The formation and growth mechanisms of Mid-Ocean Ridges(MOR)are relatively well known,whereas those of back-arc spreading ridges are comparatively less known because geophysical,geochemical,and morphological data are ...
supported by the Czech Science Foundation,Czechia(grant number 19-27682X to K.S.)。
The processes leading to the assembly of the Rodinia supercontinent through Grenvillian collisional orogeny are relatively well known.In contrast,accretionary orogenic processes occurring at the supercontinent periphe...
supported by the China Geological Survey(DD20160009,DD20190065 and DD20190004);the National Natural Science Foundation of China(41888101);the Natural Sciences and Engineering Research Council of Canada。
The Central Asian orogenic belt(CAOB),surrounded by the Baltica and Siberia cratons to the north,and the Tarim and North China cratons to the south,records successive evolution cycles of subduction and accretion/colli...
granted by the Natural Science Research Program of Colleges in Anhui Province(Grant Nos.2020zk01,KJ2019A1047 and KJ2021A1532);the Domestic Visit Training Program for Outstanding Young Teachers in Colleges in Anhui Province(Grant No.gxgnfx2020168)。
The Fuchuan ophiolite is located in the northeasternmost segment of the Neoproterozoic Jiangnan orogen and consists mainly of harzburgites,with minor dunites,pyroxenite and gabbro veins and dykes.In order to investiga...
the Ministry of Mines and Energy of Namibia for providing the financial support。
A study of the NW Kakamas Domain in South Africa/Namibia provides a new,unified lithostratigraphy and evolutionary history applicable to the whole Namaqua Sector.The Mesoproterozoic history ranges from~1350 Ma to 960 ...
supported by the National Natural Science Foundation of China(No.91962104);the Geological Survey Project from the Ministry of Science and Technology,China(No.1212011120326)。
Compositional changes in successively erupted felsic rocks can be used to infer physical changes in lower crustal conditions and to enhance the understanding of the tectonic regime.This study presents geochronological...
supported by the National Key Basic Research Program of China(Grant No.2013CB429701);the National Natural Science Foundation of China(Grant Nos.41606083,91958210,41606050 and 41210005);AoShan Technological Innovation Projects of National Laboratory for Marine Science and Technology(Qingdao)(2015ASKJ03);National Marine Geological Special Project(DD20190236,DD20190365,DD20190377)。
The marginal sea and back-arc basins in the Western Pacific Ocean have become the focus of tectonics due to their unique tectonic location.To understand the deep crustal structure in the back-arc region,we present a 5...
supported by National Natural Science Foundation of China(41802236);“the Fundamental Research Funds for the Central universities”(N170103013,N2001004 and N170104022);Opening Foundation of Key Laboratory of Mineral Resources Evaluation in Northeast Asia,Ministry of Natural Resources(DBY-KF-18-05)。
The early Paleozoic tectonic evolution of the Xing'an-Mongolian Orogenic Belt is dominated by two oceanic basins on the northwestern and southeastern sides of the Xing'an Block,i.e.,the Xinlin-Xiguitu Ocean and the Ne...
The National Natural Science Foundation of China under contract Nos 41706052,41476044 and 41325021;the National Program on Global Change and Air-Sea Interaction under contract No.GASI-GEOGE-02;the National Basic Research Program(973 Program)of China under contract No.2013CB429700;the International Partnership Program of Chinese Academy of Sciences under contract No.133137KYSB20170003;the Strategic Priority Research Program of the Chinese Academy of Sciences under contract No.XDA11030302;the Special Fund for the Taishan Scholar Program of Shandong Province under contract No.ts201511061;the National Special Fund for the 13th Five Year Plan of COMRA under contract No.DY135-G2-1-02;the AoShan Talents Program supported by Qingdao National Laboratory for Marine Science and Technology under contract No.2015ASTP-0S17;the Innovative Talent Promotion Program under contract No.2012RA2191;the Science and Technology Development Program of Shandong Province under contract No.2013GRC31502;the Scientific and Technological Innovation Project financially supported by Qingdao National Laboratory for Marine Science and Technology under contract No.2015ASKJ03;the National High Level Talent Special Support Program;CAS/SAFEA International Partnership Program for Creative Research Teams;Qingdao Collaborative Innovation Center of Marine Science and Technology
Hydrothermal precipitates associated with active vents in the eastern Manus Basin, an actively opening back-arc basin in the Bismarck Sea, Papua New Guinea, are among the most Cu-rich on the modern seafloor. The volca...
supported by the Sub Project of "National Key Research and Development Plan of China"-"Study on the Distribution Rule of Tianshan-Altai Bulk Minerals and Evaluation of Deep Resource Potential" (grant No. 2018YFC0604001);the Xinjiang Geological Exploration Fund (grant No. A16-1-LQ14);the National Natural Science Foundation of China (grants No. 41273033 and 41303027)
Objective Mafic magmas can form in different tectonic settings with various geochemical characteristics depending on their mantle sources. Basalts generated in back-arc basins provide valuable perspectives on mantle s...