supported by the National Basic Research Program of China(Grant Nos.2011CB403000,2017YFC0602803);the Strategic Priority Research Program of Chinese Academy of Sciences(Grant No.XDA20070201);the Second Tibetan Plateau Scientific Expedition and Research Program(STEP)(Grant No.2019QZKK0707);the National Natural Science Foundation of China(Grant Nos.41988101,41907263,41974080);the Funding of the Qingtan Scholar Talent Project of Zaozhuang University。
Knowledge on the origin and mechanism of the large potash formation in the southeast Tethyan tectonic domain are still under debate,one of which mainly due to the controversial ages of the potash-bearing strata.Here w...
granted by the National Natural Science Foundation of China(Grant No.41272030);the IGCP 608;the National Basic Research Program of China(Grant No.2012CB822001).
1 Introduction The collision evolution between the Indian plate and the Eurasian plate is one of the significant geological events since the Mesozoic.It has profoundly influenced the global tectonic framework and led ...
sponsored by National Program on Key Basic Research Project(973 Program, Grant No. 2016YFC0600308);the China Geological Survey(Grant No. DD20160015)
The Upper Triassic flysch sediments(Nieru Formation and Langjiexue Group)exposed in the Eastern Tethyan Himalayan Sequence are crucial for unraveling the controversial paleogeography and paleotectonics of the Himalaya...
funded by the State Fund for Natural Science of China(No40976029);the National Basic Research Program of China("973")(2007CB411700 and 2009CB2194);the Major Knowledge Innovation Programs of the Chinese Academy of Sciences(kzcx2-yw- 203-01);the National Program of Sustaining Science and Technology(2006BABl 9B02);the Program of the Ministry of Land and Resources,China(GT-YQ-QQ-2008-1-02 and 2009GYXQ06)
The basement of the South China Sea(SCS)and adjacent areas can be divided into six divisions(regions)-Paleozoic Erathem graben-faulted basement division in Beibu Gulf,Paleozoic Erathem strike-slip pull-apart in Yi...
This work was supported by the Natural Science Foundation of China (NSFC) (grant No. 40232024);Chinese Geological Survey (grant No. 1212010611801) ;Ministry of Science and Technology of China (grant No. 2001CB711002).
The middle Permian Cryptospirifer fauna (brachiopod) has hitherto been found in more than 30 localities in the Yangtze Platform, South China. Examination of data from various localities shows that it occurs stratigr...
the National Natural Science Foundation of China(Grant No.40072011);the China National Commission on Stratigraphy;the Minis try of Science and Technology,and the Chinese“973 Program”(Grant No.G2000077705).
The Olenekian Stage of the Lower Triassic is named from the Boreal Realm, but the stage has never been properly defined, nor has it been applied in the low-latitude Tethyan Realm, with exception of North Caucasus and ...
the National Key Project for Basic Research on Tibetan Plateau(G1998040800), the National Natural Science Fountain of China (Grant Nos. 49772107, 49802005, 40103003), Key Basic (9501101-3) and Special Projects on Tibetan Plateau (No. 200101020401) of t
The trachyte and basaltic trachyte and intruded granite-porphyry of Gazacun formation of Wuyu Group in central Tibet are Neogene shoshonitic rocks. They are rich in LREE, with a weak to significant Eu negative anomali...