Double provenance depositional model and exploration prospect in the deep-water area of Qiongdongnan Basin

Based on the newly collected seismic data and the provenance supply mode, the depositional sequence, provenance features, and oil-gas exploration prospects were analyzed. The study area has the typical double-layer geologic structure of rift-depression and has double provenance supply in the north a...

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Main Authors: Gen-shun YAO, Sheng-qiang YUAN, Shi-guo WU, Chuang ZHONG
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2008-12-01
Series:Petroleum Exploration and Development
Online Access:http://www.sciencedirect.com/science/article/pii/S1876380409601014
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author Gen-shun YAO
Sheng-qiang YUAN
Shi-guo WU
Chuang ZHONG
author_facet Gen-shun YAO
Sheng-qiang YUAN
Shi-guo WU
Chuang ZHONG
author_sort Gen-shun YAO
collection DOAJ
description Based on the newly collected seismic data and the provenance supply mode, the depositional sequence, provenance features, and oil-gas exploration prospects were analyzed. The study area has the typical double-layer geologic structure of rift-depression and has double provenance supply in the north and south. The provenance supply in rifting period was mainly from the southern Xisha Uplift and the southwestern Indo-China Peninsula and was also from the northern South China Block; whereas the provenance supply in post-rifting period was mainly from Indo-China Peninsula. In the rifting period, the southern sediment formed a large-scale progradation body in Lingshui Formation and encountered the subsea apron formed by the northern provenance in the central depression; in the post-rifting period, the large-scale turbidite channel developed in Sanya Formation, the large-scale reef developed in the southeast of the study area in Meishan Formation in the depositional stage, and the large-scale incised valleys developed in Huangliu Formation in the late depositional stage. In the Late Quaternary Period, the northern provenance and southern provenance joined in the deep-water area of Qiongdongnan Basin. The seismic data and basin modeling indicate that the reservoirs of subsea apron and sand-rich turbidite channel above the hydrocarbon-generating sag can be the good exploration targets in the deep-water area. Key words: Qiongdongnan Basin, double provenance, depositional model, deep-water hydrocarbon, exploration prospect
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spelling doaj.art-616bc6133ccb4b39aabce134d1da98f52022-12-21T22:23:44ZengKeAi Communications Co., Ltd.Petroleum Exploration and Development1876-38042008-12-01356685691Double provenance depositional model and exploration prospect in the deep-water area of Qiongdongnan BasinGen-shun YAO0Sheng-qiang YUAN1Shi-guo WU2Chuang ZHONG3Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; Graduate University of Chinese Academy of Sciences, Beijing 100049, China; PetroChina Hangzhou Institute of Geology, Hangzhou 310023, China; Corresponding authorKey Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; Graduate University of Chinese Academy of Sciences, Beijing 100049, ChinaKey Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; China University of Petroleum (Huadong), Qingdao 266555, ChinaLuliang Oil Production Company, PetroChina Xinjiang Oilfield Company, Karamay 834000, ChinaBased on the newly collected seismic data and the provenance supply mode, the depositional sequence, provenance features, and oil-gas exploration prospects were analyzed. The study area has the typical double-layer geologic structure of rift-depression and has double provenance supply in the north and south. The provenance supply in rifting period was mainly from the southern Xisha Uplift and the southwestern Indo-China Peninsula and was also from the northern South China Block; whereas the provenance supply in post-rifting period was mainly from Indo-China Peninsula. In the rifting period, the southern sediment formed a large-scale progradation body in Lingshui Formation and encountered the subsea apron formed by the northern provenance in the central depression; in the post-rifting period, the large-scale turbidite channel developed in Sanya Formation, the large-scale reef developed in the southeast of the study area in Meishan Formation in the depositional stage, and the large-scale incised valleys developed in Huangliu Formation in the late depositional stage. In the Late Quaternary Period, the northern provenance and southern provenance joined in the deep-water area of Qiongdongnan Basin. The seismic data and basin modeling indicate that the reservoirs of subsea apron and sand-rich turbidite channel above the hydrocarbon-generating sag can be the good exploration targets in the deep-water area. Key words: Qiongdongnan Basin, double provenance, depositional model, deep-water hydrocarbon, exploration prospecthttp://www.sciencedirect.com/science/article/pii/S1876380409601014
spellingShingle Gen-shun YAO
Sheng-qiang YUAN
Shi-guo WU
Chuang ZHONG
Double provenance depositional model and exploration prospect in the deep-water area of Qiongdongnan Basin
Petroleum Exploration and Development
title Double provenance depositional model and exploration prospect in the deep-water area of Qiongdongnan Basin
title_full Double provenance depositional model and exploration prospect in the deep-water area of Qiongdongnan Basin
title_fullStr Double provenance depositional model and exploration prospect in the deep-water area of Qiongdongnan Basin
title_full_unstemmed Double provenance depositional model and exploration prospect in the deep-water area of Qiongdongnan Basin
title_short Double provenance depositional model and exploration prospect in the deep-water area of Qiongdongnan Basin
title_sort double provenance depositional model and exploration prospect in the deep water area of qiongdongnan basin
url http://www.sciencedirect.com/science/article/pii/S1876380409601014
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