supported by the National Key Research and Development Program of China(Grant No.2023YFF0803304);the National Natural Science Foundation of China(Grant Nos.41825006&41590623)。
As the most seismically active regions in the world,oceanic subduction zones show contrasting seismicity in different regions.To investigate the relationships among the thermal structure,metamorphism,deformation,and f...
supported by the National Natural Science Foundation of China (Grant Nos. 42249583, 92258303);the Laoshan Laboratory。
1. Introduction The oldest oceanic crust with ages up to 200 Ma, is subducting along the West Pacific Convergent margin. Interestingly, it is right next to a Cenozoic microplate, the Caroline Plate. The Mussau Trench ...
supported by the National Natural Science Foundation of China(Grant Nos.92258303&42221005);the Marine S&T Fund of Shandong Province for The Laoshan Laboratory(Grant No.LSKJ202204100);the Major Basic Research Project of Shandong Province(Grant No.ZFJH202308);the Taishan Scholar Program of Shandong(Grant No.tspd20230609)。
The proto-atmosphere serves as a crucial starting point for the carbon cycle.Estimations based on atmospheric data from Mars and Venus suggest that Earth's proto-atmosphere contained>110 bar of CO_(2)and>2.6 bar of ni...
The research paper"Geodynamic processes of the southeastern Neo-Tethys Ocean and the formation mechanism of the curved subduction system in Southeast Asia"(Sci China Earth Sci,2023,66:703-717)contained errors.The corr...
funded by the National Natural Science Foundation of China(Grant Nos.42073029,42273043);the Fundamental Research Funds for the Central Universities。
1.Fluid metasomatism in subduction zones Subduction zones are the key tectonic setting that links Earth's surficial sphere to deep sphere(Zheng and Chen,2016).Fluid action occurring in subduction zones is closely rela...
a review of the geodynamic studies and extended thoughts during the past four years (2019–2022)in the platform of“Major Research Plan on Tethys Geodynamic System”funded by the National Natural Science Foundation of China (Grant No.91855208);supported by the National Natural Science Fundation of China for Distinguished Young Scholars (Grant No.42225403)。
Tethys tectonic system has experienced a long-term evolution history,including multiple Wilson cycles;thus,it is an ideal target for analyzing plate tectonics and geodynamics.Tethyan evolution is typically characteriz...
supported by the National Natural Science Foundation of China(Grant Nos.91755215,42230311,41930112,41902068);the China Geological Survey Project(Grant No.DD20221661).
The geometry and deformation of the Indian continental mantle lithosphere(ICML)beneath the India-Eurasia collision zone are critical to understanding the accommodation of continent-continent convergence.In this paper,...
financially supported by the National Natural Science Foundation of China(Grant No.42072061)。
1.Introduction The oceanic arc basalts and continental arc andesites are typical products of subduction zone magmatism(Straub et al.,2011;Zheng et al.,2020).However,there has been controversy over the lithology of the...
supported by the National Natural Science Foundation of China(Grant Nos.42230303,41504076,41874125);the China Geological Survey Project(Grant No.DD20190010);the Fundamental Research Funds for the Central Universities(Grant No.JLUXKJC2021ZZ11).
The Jiamusi and Songnen blocks converged in the easternmost segment of the Central Asian Orogenic Belt as a result of the subduction and subsequent closure of the Mudanjiang oceanic plate during the Permian-Jurassic.T...
supported by the National Natural Science Foundation of China(Grant Nos.42025601,41890811&92155203)。
Southeast Asia is located at the intersection of the Tethys and Pacific domains. The superimposed effects of the two tectonic domains have resulted in complicated deep structure, surface magma responses, and dynamic p...