supported by the National Key Research and Development Project (Grant No. 2017YFC0601405);the National Natural Science Foundation of China (Grant Nos. 41572189 & 41820104004);the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDB18030604)
The northwestward subduction of the Izanagi Plate beneath the eastern Eurasian Plate during the Late Mesozoic caused a series of compressional deformation events in the Yanshan fold and thrust belt(YFTB), but the tect...
supported by National Natural Science Foundation of China(Grant Nos.40672080,40921062,41302083);Fundamental Research Funds for the Central Universities,China University of Geosciences(Wuhan)(CUG120807)
The Biyang Depression, lying in the eastern Nanxiang Basin, has a dustpan-shape with faults developed to the southwest and southeast. The Paleogene Hetaoyuan Formation in this depression hosts one of the oldest soda-d...
supported by National Natural Science Foundation of China(Grant Nos.90914003,40872017);National Basic Research Program of China(Grant No.2006CB70145)
The sequence stratigraphy and geochronology of the terrestrial dinosaur-bearing strata,i.e.,the Qiupa Formation,were poorly studied in the Luanchuan-Tantou Basin in western Henan,China.This study shows that these stra...
supported by Chinese Academy of Sciences (Grant Nos.KZCX2-YW-122,2008ZX05008-001-001);Ministry of Science and Technology (Grant No.2006CB806402);National Natural Science Foundation of China (Grant No.40772002)
The Ordovician graptolite sequence of the Yongxin-Chongyi area in southern Jiangxi was suggested as a standard for the correlation of Ordovician in the Zhujiang region of South China. Based on a restudy of the Upper O...
supported by the Important National Science & Technology Specific Projects (Grant No.2008ZX05001);Scientific Development Projects of Petrochina Company Limited (Grant No.2008B-0100);the Doctoral Education Program Fund of Ministry of Education,China (Grant No.20060491505);American Association of Petroleum Geologists Grants-in-Aid Foundation Program;National Natural Science Foundation of China (Grant Nos.40739904,40902039)
Carbonate cemented zones are normally adjacent to the top overpressured surface in the central Junggar Basin,NW China.Stable carbon and oxygen isotopic compositions and petrological investigations of carbonate cements...
Supported by Science and Technology Project of Sinopec (Grant No. G0800-06-ZS-324) 1) Mineral Resources Authority of Mongolia. Geological Map of Mongolia (1:1000000), Ulaanbaatar. 1998 2) Kociurzhinskim B V, Poliakovym V M, Efriemovoii V N. Geological Map of Chita (1:1000000), Russia. 20003) Krasnyi L I, Peng Y B. Geological Map of Amur Region and Adjacent Areas (Scale 1:2500000), Harbin, China. 1996
An analysis of the distribution of the Late Paleozoic strata on Northeast China and adjacent region reveals a zonal pattern of the distribution around the core of the Jiamusi-Mongolia Block. The main part of Late Pale...
A sediment-continuous section of Jurassic-Cretaceous (J-K) boundary strata was found in Zhangjiagou of Luanping, northern Hebei Province, China. The boundary strata were systematically divided into 5 sequences, 13 sub...
The two sections containing hominoid fossils in the Yuanmou Basin, Yunnan Prov-ince have been studied by means of magnetostratigraphy. The results are as follows. The Xiaohe section records over 8 polarity zones corre...
The organic matter-rich strata of the Yurtusi Formation of Lower Cambrian are wildly spread and steady in the Tarim Basin, in which cherts are developed, companied with phos-phorite. Al/(Al+Fe+Mn) ratio and Si/(Si+Al+...
The main character of melange strata in an erogenic belt is the integration of mixed materials due to the superposition, displacement or loss of various tectonic slices (blocks) of different origins and environments, ...