The control of small-scale syndepositional normal faults on sandstone distribution: example from the Paleogene bottom Sandstone Member in the Tabei Uplift, Tarim Basin, China

IntroductionThe syndepositional normal faults related paleogeomorphic units in sedimentary basins play a crucial role in controlling sediment transport and infill processes. Previous studies have primarily focused on the control of depositional systems by large-scale syndepositional faults. However,...

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Main Authors: Gao Xiaoyang, Dou Luxing, He Wenxiang, Sun Qi, Yi Zhenli, Li Bin, He Qiaolin, Jin Jineng, Hu Yong, Yan Jingwen, Zhang Li
Format: Article
Language:English
Published: Frontiers Media S.A. 2025-03-01
Series:Frontiers in Earth Science
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Online Access:https://www.frontiersin.org/articles/10.3389/feart.2025.1568199/full
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author Gao Xiaoyang
Dou Luxing
He Wenxiang
Sun Qi
Yi Zhenli
Li Bin
He Qiaolin
Jin Jineng
Hu Yong
Yan Jingwen
Zhang Li
author_facet Gao Xiaoyang
Dou Luxing
He Wenxiang
Sun Qi
Yi Zhenli
Li Bin
He Qiaolin
Jin Jineng
Hu Yong
Yan Jingwen
Zhang Li
author_sort Gao Xiaoyang
collection DOAJ
description IntroductionThe syndepositional normal faults related paleogeomorphic units in sedimentary basins play a crucial role in controlling sediment transport and infill processes. Previous studies have primarily focused on the control of depositional systems by large-scale syndepositional faults. However, there is still a lack of systematic understanding about the control of intensively developed small-scale syndepositional normal faults on sandstone facies distribution in continental basin.MethodsThis study integrates 3D seismic data, well logs, and core descriptions to determine the depositional facies and small-scale syndepositional normal fault related paleogeomorphology are consistent during deposition of the Paleogene Bottom Sandstone Member of the WM7 fault zone area in the Tabei Uplift, Tarim basin.ResultsThe results indicate that the Paleogene Bottom Sandstone Member consists of deltaic sandstone facies and fine-grained lacustrine deposits containing evaporites near an erosional uplift. During the deposition of the Bottom Sandstone Member, an erosional uplift zone developed in the eastern part of the WM7 fault zone, where numerous incised valleys formed. In contrast, the fault zone and its western region were characterized by a delta–saline lake depositional system controlled by a syndepositional graben, with numerous small-scale en echelon syndepositional faults developing within the fault zone.DiscussionThese special geomorphic units composed of syndepositional faults were primarily formed by differential subsidence of strata. These faults and their associated paleogeomorphic units controlled the distribution characteristics of incised valleys and distributary channels. By analyzing the control exerted by micro - geomorphic units composed of syndepositional normal faults near the paleo-uplift on the distribution of sandstone, new insights are provided for predicting the distribution of sandstone in complex geomorphic units formed by small-scale syndepositional fault combinations in continental basins.
