the National Natural Science Foundation of China(No.41702135);the Yangtze Youth Fund(No.2015qq33),the 13th“Five-year”plan of the Ministry of Science and Technology of China(No.2016ZX05037-002);National Science and Technology Major Project(NO.2016ZX05015-006).
Pearl River Mouth Basin undergoes complex tectonic evolution processes and forms lacustrine,transitional and marine sediments.Drilling shows that there exist large petroleum reserves in the hydrocarbon-rich sags of Pe...
supported by the National Natural Science Foundation of China(No.41230210);the Projects of International Cooperation and Exchanges from the Ministry of Science and Technology of China(Grant No.2010DFB20190);the Fundamental Research Funds for the Institute of Earthquake Science,China Earthquake Administration
Shanxi Graben is in the middle part of the North China Craton, from south to north. With the teleseismic data recorded by Regional Seismograph Networks and the temporary ZBnet-W Seismic Array around east part of Shanx...
Supported by the National Basic Research Program of China(Grant No.2003CB214607);the Development Project of Changjiang River Scholars and the Innovation Research Team in University(Grant No.IRT0559)
The Helan Mountain lies in the northwest margin of Ordos Basin and its uplift periods have close relations with the tectonic feature and evolution of the basin.There are many views on the uplift time of Helan Mountain...
the National Key Basic Research Project (Grant No. G1998040800) and the Potential Analyses of Oil and Gas in Tibetan Plateau Project of the Ministry of Land and Resources of China.
The latest Qiangtang Terrane structure is characterized by the south-north-trending graben formed during the eastwestward extensional processes. The Shuanghu graben is composed of a series of nearly parallel NE to NNE...