BASIN TYPES AND CHARACTERISTICS OF BASIN GROUPS IN EAST ASIA

KANG Yong-shang; SHANG Yue-nan; YUE Lai-qun; DIAO Shun; QI Xue-feng

Volume 18 Issue 4

Dec. 2012

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Article Navigation > Journal of Geomechanics > 2012 > 18(4): 347-358

KANG Yong-shang, SHANG Yue-nan, YUE Lai-qun, et al., 2012. BASIN TYPES AND CHARACTERISTICS OF BASIN GROUPS IN EAST ASIA. Journal of Geomechanics, 18 (4): 347-358.

Citation:

KANG Yong-shang, SHANG Yue-nan, YUE Lai-qun, et al., 2012. BASIN TYPES AND CHARACTERISTICS OF BASIN GROUPS IN EAST ASIA. Journal of Geomechanics, 18 (4): 347-358.

Citation:

KANG Yong-shang, SHANG Yue-nan, YUE Lai-qun, et al., 2012. BASIN TYPES AND CHARACTERISTICS OF BASIN GROUPS IN EAST ASIA. Journal of Geomechanics, 18 (4): 347-358.

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BASIN TYPES AND CHARACTERISTICS OF BASIN GROUPS IN EAST ASIA

1.
College of Earth Sciences, China University of Petroleum, Beijing 102249, China
2.
State Key Laboratory of Petroleum Resources and Detection, China University of Petroleum, Beijing 102249, China
3.
Strategic Research Center of Oil & Gas Resources, Ministry of Land and Resources, Beijing 100034, China
4.
Department of Science and Technology Development, CNPC, Beijing 100724, China
5.
PetroChina Petroleum Exploration and Development Insitute, Beijing 100083, China

More Information

Received: 2012-08-23
Published: 2012-12-01

Abstract

Abstract

Tectonic evolution in East Asia was polyphased and complicated. The geological framework of East Asia basically formed during Indo-Chinese epoch. As an important tectonic evolution stage, Yanshannian epoch played a significant role in the evolution and formation process of sedimerntary basins in East Asia. In this paper, sedimentary basins in East Asia were divided into 6 types based on the three-dimensional stress (extension or compression) and the reformation degree of basins due to this stress background since Yanshannian, considering the evolution history of the basin themselves, and combined with previous research achievements on basin types. They were cratonic basin, intracontinental compaction flexture basin, strike-slip pull-apart basin, rift basin, forearc basin and back-arc basin. Basins in East Asia are further classified into two groups according to their formation periods (before or since Yanshannian epoch) and into seven groups in space according to the tectonic domains, to which one basin belongs. This classification study showed that basins in one tectonic domain were compatible relatively to such as basin type, depositional sequence, evolution history and so on, and basins in different tectonic domains displayed definite differentiation on these respects. The results of comparability or the community of the basins in the same basin group and the diversity of basins among the different basin groups, have great theoretical meaning for understanding the genesis and evolution of different basins. At the same time, this study also lays the foundation of analogy analysis for evaluation of oil and gas resource potential in the basins with lower degree of exploration.
- East Asia,
- tectonic evolution,
- basin types,
- basin groups

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References(29)

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