Formation conditions and accumulation characteristics of Bozhong 19-6 large condensate gas field in offshore Bohai Bay Basin

Based on the study of natural gas resource, low buried hill trap formation mechanism, high quality reservoir control factors and natural gas preservation conditions, the formation conditions and reservoir accumulation characteristics of Bozhong 19-6 large condensate gas field were summarized. Large...

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Main Authors: Changgui XU, Haibo YU, Jun WANG, Xiaojian LIU
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2019-02-01
Series:Petroleum Exploration and Development
Online Access:http://www.sciencedirect.com/science/article/pii/S1876380419300035
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spelling doaj-6ae300101d624eed8ee24841e0abc4742021-03-02T11:04:20ZengKeAi Communications Co., Ltd.Petroleum Exploration and Development1876-38042019-02-014612740Formation conditions and accumulation characteristics of Bozhong 19-6 large condensate gas field in offshore Bohai Bay BasinChanggui XU0Haibo YU1Jun WANG2Xiaojian LIU3Corresponding author; CNOOC China Limited, Tianjin Branch, Tianjin 300459, ChinaCNOOC China Limited, Tianjin Branch, Tianjin 300459, ChinaCNOOC China Limited, Tianjin Branch, Tianjin 300459, ChinaCNOOC China Limited, Tianjin Branch, Tianjin 300459, ChinaBased on the study of natural gas resource, low buried hill trap formation mechanism, high quality reservoir control factors and natural gas preservation conditions, the formation conditions and reservoir accumulation characteristics of Bozhong 19-6 large condensate gas field were summarized. Large gas generation potential of multiple sets of thick humic-sapropelic source rocks in high maturity stage in Bozhong depression was the basis of large gas field formation. The multi-stage tectonic evolution since Indosinian period formed large-scale buried hill traps. The Tanlu fault activity formed multi-type reservoirs, and buried hill metamorphic rock of Archean and sand-conglomerate of Kongdian Formation were high-quality reservoirs. Thick overpressure lacustrine mudstone and weak neotectonic movement provided good preservation conditions. Bozhong 19-6 gas reservoir was a condensate gas reservoir with very high condensate oil content, and the gas origin was humic-sapropelic and kerogen-cracking gas, and the gas field had large gas thickness, high gas column characteristics and the accumulation process was first oil and then gas. The buried hill reservoir was a massive reservoir and the Kongdian reservoir was a stratified reservoir. The gas field had multi-channel hydrocarbon intense charge from overpressure source rocks, atmospheric-weak overpressure reservoir favorable for accumulation, thick overpressure mudstone caprock favorable for preservation, and natural gas ultra-late rapid accumulation model. Key words: offshore Bohai Bay Basin, Bozhong 19-6 gas field, condensate gas, low buried hill, metamorphic rock reservoir, accumulation characteristics, Archeanhttp://www.sciencedirect.com/science/article/pii/S1876380419300035
collection DOAJ
language English
format Article
sources DOAJ
author Changgui XU
Haibo YU
Jun WANG
Xiaojian LIU
spellingShingle Changgui XU
Haibo YU
Jun WANG
Xiaojian LIU
Formation conditions and accumulation characteristics of Bozhong 19-6 large condensate gas field in offshore Bohai Bay Basin
Petroleum Exploration and Development
author_facet Changgui XU
Haibo YU
Jun WANG
Xiaojian LIU
author_sort Changgui XU
title Formation conditions and accumulation characteristics of Bozhong 19-6 large condensate gas field in offshore Bohai Bay Basin
title_short Formation conditions and accumulation characteristics of Bozhong 19-6 large condensate gas field in offshore Bohai Bay Basin
title_full Formation conditions and accumulation characteristics of Bozhong 19-6 large condensate gas field in offshore Bohai Bay Basin
title_fullStr Formation conditions and accumulation characteristics of Bozhong 19-6 large condensate gas field in offshore Bohai Bay Basin
title_full_unstemmed Formation conditions and accumulation characteristics of Bozhong 19-6 large condensate gas field in offshore Bohai Bay Basin
title_sort formation conditions and accumulation characteristics of bozhong 19-6 large condensate gas field in offshore bohai bay basin
publisher KeAi Communications Co., Ltd.
series Petroleum Exploration and Development
issn 1876-3804
publishDate 2019-02-01
description Based on the study of natural gas resource, low buried hill trap formation mechanism, high quality reservoir control factors and natural gas preservation conditions, the formation conditions and reservoir accumulation characteristics of Bozhong 19-6 large condensate gas field were summarized. Large gas generation potential of multiple sets of thick humic-sapropelic source rocks in high maturity stage in Bozhong depression was the basis of large gas field formation. The multi-stage tectonic evolution since Indosinian period formed large-scale buried hill traps. The Tanlu fault activity formed multi-type reservoirs, and buried hill metamorphic rock of Archean and sand-conglomerate of Kongdian Formation were high-quality reservoirs. Thick overpressure lacustrine mudstone and weak neotectonic movement provided good preservation conditions. Bozhong 19-6 gas reservoir was a condensate gas reservoir with very high condensate oil content, and the gas origin was humic-sapropelic and kerogen-cracking gas, and the gas field had large gas thickness, high gas column characteristics and the accumulation process was first oil and then gas. The buried hill reservoir was a massive reservoir and the Kongdian reservoir was a stratified reservoir. The gas field had multi-channel hydrocarbon intense charge from overpressure source rocks, atmospheric-weak overpressure reservoir favorable for accumulation, thick overpressure mudstone caprock favorable for preservation, and natural gas ultra-late rapid accumulation model. Key words: offshore Bohai Bay Basin, Bozhong 19-6 gas field, condensate gas, low buried hill, metamorphic rock reservoir, accumulation characteristics, Archean
url http://www.sciencedirect.com/science/article/pii/S1876380419300035
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