supported by National Natural Science Foundation of China (Grant Nos. 41172125, 40972090, 40802030, 40672143 and 40472107);National Basic Research Program of China (Grant Nos. 2012CB214804,2005CB422107 and G1999043305);Investigation and Evaluation on Strategic Region of National Oil and Gas Resource (Grant No. 2009GYXQ0205);Doctoral Fund of Ministry of Education of China (Grant No.200804250001);National Key Scientific Project (Grant No.2011ZX05002-003-001HZ);Northwest Oilfield Company of SINOPEC has given full support with fundamental geologic data
The salt beds of the Middle-Lower Cambrian are widespread in the middle-west parts of the Central Uplift and adjacent areas, the Tarim Basin. This paper presents the results of seismic interpretation and drilling data...
support from the National Natural Science Foundation of China (grant No.40672143,40472107,and 40172076);the National Major Fundamental Research and Development Project (grant No.2005CB422107 and G1999043305);the Development Foundation of Key Laboratory for Hydrocarbon Accumulation of Education Ministry (grant No.2003-03);the Project of Southwestern Exploration and Development Division Company,SINOPEC (GJ-51-0602).
By analyzing the balanced cross sections and subsidence history of the Longmen Mountain thrust belt, China, we concluded that it had experienced five tectonic stages: (1) the formation stage (T3x) of the miniatur...
support from:National Natural Science Foundation of China (Grant no.40672143,40472107,40172076);National Major Fundamental Research and Development Project (Grant no.2005CB422107,G1999043305);Development Foundation of Key Laboratory for Hydrocarbon Accumulation of Education Ministry (Grant no.2003-01);Project of Southern Exploration and Development Division Company,SINOPEC (2003-04).
Field investigation and seismic section explanation showed that the Longmen Mountain Thrust Belt has obvious differential deformation: zonation, segmentation and stratification. Zonation means that, from NW to NE, th...
Supported by National Natural Science Foundation of China (Grant Nos.40672143,40472107 and 40172076);National Basic Research Program of China (Grant Nos.2005CB422107 and G1999043305);Development Foundation of Key Laboratory for Hydrocarbon Accumulation of Education of Ministry (Grant No.20003-01);Project of Southwest Branch Company,SINOPEC (Grant No.GJ-51-0602)
As is well known that many decollement layers were developed in the Longmenshan thrust belt,Si-chuan Basin,China. Through field investigation,explanation of seismic profiles and analysis of the balanced sections,we ca...
Supported by National Natural Science Foundation of China (Grant Nos.40672143 and 40472107)
Attention has been paid to the deformations in the south and north foreland basins of the Tianshan Mountains and their relations to the tectonic movements of the mountains. Based on the seismic data interpretation and...
supported by the National Natural Science Foundation of China (Nos. 40672143, 40472107, 40172076);the National Basic Research Program (Nos. 2005CB422107, G1999043305);Project of Northwest Oilfield Company, SINOPEC (KY-S-2006-014)
Basic and intermediate-acidic igneous rocks were developed during the late Hercynian in North Tarim basin. The geochemistry characteristics of the rocks show that basic volcanic rock has K2O/Na2O = 0.18-0.61 〈 1 and ...
supported by the National Natural Science Foundation of China (Nos. 40672143, 40472107, 40172076);the National Basic Research Program of China (Nos. 2005CB422107, G1999043305);Development Foundation of Key Laboratory for Hydrocarbon Accumulation of the Ministry of Education of China (No. 2003-03);Project of the South-west Petroleum Natural Gas Subcompany of SINOPEC (No. GJ-51-0602)
Through field geological survey, the authors found that abundant thrust faults developed in the Longmen (龙门) Mountain thrust belt. These faults can be divided into thrust faults and strike-slip faults according to...
the National Natural Science Foundation of China(Grant No.40672143,40472107 and 40172076);the National Major Fundamental Research and Development Project(Grant No.2005CB422107 and G1999043305);Development Foundation of Key Laboratory for Hydrocarbon Accumulation of the Education Ministry(Grant No.2003-01);Project of Southern Exploration and Development Division Company,SINOPEC(2003-04).
The Triassic Jialingjiang Formation and Leikoupo Formation are characterized by thick salt layers. Three tectono-stratigraphic sequences can be identified according to detachment layers of Lower-Middle Triassic salt b...