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 ...
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...
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 Russian Science Foundation(#21-77-20022,stratigraphy,geochronology,geochemistry);Fundamental Research Funds for the Central Universities of China(2682023CX016,paper preparation);Ministry of Science and Higher Education of Russia,State Assignment Projects(122041400044-2 and FSUS-2020-0039)(petrography,isotopes,geodynamic implications).
The Itmurundy Zone of Central Kazakhstan is a key structure in the core of the Kazakh Orocline representing a typical Pacific-type orogenic belt hosting accretionary complex,ophiolite massifs and serpentinite mélange...
funded by the Second Tibetan Plateau Scientific Expedition and Research(STEP)Program(Grant No.2019QZKK0702);National Natural Science Foundation of China(Grant Nos.92055208,42174080);Natural Science Foundation of Guangxi,China(Grant No.AD21220033);Shandong Provincial Natural Science Foundation(Grant No.ZR2020QD045);China Geological Survey(Grant No.DD20190167).
Oceanic plateau accretion and subsequent flat-slab subduction in modern convergent settings have profoundly influenced the nature of subduction and mantle dynamics.However,evaluating similar impacts in ancient converg...
supported by the National Natural Science Foundation of China(Grant Nos.42172124,41702110,42330810 and U19B6003-01-01);the National Key R&D Program of China(Grant No.2023YFF0804302).
The Carboniferous to Permian tectono-sedimentary evolution of the southern Junggar area brings new insights into understanding the subduction-collision processes in the northern Tianshan region.Integrating geophysics,...
SHAvdL and DJJvH were funded by NWO Vici grant 865.17.001 to DJJvH.LC acknowledges funding from the National Natural Science Foundation of China(grant 42106073);Open Fund of the State Key Laboratory of Marine Geology(Tongji University)(grant MGK202107).
The South China,Indochina,and Borneo margins surrounding the South China Sea contain long-lived arcs that became inactive at approximately 85 Ma,even though an embayment of oceanic crust(the‘Proto-South China Sea’)r...
supported financially by funds from the National Natural Science Foundation of China (92055208,41888101);the Guangxi Science Innovation Base Construction Foundation (GuikeZY21195031);the Fifth Bagui Scholar Innovation Project of Guangxi Province (to XU Jifeng);Gansu Province Youth Science and Technology Fund Project (23JRRG0017);Guangxi Young and Middle-aged Teachers'Basic Competence Enhancement Program (2023KY0270).
The chemical evolution and pressure-temperature conditions of subduction zone magmatism along ancient suture zones in orogenic belts can provide important information regarding plate convergence processes in paleo-oce...
Funding for this research was provided by the National Natural Science Foundations of China (Grant No.41702054);the China Geological Survey Program (DD2016007907)awarded to Changfeng Liu and administered by the Institute of Geological Survey,China University of Geosciences (Beijing).
One of the ophiolites that record the Proto-Tethys Ocean’s episodic closure is the Munabulake ophiolitic mélange,which is situated in the middle of the Kunlun-Qaidam and Altun-Qilian blocks.Detailed field mapping re...
Funding to J.F.Casey for mapping,sample collections,and geochemical work in the Bay of Islands region were derived from U.S.National Science Foundation grants EAR80-26445,EAR-83-09535,EAR-88-04756;a University of Houston Departmental of Earth and Atmospheric Sciences grant in 2017.
The welded metamorphic sole at the base of the Bay of Islands Ophiolite Complex(BOIC)in the Northern Appalachians of Newfoundland shows a typical inverted pressure-temperature(P-T)metamorphic gradient from HT-MP granu...