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AAPG Bulletin

Abstract

AAPG Bulletin, V. 93, No. 2 (February 2009), P. 155-179.

Copyright copy2009. 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: Previous HitOilNext Hit 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 Previous HitOilNext Hit 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) Previous HitoilNext Hit field, the largest offshore Previous HitoilNext Hit 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 Previous HitrockNext Hit and crude Previous HitoilNext Hit samples from the PL19-3 field were analyzed to determine the origin and formation mechanisms of this large Previous HitoilNext Hit field. Three organic-rich, Previous HitoilNext Hit-prone source Previous HitrockNext Hit intervals exist in the Bozhong subbasin, each of which has a distinct biomarker assemblage. Previous HitOilNext Hit samples from different wells have different biomarker associations, and three source-related Previous HitoilNext Hit 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 Previous HitoilNext Hit 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 Previous HitoilNext Hit generated from Dongying Formation source rocks in the eastern Bozhong depression and Bodong depression, in the southeast by Previous HitoilNext Hit generated from Shahejie Formation source rocks in the Miaoxi depression, and in the northwest by Previous HitoilNext Hit generated from Shahejie Formation source rocks in the central Bozhong depression. Previous HitOilNext Hit charge from multiple source Previous HitrockNext Hit intervals and multiple generative kitchens and focusing of Previous HitoilNext Hit originating from a large area of the Bozhong depression into the same trap resulted in rapid Previous HitoilNext Hit accumulation in the PL19-3 structure and the formation of this large Previous HitoilNext Hit field in a very young trap within an active fault zone.

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