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spelling doaj-art-daf8e53355ba40ecb98fa0b3fdb17eee2025-08-20T03:44:27ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632025-03-011310.3389/feart.2025.15681991568199The control of small-scale syndepositional normal faults on sandstone distribution: example from the Paleogene bottom Sandstone Member in the Tabei Uplift, Tarim Basin, ChinaGao Xiaoyang0Dou Luxing1He Wenxiang2Sun Qi3Yi Zhenli4Li Bin5He Qiaolin6Jin Jineng7Hu Yong8Yan Jingwen9Zhang Li10College of Resources and Environment, Yangtze University, Wuhan, ChinaCollege of Resources and Environment, Yangtze University, Wuhan, ChinaCollege of Resources and Environment, Yangtze University, Wuhan, ChinaResearch Institute of Exploration and Development, Tarim Oilfield Company, CNPC, Korla, ChinaResearch Institute of Exploration and Development, Tarim Oilfield Company, CNPC, Korla, ChinaResearch Institute of Exploration and Development, Tarim Oilfield Company, CNPC, Korla, ChinaResearch Institute of Exploration and Development, Tarim Oilfield Company, CNPC, Korla, ChinaSchool of Geosciences, Yangtze University, Wuhan, ChinaCollege of Resources and Environment, Yangtze University, Wuhan, ChinaResearch Institute of Exploration and Development, Tarim Oilfield Company, CNPC, Korla, ChinaSchool of Geosciences, Yangtze University, Wuhan, ChinaIntroductionThe syndepositional normal faults related paleogeomorphic units in sedimentary basins play a crucial role in controlling sediment transport and infill processes. Previous studies have primarily focused on the control of depositional systems by large-scale syndepositional faults. However, there is still a lack of systematic understanding about the control of intensively developed small-scale syndepositional normal faults on sandstone facies distribution in continental basin.MethodsThis study integrates 3D seismic data, well logs, and core descriptions to determine the depositional facies and small-scale syndepositional normal fault related paleogeomorphology are consistent during deposition of the Paleogene Bottom Sandstone Member of the WM7 fault zone area in the Tabei Uplift, Tarim basin.ResultsThe results indicate that the Paleogene Bottom Sandstone Member consists of deltaic sandstone facies and fine-grained lacustrine deposits containing evaporites near an erosional uplift. During the deposition of the Bottom Sandstone Member, an erosional uplift zone developed in the eastern part of the WM7 fault zone, where numerous incised valleys formed. In contrast, the fault zone and its western region were characterized by a delta–saline lake depositional system controlled by a syndepositional graben, with numerous small-scale en echelon syndepositional faults developing within the fault zone.DiscussionThese special geomorphic units composed of syndepositional faults were primarily formed by differential subsidence of strata. These faults and their associated paleogeomorphic units controlled the distribution characteristics of incised valleys and distributary channels. By analyzing the control exerted by micro - geomorphic units composed of syndepositional normal faults near the paleo-uplift on the distribution of sandstone, new insights are provided for predicting the distribution of sandstone in complex geomorphic units formed by small-scale syndepositional fault combinations in continental basins.https://www.frontiersin.org/articles/10.3389/feart.2025.1568199/fullseismic sedimentologysandstone distributionsyndepositional faultsalt lake-deltatabei upliftpaleogene
spellingShingle Gao Xiaoyang
Dou Luxing
He Wenxiang
Sun Qi
Yi Zhenli
Li Bin
He Qiaolin
Jin Jineng
Hu Yong
Yan Jingwen
Zhang Li
The control of small-scale syndepositional normal faults on sandstone distribution: example from the Paleogene bottom Sandstone Member in the Tabei Uplift, Tarim Basin, China
Frontiers in Earth Science
seismic sedimentology
sandstone distribution
syndepositional fault
salt lake-delta
tabei uplift
paleogene
title The control of small-scale syndepositional normal faults on sandstone distribution: example from the Paleogene bottom Sandstone Member in the Tabei Uplift, Tarim Basin, China
title_full The control of small-scale syndepositional normal faults on sandstone distribution: example from the Paleogene bottom Sandstone Member in the Tabei Uplift, Tarim Basin, China
title_fullStr The control of small-scale syndepositional normal faults on sandstone distribution: example from the Paleogene bottom Sandstone Member in the Tabei Uplift, Tarim Basin, China
title_full_unstemmed The control of small-scale syndepositional normal faults on sandstone distribution: example from the Paleogene bottom Sandstone Member in the Tabei Uplift, Tarim Basin, China
title_short The control of small-scale syndepositional normal faults on sandstone distribution: example from the Paleogene bottom Sandstone Member in the Tabei Uplift, Tarim Basin, China
title_sort control of small scale syndepositional normal faults on sandstone distribution example from the paleogene bottom sandstone member in the tabei uplift tarim basin china
topic seismic sedimentology
sandstone distribution
syndepositional fault
salt lake-delta
tabei uplift
paleogene
url https://www.frontiersin.org/articles/10.3389/feart.2025.1568199/full
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