benefited from the financial support of the Chinese Academy of Sciences Pioneer Hundred Talents Program;the Second Tibetan Plateau Scientific Expedition and Research Program (Grant No. 2019QZKK0708);the MEXT KAKENHI grant (Grant No. 21H05203);the Kobe University Strategic International Collaborative Research Grant (Type B Fostering Joint Research);the “Science of Slowto-Fast Earthquakes” project。
The dependence of the subduction regime on three-dimensional slab geometry poses a challenge for accurately estimating the evolving thermal structure of megathrusts globally. Although slab dips and ages have gained at...
supported by grants from the National Science Foundation of the USA.
East Asian continental tectonics challenges the plate tectonics paradigm with its diffuse intraplate deformation,magmatism,and earthquakes.Despite extensive studies,fundamental questions persist.This review examines t...
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:42130801,41430211,90814006,and 42072226);the“Deep-time Digital Earth”Science and Technology Leading Talents Team Funds for the Central Universities for the Frontiers Science Center for Deep-time Digital Earth,CUGB(Fundamental Research Funds for the Central Universities;Grant No:2652023001).
How the subduction direction of the Paleo-Pacific plate beneath the Eurasian plate changes in the Early Cretaceous remains highly controversial due to the disappearance of the subducted oceanic plate.Intraplate deform...
supported by Karadeniz Technical University Research Foundation(FBA-2017-7286 and FBA-2023-10635);National Natural Science Foundation of China(42103038);Open Research Project from the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences(GPMR201815).
The Meso-Cenozoic geodynamic evolution of northern Türkiye remains a subject of debate primarily due to a lack of systematic geological,geochemical,geochronological,and geophysical investigations.This paper presents ...
The occurrence of coesite in metamorphic rocks of supracrustal origin demon-strates that the low-density continental crust was subducted to subarc depths for ultrahigh-pressure(UHP)metamorphism[1,2].Thus,the finding o...
Earthquakes pose significant risks globally,necessitating effective seismic risk mitigation strategies like earthquake early warning(EEW)systems.However,developing and optimizing such systems requires thoroughly under...
supported by the National Natural Science Foundation of China(No.41872101);the Graduate Innovation Fund of Jilin University(No.2022046)。
During the Late Paleozoic-Early Mesozoic Era,the sediment transport system and tectonic regime in the southeastern margin of the South China Block(SESCB)all changed,significantly affected by the Paleo-Pacific subducti...
supported by NSFC(42306084);Hunan Provincial Natural Science Foundation of China(2023JJ40223);Scientific Research Fund of Hunan Provincial Education Department(21B0566).
The Sumatra subduction zone is located in the southwest of the Suna plate,between the Euro-Asia Plate and Indo-Austrilian Plates.With the obliquely subducting of the Indo-Austrilian Plate toward the the Euro-Asia Plat...