supported by National Science Foundation of China(42102059 and 92055202);the China Geological Survey(DD20221817 and DD20190057);the basic scientific research funding in CAGS(J2204);the Second Tibetan Plateau Scientific Expedition and Research(2019QZKK0702).
Two suites of mafic dykes,T1193-A and T1194-A,outcrop in Gyangze area,southeast Tibet.They are in the area of Comei LIP and have indistinguishable field occurrences with two other dykes in Gyangze,T0902 dyke with 137....
financially supported by the National Natural Science Foundation of China(Grant No.42072150).
The research on the correlation between hydrocarbon accumulations and magmatic activities has always attracted aroused much wide attention.Existing research has primarily the hydrocarbon generations capability of sour...
Supported by the projects of China Geological Survey(DD20230004,DD20190039-06,DD20190360-2,DD20190360,DD20221632-01);the National Natural Science Foundation of China(42002227).
1.Objective The Bainaimiao Arc Belt(BAB),one of the most important units of the southeastern Central Asian Orogenic Belt(CAOB),locates along the northern margin of the North China Craton(NCC).There is a lack of unders...
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...
We are grateful to three anonymous reviewers for their constructive comments and suggestions;This study was financially supported by the National Nature Science Foundation of China(Nos.41572049,41902050,41430209,41421002);the Major State Basic Research Development Projects(No.2015CB856103);the State Key Laboratory of Continental Dynamics,Northwest University.
Mafic dyke swarm is widely developed in Proterozoic continental lithosphere.The Gangou diabase dyke from the Xixia area,intruded into the Douling complex of the South Qinling belt,yields zircon UPb age of 731 Ma.It ha...
supported by the Geological Survey of China (No. 1212011085490);the National Natural Science Foundation of China (No. 41421002)
The end-Permian to Early–Middle Triassic magmatic rocks in Inner Mongolia can provide valuable insights into the relationships between the collisional processes and the magmatic responses during the final orogenic ev...
supported by the Guizhou Scientific and Technology Planning Project (Nos. QKHZDZX [2014]6003, QKHPTRC[2018]5626 and QKH[2016]PTRC5401)
Compositionally and texturally zoned diabase dykes and sills occur in the outer zone of the Emeishan large igneous province(ELIP) in the southern Guizhou Province,Southwest China. Based on the detailed petrology,whole...
financially supported by China Geological Survey (Grant no. DD20160060);the National Natural Science Foundation of China (Grant nos. 4153209, 41872135)
In order to understand the petrogenesis and tectonic setting of diorite and diabase units on Doumer Island, Antarctic Peninsula, this paper reports new laser ablation-inductively coupled plasma-mass spectrometry(LA-IC...
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...
Northern part of Eastern Dharwar Craton (EDC) in Karnataka is essentially a granitoid country, frequently intruded by diabase dykes of varied dimensions. Compositionally, majority of them are constituted by pyroxene a...