The evolution of basins and petroleum resource potential in the southern Pacific region

Yang Weili; Kang Yongshang; Yao Yongjian; Zhang Jianjun; Li Bo; Chen Hongwen; Wang Weihong

doi:10.3969/j.issn.0253-4193.2019.05.008

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Yang Weili, Kang Yongshang, Yao Yongjian, Zhang Jianjun, Li Bo, Chen Hongwen, Wang Weihong. The evolution of basins and petroleum resource potential in the southern Pacific region[J]. Haiyang Xuebao, 2019, 41(5): 79-96. doi: 10.3969/j.issn.0253-4193.2019.05.008

Citation:

Yang Weili, Kang Yongshang, Yao Yongjian, Zhang Jianjun, Li Bo, Chen Hongwen, Wang Weihong. The evolution of basins and petroleum resource potential in the southern Pacific region[J]. Haiyang Xuebao, 2019, 41(5): 79-96. doi: 10.3969/j.issn.0253-4193.2019.05.008

Citation:

Yang Weili, Kang Yongshang, Yao Yongjian, Zhang Jianjun, Li Bo, Chen Hongwen, Wang Weihong. The evolution of basins and petroleum resource potential in the southern Pacific region[J]. Haiyang Xuebao, 2019, 41(5): 79-96. doi: 10.3969/j.issn.0253-4193.2019.05.008

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The evolution of basins and petroleum resource potential in the southern Pacific region

doi: 10.3969/j.issn.0253-4193.2019.05.008

1.
College of Geosciences, China University of Petroleum(Beijing), Beijing 102249, China
2.
College of Geosciences, China University of Petroleum(Beijing), Beijing 102249, China;State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum(Beijing), Beijing 102249, China
3.
Guangzhou Marine Geological Survey, Guangzhou 510760, China
4.
Beijing Petropark Co., Ltd., Beijing 102200, China

Received Date: 2018-07-06

Abstract

Abstract

Based on regional tectonic evolution history, basin types in the southern Pacific region are classified and the petroleum geology of the major basin types is studied. The petroleum occurrences and resource potential are finally analysed in an objective to provide support for international cooperation between countries. Our studies show that:(1) The southern Pacific region underwent four stages including Hunter-Bowen orogeny, Antarctic Plate separates form the Australia Plate, the Tasman and Coral seas expending and oceanic crust subduction and arc-land collision occurred in Papua New Guinea, and formed six types of basin that is cratonic basin, rift basin, late permian-triassic foreland basin, paleogene-neogene foreland basin, paleogene-present forearc basin and the back-arc basin. The eastern inland of Australia is mainly the cratonic basin, and the southern margin and sea area of eastern Australia and the New Zealand are mainly the rift basin; (2) The rift margin basin is widely distributed in the south of Australia and the sea area of eastern Australia and the New Zealand. The most concentrated oil and gas accumulation in the rift basin in the study area, but the southern and eastern regions are different, the ratio of oil to gas is about 2:1 in the south margin rift basin. However, there is no hydrocarbon accumulation in the rift basin in the eastern sea because of poor hydrocarbon accumulation conditions; (3) According to the remaining recoverable reserves and prospective resource in basin, analyze the resource potential of sedimentary basins in the eastern of Australia. It is believed that the oil and gas resources in the cretaceous-paleogene rift basin and the paleogene-neogene foreland basin have the greatest potential, and the Gippsland Basin, Taranaki Basin and Papua Basin are optimized as favorable ones for hydrocarbon exploration in the southern Pacific region.
- southern Pacific region,
- plate evolution,
- type of basins,
- accumulation characteristics,
- resource potential1

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References(39)

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