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funded by the Natural Science Foundation of Guangxi Province(Nos.2022GXNSFAA035570,2022GXNSFBA035463);the National Natural Science Foundation of China(Nos.42162018,42072259);the Innovation Project of Guangxi Graduate Education(No.YCBZ2021065)。
The Luojiashan gabbro is a newly discovered mafic pluton emplaced in the Neoproterozoic Yingyangguan Formation in Yingyangguan region of northeastern Guangxi,South China.Comprehensive whole-rock geochemical and zircon...
The National Science and Technology Major Project under contract No. 2016ZX05026-004;the National Key R&D Program of China under contract No. 2019YFC0605402;the National Natural Science Foundation of China under contract No.41790453。
The southwest Lahad Datu felsic rocks were previously thought to have formed in the late Triassic as part of the microcontinental crystalline basement.Based on U-Pb ages,geochemistry,and the Hfisotopes of zircon from ...
Granitoids at Butre area, south-western part of the Birimian of Ghana are gabbro to granodiorite which intruded comagmatic basalt and andesite of volcanic island arc setting. Differentiation was from probably mantle f...
supported by the National Natural Science Foundation of China Program(Grant Nos.41672072,41302074);the Third Xinjiang Scientific Expedition Program(Grant No.2021xjkk1301)。
The Xiaobaishitou gabbro-diorite pluton comprises a medium-grained gabbro-diorite suite and a fine-grained diorite suite,which intrude the Kawabulag Group in the East Tianshan Orogen of the Central Asian Orogenic Belt...
financial support from the Natural Science Foundation of Urmia University。
The mafic intrusive Moskin and Parvaneh regions in the northwest and south of Urmia were investigated for their geochemistry and petro-physical properties such as size,shape,and spatial distribution of their crystals....
financially supported by the Geological Exploration Foundation of the Xinjiang Uygur Autonomous Region(Grant No.T15-1-LQ12)。
Objective Ophiolite constitutes an important record of the history of the geological evolution of orogenic belts.There are four important Paleozoic ophiolite(mélange)zones in the Yining Block,northwestern China:north...
This study was financially supported by Open Fund of the Research Center for Petrogenesis and Mineralization of Granitoid Rocks(PMGR202002);projects of China Geological Survey(12120113063200,DD20160031,DD20190050).
1.Objectives As one of three major tectonic blocks of China,the South China Block has undergone multiple periods of tectonic-magmatic-metamorphic events.Among these events,the Caledonian orogeny results in the formati...
financially supported by the National Natural Science Foundation of China(Grant No.41702054);supported by the Research Funds for the Central Universities(Changfeng-Liu,2652018281)。
The Xingmeng Orogenic Belt evolved through a long-lived orogeny involving multiple episodes of subduction and accretion.However,there is a debate on its tectonic evolution during the Late Paleozoic.Here,we report geoc...
supported by the National Natural Science Foundation of China(Grant Nos.41402042,41002064);Fundamental Research Funds for the Central Universities(Grant Nos.310827172006,300102278402);Geological investigation work project of China Geological Survey(No.12120115069701)。
The giant Central Asian Orogenic Belt is an extensive accretionary orogen,of which the Solonker suture,as a major regional suture,coincides closely with an early Permian paleobiogeographical boundary.This suture is co...
granted by the National Key Basic Research Program from the Chinese Ministry of Science and Technology(Grant No.2015CB856101);Foundation of Research Center for Tibetan Plateau Geology(21201010000150014-29);the China Geological Survey(No.1212011221066)
Discontinuous ophiolite suites along the Yarlung Zangbo suture zone(YZSZ)in southern Tibet representing remnants of the Neo-Tethyan oceanic lithosphere are considered to be formed between Late Jurassic and Early Creta...