the National Natural Science Foundation(grant no.41472173);the Ministry of Land and Resources Outstanding Youth Science and Technology Talent Training Program of China(grant no.201311111);the National Oil Shale Geological Survey and Evaluation Program(grant no.dkyd201908-02).
Many studies have focused on the Cretaceous evolution of NE China,including the 973 Scientific Exploration Well Work program,which completed two drill holes in this area.The Cretaceous Basin Group of eastern NE China ...
the Geological Survey project of China Geological Survey(grant No.DD20160040).
The Beishan area,located on the southern margin of the Central Asian orogenic belt,includes four main ophiolitebearing belts.From north to south,these are the Hongshishan ophiolitic belt,the Jijitaizi-Xiaohuangshan op...
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...
financially supported by the National Natural Science Foundation (grants No. 41102065 and 41872110);the Sichuan Science and Technology Program (grant No. 2018JY0465)
Objective The Shiquanhe ophiolite is an important tectonic belt in western Tibet. It has been debated whether the Shiquanhe ophiolite represents an allochthonous nappe derived from the Bangong-Nujiang suture zone to t...
financially supported by the National Natural Science Foundation of China(grant No.41502079);China Geological Survey(grants No.[2012]03-002-055 and [2014]01-028-042)
Objective Lhasa terrane has recorded the geologic history conceming the formation and evolution of Paleo-Tethys and the intra-continental convergence in Qinghai-Tibet Plateau (Yin and Harrison, 2000). Previous inve...
financially supported by the Nature Science Foundation of China (grants No.41372109,90914003 and 41672111);China Geological Survey (grants No.12120115068901,1212011120142 and 12120114064301);the National Science and Technology Works Special Project (grant No.2015FY310100)
Objective Previous studies indicate that the North China Craton(NCC)had undergone the loss of thickened lithosphere and fundamental change of physical and chemical property of lithospheric mantle(the destruction of...
supported by 973 (2012CB416601) and NFSC (41322018) projects
To define a tectonic environment switching from rifting to subduction and their respective duration time are usually largely debated.Such case occurs for the Liaohe rift:whether it went through a long subduction from ...
supported by 973 (2012CB416601) and NFSC (41322018) projects
It is well known that there are widespread igneous events at;100 Ma in the Eastern North China Craton;however,their tectonic environments are controversial.They were thought to be either related to an intra-continenta...
The 1780-1760 Ma Taihang dyke swarm and the coeval Xiong’er volcanic province are the most widespread magmatic events occurring post the amalgamation of the two North China cratons.It has been debated whether
Until recently the time period 2400-2200 Ma in the Erath history was characterized by low amount of age data for igneous events,and was even considered as‘magmatic age gap’(Condie et al,2009;Eriksson and Condie,2014).