supported by the National Oil and Gas Major Project(Grant Nos.2017ZX05035&2016ZX05046)。
The Sichuan Basin is rich in shale oil and gas resources,with favorable geological conditions that the other shale reservoirs in China cannot match.Thus,the basin is an ideal option for fully"exploring petroleum insid...
supported by the National Natural Science Foundation of China(Grant Nos.41572203,41890834,&41961144020);the 111 Project from the Ministry of Education of China(Grant No.BP0719022);the MOST Special Fund(Grant No.MSFGPMR02-3);the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan,and the Chinese Academy of Sciences(Grant No.QYZDY-SSW-DQC017).
When plate tectonics emerged and how it has evolved over Earth history are two of the most fundamental challenges in Earth Sciences.These questions are tackled using a holistic approach to analyze tectonic styles in t...
supported by the National Natural Science Foundation of China(Grant Nos.41290260,41521061,41530103);Chinese Academy of Sciences(Grant No.XDPB05)
It is the first time to document the trilobite Mucronaspis(Songxites) wuningensis and the brachiopod ParomalomenaAegiromenella Assemblage from the Xinkailing Bed(Hirnantian, uppermost Ordovician) in Taoyuan and Cili c...
supported by the National Natural Science Foundation of China (Grant No. 41472027);the Chinese Geological Survey (Grant No. 1212011120927)
Many plateau-edge reefs and reef mounds of the Late Permian have been discovered in Linxi County and adjacent areas of Inner Mongolia, China. These reefs verify that the Hinggan-Inner Mongolia Area was an open and uno...
supported by National Science and Technology Major Project (Grant No. 2009ZX05009);National Basic Research Program of China (Grant No. 2011CB808800);National Natural Science Foundation of China (Grant Nos. 41172036, 40730209);the "111" Project (Grant No. B08030)
Gypsum-salt rocks and coccolith calcareous shale are widely deposited in the lower part of the Paleogene Shahejie Formation in the Dongying Sag, Sbandong Province. The gypsum-salt rock is believed to be formed during ...
supported by National Basic Research Program of China (Grant No. 2011CB808800);National Natural Science Foundation of China (Grant No. 41072078)
The Chihsia Formation is one of the four sets of regional marine hydrocarbon source rocks from South China.In the past two decades,detailed geochemical and sedimentological studies have been carried out to investigate...
NSFC Innovation Research Group Program (Grant No. 40621002);MOE Innovative Research Team Program (Grant No. IRT0546);China Geological Survey Project (Grant No. 1212010610709);"111" Project (Grant No. B08030)
The end-Permian mass extinction not only severely distressed the Paleozoic ecosystems but also dramatically changed the sedimentary systems, resulting in a peculiar Early Triassic ecosystem and submarine environment d...
the Basic Geology Survey Plan of China Geological Survey (No. 200213000003)
Pan-riftizational tectonic activity reached climax at Luodianian (Permian) in the East Tethyan Domain, Qinghai-Tibet Plateau. Because of eruptive volcanics and influence of terrigenous materials, a complex volcanic-se...
Supported by the National Basic Research Program of China (Grant Nos. 2003CB214607 and 2006CB202201) and the National Natural Science Foundation of China (Grant Nos. 40472083 and 40672102)
The No. 6 Coal-bed from the Heidaigou Mine, Jungar Coalfield, Inner Mongolia is a super-large Ga deposit. The dominant carrier of Ga is boehmite in coal. The study of coal facies may provide genetic enrichment informa...
This work was jointly supported by the National Natural Science Foundation of China (Grant No. 40172014);the state key project “Study of Sequence Stratigraphy on the Paleocontinents and Their Margins of China and Earth Rhythms (SSER)” of the Ministry of Science and Technology of China,and the Laboratory of Palaeobiology and Stratigraphy, the Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences (Grant No. 013101). Geological Congress in Rio de Janeiro, Brazil in 2000.
The regional distribution in different depositional facies belts is here regarded as an important criterion for defining and recognizing the various orders of sequences. The third-order sequence is possibly global in ...