Strike-slip structures and hydrocarbon accumulation in complex fault blocks in Subei Basin

The research on basin formation and hydrocarbon generation and accumulation in the Subei Basin was carried out based on structural geometry and kinematic analyses. The Subei Basin has experienced three evolutionary stages: rift-subsiding, fault depression and depression. During the tectonic developm...

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Main Authors: Xuming QIU, Wei CHEN, Heyong LI, Hongliang DUAN
Format: Article
Language:zho
Published: Editorial Office of Petroleum Geology and Experiment 2023-05-01
Series:Shiyou shiyan dizhi
Subjects:
Online Access:https://www.sysydz.net/cn/article/doi/10.11781/sysydz202303393
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author Xuming QIU
Wei CHEN
Heyong LI
Hongliang DUAN
author_facet Xuming QIU
Wei CHEN
Heyong LI
Hongliang DUAN
author_sort Xuming QIU
collection DOAJ
description The research on basin formation and hydrocarbon generation and accumulation in the Subei Basin was carried out based on structural geometry and kinematic analyses. The Subei Basin has experienced three evolutionary stages: rift-subsiding, fault depression and depression. During the tectonic development dominated by extension and tension in the Himalayan period in the eastern China, there were echelon, pinnate, broom-like and other strike-slip fault combinations in the basin, and it has been found that oil reservoirs and traps were directionally arranged and closely related to strike-slip actions. The extension and strike-slip process controlled basin formation and evolution, which resulted in the oblique arrangement of sags, and formed multiple hydrocarbon generation sub-sags in each sag. The differential development characteristics of basin-controlling and sag-controlling faults controlled the main migration directions of oil and gas, forming three migration modes. The oil and gas migration patterns under the control of echelon and pinnate sag-controlling faults were quite different. The fault transform zone and structural high zone formed by secondary fault combination and formation deformation are important places for oil and gas enrichment, and many types of fault nose and fault block reservoirs were formed.
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spelling doaj.art-67c9e5d392414f5593bd51f70bce3bb12024-03-05T03:20:30ZzhoEditorial Office of Petroleum Geology and ExperimentShiyou shiyan dizhi1001-61122023-05-0145339340110.11781/sysydz202303393sysydz-45-3-393Strike-slip structures and hydrocarbon accumulation in complex fault blocks in Subei BasinXuming QIU0Wei CHEN1Heyong LI2Hongliang DUAN3SINOPEC Jiangsu Oilfield Branch Company, Yangzhou, Jiangsu 225009, ChinaSINOPEC Jiangsu Oilfield Branch Company, Yangzhou, Jiangsu 225009, ChinaSINOPEC Jiangsu Oilfield Branch Company, Yangzhou, Jiangsu 225009, ChinaSINOPEC Jiangsu Oilfield Branch Company, Yangzhou, Jiangsu 225009, ChinaThe research on basin formation and hydrocarbon generation and accumulation in the Subei Basin was carried out based on structural geometry and kinematic analyses. The Subei Basin has experienced three evolutionary stages: rift-subsiding, fault depression and depression. During the tectonic development dominated by extension and tension in the Himalayan period in the eastern China, there were echelon, pinnate, broom-like and other strike-slip fault combinations in the basin, and it has been found that oil reservoirs and traps were directionally arranged and closely related to strike-slip actions. The extension and strike-slip process controlled basin formation and evolution, which resulted in the oblique arrangement of sags, and formed multiple hydrocarbon generation sub-sags in each sag. The differential development characteristics of basin-controlling and sag-controlling faults controlled the main migration directions of oil and gas, forming three migration modes. The oil and gas migration patterns under the control of echelon and pinnate sag-controlling faults were quite different. The fault transform zone and structural high zone formed by secondary fault combination and formation deformation are important places for oil and gas enrichment, and many types of fault nose and fault block reservoirs were formed.https://www.sysydz.net/cn/article/doi/10.11781/sysydz202303393extension and strike-slipfault transform zonestructural high zoneoil and gas enrichmentsubei basin
spellingShingle Xuming QIU
Wei CHEN
Heyong LI
Hongliang DUAN
Strike-slip structures and hydrocarbon accumulation in complex fault blocks in Subei Basin
Shiyou shiyan dizhi
extension and strike-slip
fault transform zone
structural high zone
oil and gas enrichment
subei basin
title Strike-slip structures and hydrocarbon accumulation in complex fault blocks in Subei Basin
title_full Strike-slip structures and hydrocarbon accumulation in complex fault blocks in Subei Basin
title_fullStr Strike-slip structures and hydrocarbon accumulation in complex fault blocks in Subei Basin
title_full_unstemmed Strike-slip structures and hydrocarbon accumulation in complex fault blocks in Subei Basin
title_short Strike-slip structures and hydrocarbon accumulation in complex fault blocks in Subei Basin
title_sort strike slip structures and hydrocarbon accumulation in complex fault blocks in subei basin
topic extension and strike-slip
fault transform zone
structural high zone
oil and gas enrichment
subei basin
url https://www.sysydz.net/cn/article/doi/10.11781/sysydz202303393
work_keys_str_mv AT xumingqiu strikeslipstructuresandhydrocarbonaccumulationincomplexfaultblocksinsubeibasin
AT weichen strikeslipstructuresandhydrocarbonaccumulationincomplexfaultblocksinsubeibasin
AT heyongli strikeslipstructuresandhydrocarbonaccumulationincomplexfaultblocksinsubeibasin
AT hongliangduan strikeslipstructuresandhydrocarbonaccumulationincomplexfaultblocksinsubeibasin