This work was mainly supported by National Natural Science Foundation of China(NNSF,Grant No.41803028);Natural Science Foundation of Shandong Province(NSFSP,Grant No.ZR2018BD020)to Fengli Shao;Grant Nos.41802201,41630968 and 41688103 from NNSF;Grant Nos.ZR2018BD012 and ZR2020QD044 from NSFSP;Grant No.2019RZA02002 from soft science project of Shandong Province Key Research and Development Plan。
The East Kunlun Orogenic Belt(EKOB),which is in the northern part of the Greater Tibetan Plateau,contains voluminous Late Triassic intermediate-felsic volcanic rocks.In the east end of the EKOB,we identified highly di...
We present a detailed review of the petrological and geochemical aspects of rhyolite and associated silicic volcanic rocks(up to 20 vol%of all rocks)reported to date from twelve well known Phanerozoic continental mafi...
granted by the National Natural Science Foundation of China(Grant Nos.41272221,41772228,41702239);the Geological Survey Program of China(Grant Nos.1212011120159,DD20160201-04)
The Qilian orogenic belt,as an important component of the central orogenic system,can be divided into three tectonic units from north to south:the North Qilian tectonic belt,the Central Qilian tectonic belt and the So...
Supported by National Basic Research Program of China(No.2009CB219305)
Early Cretaceous A-type rhyolites of the Shangkuli Formation in the Hailar Basin of NE China exhibit geochemical characteristics of high silicon,alkali,Fe/Mg,Ga/Al,Zr,Pb,HFSEs,and REE contents but low Ca,Ba,Sr and Eu,...
supported by the NSFC(Nos.41172202 and 41190073);the China Geological Survey(No.1212011121256);the Ministry of Education of China(No.20110145130001);the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences in Wuhan(No.MSFGPMR201402)
Zircon U-Pb dating, Lu-Hf isotopic and geochemical data for the Silurian rhyolites from the Loei fold belt are presented to constrain their petrogenesis and tectonic settings. The rhyolites give a weighted mean 206Pb/...
supported by the Knowledge Innovation Program of the Chinese Academy of Sciences (KZCX2-YW-Q09-03);the National Natural Science Foundation for Distinguished Young Scholars (40625008);the National Basic Research Program of China (2011CB403101)