东南亚地区烃源岩特征与主控因素

姚永坚; 吕彩丽; 康永尚; 杨楚鹏; 殷征欣; 韩冰; 万荣胜; 徐巧越

doi:10.3799/dqkx.2013.036

Volume 38 Issue 2

Mar. 2013

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Article Navigation > Earth Science > 2013 > 38(2): 367-378

YAO Yong-jian, LV Cai-li, KANG Yong-shang, YANG Chu-peng, YIN Zheng-xin, HAN Bing, WAN Rong-sheng, XU Qiao-yue, 2013. Characteristics of Hydrocarbon Source Rocks and Their Main Controlling Factors in Southeast Asia. Earth Science, 38(2): 367-378. doi: 10.3799/dqkx.2013.036

Citation:

YAO Yong-jian, LV Cai-li, KANG Yong-shang, YANG Chu-peng, YIN Zheng-xin, HAN Bing, WAN Rong-sheng, XU Qiao-yue, 2013. Characteristics of Hydrocarbon Source Rocks and Their Main Controlling Factors in Southeast Asia. Earth Science, 38(2): 367-378. doi: 10.3799/dqkx.2013.036

Citation:

YAO Yong-jian, LV Cai-li, KANG Yong-shang, YANG Chu-peng, YIN Zheng-xin, HAN Bing, WAN Rong-sheng, XU Qiao-yue, 2013. Characteristics of Hydrocarbon Source Rocks and Their Main Controlling Factors in Southeast Asia. Earth Science, 38(2): 367-378. doi: 10.3799/dqkx.2013.036

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Characteristics of Hydrocarbon Source Rocks and Their Main Controlling Factors in Southeast Asia

doi: 10.3799/dqkx.2013.036

1.
Guangzhou Marine Geological Survey Bureau, Guangzhou510760, China
2.
Key Laboratory of Marine Geology and Environment, CAS, Qingdao266071, China
3.
State Key Laboratory of Petroleum Resources and Detection, China University of Petroleum, Beijing100249, China
4.
College of Marine Science, Sun Yat-Sen University, Guangzhou510006, China

Received Date: 2012-05-23
Publish Date: 2013-03-01

Abstract

Abstract

Based on the research of the sedimentary and structural features, hydrocarbon source rocks in the main sedimentary basins in Southeast Asia can be defined into multi-phases and those in Miocene, Oligocene and Eocene are the most important three sets. The pre-Cenozoic source rocks have certain potentials, but with limited distribution. The three sets are mainly fluvial facies to paralic delta with terrigenous kerogen-based coal and carbonaceous shale (mudstone), followed by lacustrine and marine depositional including mudstone and shale. The total organic carbon in these rocks has reached to intermediate to good dominated by Ⅱ-Ⅲ type of kerogen, and most of them are in the stage of mature to over-mature. The generation and distribution of the source rocks are mainly controlled by two geological factors, namely, tectonic evolution and depositional environments of the basins, and closely related to the direction and scale of regional transgression. Therefore, the fractionations in the type and the thermal evolution degree of hydrocarbon source rocks are the most important factors contributing to the various types of oil and gas reservoirs in Southeast Asia.
- Southeast Asia,
- hydrocarbon source rocks,
- controlling factors,
- basin,
- petroleum geology

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References(42)

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