相关期刊:《Acta Geologica Sinica(English Edition)》《Science China Earth Sciences》《Wuhan University Journal of Natural Sciences》《Journal of Earth Science》更多>>
supported by the National Natural Science Foundation of China (Nos. 41772066, 41902075, 41862010, 42172098, and 42002091);the Open Fund from the Key Laboratory of the Northern Qinghai-Tibet Plateau Geological Processes and Mineral Resources (No. 2019-KY-04);the Open Fund from the State Key Laboratory of Nuclear Resources and Environment of the East China University of Technology (No. NRE1309);the Postgraduate Innovation Fund Project of Jiangxi Province, China (No. YC2021-B161)
Many sandstone-type uranium mineralization sites have been identified along the northern margin of the Qaidam Basin in North China.Intense tectonism and multistage magmatism that occurred there have restricted the use...
Kazhdumi is one of the Bangestan Group formations aging late early Cretaceous (Albian). Three subsurface sections of the sandstone bearing part of Kazhdumi in the studied area located at northwest of the Persian Gulf ...
Supported by the Geological Relic Protection Project of Ministry of Finance and Ministry of Land and Resources of China
The paleoflow direction of the basal conglomerate of the Changzhougou formation is obtained by the paleocurrent analysis of certain sedimentary structures,and the ancient sedimentary environment of the Qian’an Region...
supported by the National Natural Science Foundation of China (Nos. 41290253, 40772116);the National Basic Research Program of China (973 Projects) (Nos.2010CB83340, 2013CB955904)
The north-trending Liupan Shan (六盘山) is an important tectonic boundary between the Tibetan Plateau and the Ordos platform. The Late Cenozoic red earth deposits of the Liupan Shan record its tectonic history and e...
supported by the National Natural Science Foundation of China(No.40572077);Specialized Research Fund for the Doctoral Program of Higher Education(No.20060616005).
Paleocurrent indicator data collected in field work were used to study the early Cenozoic regional paleodrainage patterns in the Hob Xil basin in northern Tibetan plateau. The paleocurrent directions of the Eocene Fen...
Basin-fill sequences of Mesozoic typical basins in the Yanshan area, North China may be divided into four phases, reflecting lithosphere tectonic evolution from flexure (T3), flexure with weak rifting (J1+2), tectonic...
We focus on early Cenozoic uplift, erosion and growth of northern Tibet plateau by reconstructing paleo\|drainage pattern in the Hoh Xil basin. Stratigraphical infilling sequences and lithic type orogenic basins are d...
Based on analysis of magnetic febric and magnetic relict, the paleocurrents recorded in drilling cores in Subei coastal plain are bidirectional. NE_SW in the northern core and NW_SE in the southern core. The paleocurr...