Characteristics of Chinese Petroleum Geology: Geological by Chengzao Jia

By Chengzao Jia

"Characteristics of chinese language Petroleum Geology: Geological good points and Exploration circumstances of Stratigraphic, Foreland and Deep Formation Traps" systematically provides the development made in petroleum geology in China and highlights the most recent advances and achievements in oil/gas exploration and learn, in particular in stratigraphic, foreland and deep formation traps. The e-book is meant for researchers, practitioners and scholars operating in petroleum geology, and can also be an authoritative reference paintings for international petroleum exploration specialists who are looking to study 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 learn for 30 years and in oil/gas exploration for greater than 20 years.


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3 Intra-Continental Faulted Basin Developed During the Jurassic–Cretaceous Periods From the Jurassic–Cretaceous periods, the Paleo-Pacific ocean was closed along the eastern margin of the Paleo-Asian continent and a collision occurred between the Paleo-Asian continent and Western Pacific plate. During the same time interval, Bangong-Nujiang ocean disappeared along the southern margin of the Paleo-Asian continent and the Lhasa terrane collided with the Paleo-Asian continent (Fig. 7c). In addition, the Paleo-Tethys oceanic domain still had marine deposits in the region south of the Tibetan plateau while the rest of the Chinese basins received terrestrial deposits.

Petroleum Geology & Experiment, 8(2):97-106. , 1993. Collision successor basins of western China: impact of tectonic inheritance on sand composition. Geo. Soc. Amer. , 105:323-344. , 1996. Development and Evolvement of the Sichuan Basin. Geological Publishing House, Beijing. , 1992. Raising Tibet. Science, 255:1663-1670. , 1994. Late Oligocone-Early Miocene unroofing in the Chinese Tian Shan: An early effect of the India-Asia collision. Geology, 22(6):487-490. , 1988. Relict back-arc basins: principles of recognition and possible new example from China.

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