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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
Abstract
AAPG Bulletin, V.
2009. The American Association of Petroleum Geologists. All rights reserved.
DOI:10.1306/09080808092
Charging of the Neogene Penglai 19-3 field, Bohai Bay Basin, China:
Oil
accumulation in a young trap in an active fault zone
Oil
accumulation in a young trap in an active fault zone
Fang Hao,1 Xinhuai Zhou,2 Yangming Zhu,3 Xiaohuan Bao,4 Yuanyuan Yang5
1State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Fuxue Road No. 18, Changping, Beijing 102249, China; [email protected]
2Tianjin Branch of China National Offshore
Oil
Company Ltd., Tianjin 300452, China
3Department of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang 310027, China
4State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
5State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Fuxue Road No. 18, Changping, Beijing 102249, China
ABSTRACT
The Penglai 19-3 (PL19-3)
oil
field, the largest offshore
oil
field in China, was found in shallow reservoirs (700–1700 m, 2297–5577 ft) within the most active fault zone in east China. The PL19-3 anticline was not finally formed until about 2.0 Ma and is cut by densely distributed faults. Source
rock
and crude
oil
samples from the PL19-3 field were analyzed to determine the origin and formation mechanisms of this large
oil
field. Three organic-rich,
oil
-prone source
rock
intervals exist in the Bozhong subbasin, each of which has a distinct biomarker assemblage.
Oil
samples from different wells have different biomarker associations, and three source-related
oil
classes were identified within the PL19-3 field based on biomarker compositions and multivariate analysis of the data. The PL19-3 field displays considerable compositional heterogeneity. The compositional heterogeneity within the field and comparison between
oil
samples from the PL19-3 field and those from nearby structures suggest three field-filling directions, which is consistent with the results of migration pathway modeling. The PL19-3 field was charged in the north by
oil
generated from Dongying Formation source rocks in the eastern Bozhong depression and Bodong depression, in the southeast by
oil
generated from Shahejie Formation source rocks in the Miaoxi depression, and in the northwest by
oil
generated from Shahejie Formation source rocks in the central Bozhong depression.
Oil
charge from multiple source
rock
intervals and multiple generative kitchens and focusing of
oil
originating from a large area of the Bozhong depression into the same trap resulted in rapid
oil
accumulation in the PL19-3 structure and the formation of this large
oil
field in a very young trap within an active fault zone.
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