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By Chengzao Jia

"Characteristics of chinese language Petroleum Geology: Geological positive factors and Exploration situations of Stratigraphic, Foreland and Deep Formation Traps" systematically offers the development made in petroleum geology in China and highlights the newest advances and achievements in oil/gas exploration and study, in particular in stratigraphic, foreland and deep formation traps. The publication is meant for researchers, practitioners and scholars operating in petroleum geology, and is usually an authoritative reference paintings for overseas petroleum exploration specialists who are looking to examine extra approximately this box in China.

As President of the chinese language Petroleum Society, former Vice-President of PetroChina corporation restricted, and Academician of the chinese language Academy of Sciences, Dr. Chengzao Jia has been engaged in geological study for 30 years and in oil/gas exploration for greater than 20 years.

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Extra info for Characteristics of Chinese Petroleum Geology: Geological Features and Exploration Cases of Stratigraphic, Foreland and Deep Formation Traps

Example text

During this time interval, not only was the ancient landmass elevated and eroded to form the ancient Central Sichuan uplift but, also, on the northern margin of the Yangtze plate, the Mianlue oceanic basin was split open and it received massive marine carbonate deposits. Additionally, a basalt eruption happened during the Permian period. During the Triassic period, the Yangtze plate drifted to a latitude of 15° N and it converged with the North China plate. Because of compressive stress that was brought on by the convergence event, fold-thrust structures were well developed on the western and northern margins of the Sichuan basin; on the intra-continent, the depression and lacustrine basin were superimposed.

2001. Seismic image of Tarim basin and its collision with Tibet. Geology, 29:575-578. , 1982. Manual of Asian Geotectonic Map. Geology Press, Beijing. , 2002. Petroleum geology of sedimentary basins in northwest China. Marine Origin Petroleum Geology, 7(1):1-6 (in Chinese with English References 31 abstract). , 1995. Types of foreland basin and patterns of fold-thrust fault. Earth Science Frontiers, 2(3):59-68. , 1994. Rejuvenation of the Kuqa foreland basin, northern flank of the Tarim basin, Northwest China.

From the Devonian–Permian periods, the ancient Yangtze plate was still located south of the equator. During this time interval, not only was the ancient landmass elevated and eroded to form the ancient Central Sichuan uplift but, also, on the northern margin of the Yangtze plate, the Mianlue oceanic basin was split open and it received massive marine carbonate deposits. Additionally, a basalt eruption happened during the Permian period. During the Triassic period, the Yangtze plate drifted to a latitude of 15° N and it converged with the North China plate.

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