Controls on Gas-Reservoir Formation in the Benxi Formation in the Ganquan–Fuxian Area of the Ordos Basin, China

The Benxi Formation is one of the most important gas-producing layers in the Ganquan–Fuxian area, but the complex gas–water distribution and lack of sandstone have severely constrained natural gas exploration and development in this area. This study analyzed the structure, paleogeomorphology, sedime...

وصف كامل

التفاصيل البيبلوغرافية
الحاوية / القاعدة:Energies
المؤلفون الرئيسيون: Ming Song, Xiangzhen Meng, Renhai Pu, Xiaoping Gao, Teng Qiang, Yujie Fan
التنسيق: مقال
اللغة:الإنجليزية
منشور في: MDPI AG 2023-09-01
الموضوعات:
الوصول للمادة أونلاين:https://www.mdpi.com/1996-1073/16/19/6866
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author Ming Song
Xiangzhen Meng
Renhai Pu
Xiaoping Gao
Teng Qiang
Yujie Fan
author_facet Ming Song
Xiangzhen Meng
Renhai Pu
Xiaoping Gao
Teng Qiang
Yujie Fan
author_sort Ming Song
collection DOAJ
container_title Energies
description The Benxi Formation is one of the most important gas-producing layers in the Ganquan–Fuxian area, but the complex gas–water distribution and lack of sandstone have severely constrained natural gas exploration and development in this area. This study analyzed the structure, paleogeomorphology, sedimentary facies, reservoir closures, and gas–water distribution of the Benxi Formation in the study area through drilling, coring, logging, seismic surveying, and experimental testing. The results show that the gas reservoirs in the Benxi Formation are mainly lithologic traps distributed along NW-trending barrier sandstones, with a small portion of updip pinchout closures. The water layers are mainly composed of thin sandstones with a single-layer thickness of less than 2 m, which are tidal-channel or barrier-margin microfacies sandstones. The water saturation in some thick sandstones is related to the activity and destruction of large individual faults. The dry layers are tight sandstones with porosity of less than 3.2%, mainly associated with high amounts of volcaniclastic matrix and lithic fragments, as well as compaction. The charging of the underlying high-quality Ordovician limestone reservoirs by carboniferous source rocks in the Benxi Formation reduces the probability of gas accumulation in Benxi sandstone. Based on the control of sedimentary facies and physical properties on gas accumulation, favorable reservoir distributions were predicted using seismic attributes and gas detection methods, providing the basis for the next phase of natural gas exploration and development in this area.
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spelling doaj-art-e52886c8d8dc41f79b74ea6ae95c52512025-08-19T22:45:18ZengMDPI AGEnergies1996-10732023-09-011619686610.3390/en16196866Controls on Gas-Reservoir Formation in the Benxi Formation in the Ganquan–Fuxian Area of the Ordos Basin, ChinaMing Song0Xiangzhen Meng1Renhai Pu2Xiaoping Gao3Teng Qiang4Yujie Fan5Department of Geology, Northwest University, Xi’an 710069, ChinaShaanxi Yanchang Petroleum (Group) Corp. Ltd., Xi’an 710065, ChinaDepartment of Geology, Northwest University, Xi’an 710069, ChinaShaanxi Yanchang Petroleum (Group) Corp. Ltd., Xi’an 710065, ChinaShaanxi Yanchang Petroleum (Group) Corp. Ltd., Xi’an 710065, ChinaDepartment of Geology, Northwest University, Xi’an 710069, ChinaThe Benxi Formation is one of the most important gas-producing layers in the Ganquan–Fuxian area, but the complex gas–water distribution and lack of sandstone have severely constrained natural gas exploration and development in this area. This study analyzed the structure, paleogeomorphology, sedimentary facies, reservoir closures, and gas–water distribution of the Benxi Formation in the study area through drilling, coring, logging, seismic surveying, and experimental testing. The results show that the gas reservoirs in the Benxi Formation are mainly lithologic traps distributed along NW-trending barrier sandstones, with a small portion of updip pinchout closures. The water layers are mainly composed of thin sandstones with a single-layer thickness of less than 2 m, which are tidal-channel or barrier-margin microfacies sandstones. The water saturation in some thick sandstones is related to the activity and destruction of large individual faults. The dry layers are tight sandstones with porosity of less than 3.2%, mainly associated with high amounts of volcaniclastic matrix and lithic fragments, as well as compaction. The charging of the underlying high-quality Ordovician limestone reservoirs by carboniferous source rocks in the Benxi Formation reduces the probability of gas accumulation in Benxi sandstone. Based on the control of sedimentary facies and physical properties on gas accumulation, favorable reservoir distributions were predicted using seismic attributes and gas detection methods, providing the basis for the next phase of natural gas exploration and development in this area.https://www.mdpi.com/1996-1073/16/19/6866Benxi Formationpaleogeomorphicsedimentary faciesreservoir control factor
spellingShingle Ming Song
Xiangzhen Meng
Renhai Pu
Xiaoping Gao
Teng Qiang
Yujie Fan
Controls on Gas-Reservoir Formation in the Benxi Formation in the Ganquan–Fuxian Area of the Ordos Basin, China
Benxi Formation
paleogeomorphic
sedimentary facies
reservoir control factor
title Controls on Gas-Reservoir Formation in the Benxi Formation in the Ganquan–Fuxian Area of the Ordos Basin, China
title_full Controls on Gas-Reservoir Formation in the Benxi Formation in the Ganquan–Fuxian Area of the Ordos Basin, China
title_fullStr Controls on Gas-Reservoir Formation in the Benxi Formation in the Ganquan–Fuxian Area of the Ordos Basin, China
title_full_unstemmed Controls on Gas-Reservoir Formation in the Benxi Formation in the Ganquan–Fuxian Area of the Ordos Basin, China
title_short Controls on Gas-Reservoir Formation in the Benxi Formation in the Ganquan–Fuxian Area of the Ordos Basin, China
title_sort controls on gas reservoir formation in the benxi formation in the ganquan fuxian area of the ordos basin china
topic Benxi Formation
paleogeomorphic
sedimentary facies
reservoir control factor
url https://www.mdpi.com/1996-1073/16/19/6866
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