supported by the National Natural Science Foundation of China(Nos.42174063,92155307,41976046);Guangdong Provincial Key Laboratory of Geophysical High-resolution Imaging Technology under(No.2022B1212010002);Project for introduced Talents Team of Southern Marine Science and Engineering Guangdong(Guangzhou)(No.GML2019ZD0203)。
Existing lithospheric velocity models exhibit similar structures typically associated with the first-order tectonic features,with dissimilarities due to different data and methods used in model generation.The quantifi...
This work is supported by the Special Fund of the Institute of Geophysics;China Earthquake Administration(No.DQJB20K31);the National Key R&D Program of China(Nos.2018YFC0603502 and2017YFC1500503);the National Natural Science Foundation of China(Nos.41774090 and U1939205);financial support by China Postdoctoral Science Foundation(No.2018M641424)。
The western China lies in the convergence zone between Eurasian and Indian plates.It is an ideal place to study the lithosphere dynamics and tectonic evolutions on the continental Earth.The lithospheric strength is a ...
A global cross-section of the Earth parallel to the tectonic equator(TE) path,the great circle representing the equator of net lithosphere rotation,shows a difference in shear wave velocities between the western and...
supported by the Fundamental Research Funds for the Central Universities (Grant Nos. 2652013021 and2010ZD15)
The lithosphere temperature beneath the Tibetan plateau was estimated by local isostasy equilib- rium constrained geothermal calculation. Maps of the lateral temperature variation at depths of 40 km, 70 km, and Moho a...
There have been reports for many years that the ionosphere is very sensitive to seismic effects, and the detection of ionospheric perturbations associated with earthquakes (EQs) attracts a lot of attention as a very...
funded by National Key Technology R&D Program in the 11th Five Year Plan of China (2008BAC35B00);the international cooperation project(2009DFA21480)
Based on the case studies and statistical analysis of earthquake-related ionospheric disturbances mainly from DEMETER satellite, ground-based GPS and ionosounding data, this paper summarizes the statisw tical characte...
There are some factors, such as the topographic relief, sedimentary thickness and thermal conductivity, magmatic activity and thermal cooling, influencing the seafloor heat flow and the evolution of lithosphere struct...
Financial supports for this study were provided by the National Natural Science Foundation of China granted No.41076019;the Program 973 through grant 2007CB411702;supported by the Shanghai Pujiang Program;the Innovation Program of Shanghai Municipal Education Commission
We propose a novel seismic tomography method, Source Side Seismic Tomography (3STomo), which is designed particularly to image the subsurface structure beneath seismically active regions. Unlike the teleseismic tomo...
The Development Program on National Key Basic Researches under the Project Mechanism and Prediction of Continental Strong Earthquakes (G19980407).
The India plates continuous motion to the north, the convective removal to the thickening lithosphere caused by small-scale mantle convection and the effect of denudation on the uplifted plateau are regarded as main d...
The numerical dynamic model of Chinese mainland lithosphere's stress and strain field was constructed withelasto-viscous creep constitive relation. The most recent data of the stress field of Chinese mainland and theh...