southeastern Tibetan Plateau from joint analysis of surfacewave dispersion and receiver functions”被亚洲地球科学杂志评为被引次数最多奖。

该论文信息:
Crustal and upper-mantle structure of the southeastern Tibetan Plateau from joint analysis of surfacewave dispersion and receiver functions

作者:Li, MK (Li, Mengkui)1 ] Zhang, SX (Zhang, Shuangxi)1,2,3 ] Wang, F (Wang, Fang)1 ] Wu, TF (Wu, Tengfei)1 ] Qin, WB (Qin, Weibing)1 ]

JOURNAL OF ASIAN EARTH SCIENCES

卷: 117

 

页: 52-63

DOI: 10.1016/j.jseaes.2015.12.002

出版年: MAR 1 2016

文献类型:Article


摘要

Researches on the southeastern Tibetan Plateau provide important insights into the tectonic evolution of the Tibetan Plateau. In this study, we have constructed a high-resolution 3D shear-wave velocity model through joint inversion of receiver functions and surface wave dispersion data. The crustalthickness and Poisson's ratio models are first determined by H-k stacking of receiver functionsThe crustal thickness changes from 30 km in the south to 62 km in the north, presenting strong lateral variations. The fundamental mode of Rayleigh wave dispersion data spanning periods from 8 to 65 s were then jointly used to constraint the absolute shear-wave velocity. The shear-wave velocity structure shows lateral variations. There are low velocity zones distributed in the crust and upper mantle. Two continuously distributed low velocity zones are clearly presented in the middle-to-lower crust, which extend from north toward southeast and southwest, respectively, joining together in southern Yunnan. In this study, we deduced the migration model of soft materials in middle-to-lower crust in southeastern Tibetan Plateau, which explains that the resistance from Sichuan Basin separates the flowing materials from Tibetan Plateau into southeast and northwest branches. They flow along the west margin of Sichuan Basin and then extrude out from northeastern and southeastern Tibetan Plateau respectively. The southeast branch is blocked and cannot flow in the entire crust. It is limited in a certain range of depths and channels. The two low velocity zones in this study possibly present two flow channels of the middle-to-lower crustal materials extruded from the TibetanPlateau. (C) 2015 Elsevier Ltd. All rights reserved.

基金资助致谢
基金资助机构 授权号
973 Project of China 
2013CB733303 
National Natural Science Foundation of China 
41474093