Reservoir characteristics and genetic differences between the second and fourth members of Sinian Dengying Formation in northern Sichuan Basin and its surrounding areas

This study investigated the characteristics and genesis of reservoirs in the 2nd and 4th members of Sinian Dengying Formation in northern Sichuan and its surrounding areas, on the basis of outcrop, drilling cores and thin section observation and geochemical analysis. The reservoirs of 2nd member are...

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Main Authors: Yong LI, Xingzhi WANG, Mingyou FENG, Deming ZENG, Shengyang XIE, Rui FAN, Liangjun WANG, Tao ZENG, Xuefei YANG
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/S1876380419300059
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spelling doaj-d3571fa23e6a407a9d46e14eb975ce7a2021-02-02T03:25:35ZengKeAi Communications Co., Ltd.Petroleum Exploration and Development1876-38042019-02-014615466Reservoir characteristics and genetic differences between the second and fourth members of Sinian Dengying Formation in northern Sichuan Basin and its surrounding areasYong LI0Xingzhi WANG1Mingyou FENG2Deming ZENG3Shengyang XIE4Rui FAN5Liangjun WANG6Tao ZENG7Xuefei YANG8State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu 610500, China; School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu 610500, China; School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China; Corresponding authorSchool of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, ChinaSchool of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu 610500, China; School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, ChinaSinopec Exploration Company, Chengdu 610041, ChinaSinopec Exploration Company, Chengdu 610041, ChinaSinopec Exploration Company, Chengdu 610041, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu 610500, China; School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, ChinaThis study investigated the characteristics and genesis of reservoirs in the 2nd and 4th members of Sinian Dengying Formation in northern Sichuan and its surrounding areas, on the basis of outcrop, drilling cores and thin section observation and geochemical analysis. The reservoirs of 2nd member are distributed in the middle part of the stratum. The reservoir quality is controlled by supergene karst and the distribution of mound-shoal complex. The bedded elongated isolated algal framework solution-cave and the residual “grape-lace” cave, which are partially filled with multi-stage dolosparite, constituted the main reservoir space of the 2nd member. There is no asphalt distribution in the pores. The pore connectivity is poor, and the porosity and permeability of the reservoir is relatively low. The reservoirs of 4th member were distributed in the upper and top part of the stratum. The reservoir quality is controlled by burial dissolution and the distribution of mound-shoal complex. The bedded algal framework solution-pores or caves, intercrystalline pores and intercrystalline dissolved pores constituted the main reservoir space of the 4th member. It's partially filled with asphalt and quartz, without any dolosparite fillings in the pores and caves. The pore connectivity is good. Most of the 4th member reservoirs had medium-low porosity and low permeability, and, locally, medium-high porosity and medium permeability. Affected by the development of mound-shoal complex and heterogeneous dissolution, the platform margin along Ningqiang, Guangyuan, Jiange and Langzhong is the most favorable region for reservoir development. Deep buried Dengying Formation in the guangyuan and langzhong areas should be the most important hydrocarbon target for the future exploration. Key words: Sichuan Basin, northern Sichuan area, Sinian, Dengying Formation, mound-shoal complex, supergene karst, burial dissolution, reservoirhttp://www.sciencedirect.com/science/article/pii/S1876380419300059
collection DOAJ
language English
format Article
sources DOAJ
author Yong LI
Xingzhi WANG
Mingyou FENG
Deming ZENG
Shengyang XIE
Rui FAN
Liangjun WANG
Tao ZENG
Xuefei YANG
spellingShingle Yong LI
Xingzhi WANG
Mingyou FENG
Deming ZENG
Shengyang XIE
Rui FAN
Liangjun WANG
Tao ZENG
Xuefei YANG
Reservoir characteristics and genetic differences between the second and fourth members of Sinian Dengying Formation in northern Sichuan Basin and its surrounding areas
Petroleum Exploration and Development
author_facet Yong LI
Xingzhi WANG
Mingyou FENG
Deming ZENG
Shengyang XIE
Rui FAN
Liangjun WANG
Tao ZENG
Xuefei YANG
author_sort Yong LI
title Reservoir characteristics and genetic differences between the second and fourth members of Sinian Dengying Formation in northern Sichuan Basin and its surrounding areas
title_short Reservoir characteristics and genetic differences between the second and fourth members of Sinian Dengying Formation in northern Sichuan Basin and its surrounding areas
title_full Reservoir characteristics and genetic differences between the second and fourth members of Sinian Dengying Formation in northern Sichuan Basin and its surrounding areas
title_fullStr Reservoir characteristics and genetic differences between the second and fourth members of Sinian Dengying Formation in northern Sichuan Basin and its surrounding areas
title_full_unstemmed Reservoir characteristics and genetic differences between the second and fourth members of Sinian Dengying Formation in northern Sichuan Basin and its surrounding areas
title_sort reservoir characteristics and genetic differences between the second and fourth members of sinian dengying formation in northern sichuan basin and its surrounding areas
publisher KeAi Communications Co., Ltd.
series Petroleum Exploration and Development
issn 1876-3804
publishDate 2019-02-01
description This study investigated the characteristics and genesis of reservoirs in the 2nd and 4th members of Sinian Dengying Formation in northern Sichuan and its surrounding areas, on the basis of outcrop, drilling cores and thin section observation and geochemical analysis. The reservoirs of 2nd member are distributed in the middle part of the stratum. The reservoir quality is controlled by supergene karst and the distribution of mound-shoal complex. The bedded elongated isolated algal framework solution-cave and the residual “grape-lace” cave, which are partially filled with multi-stage dolosparite, constituted the main reservoir space of the 2nd member. There is no asphalt distribution in the pores. The pore connectivity is poor, and the porosity and permeability of the reservoir is relatively low. The reservoirs of 4th member were distributed in the upper and top part of the stratum. The reservoir quality is controlled by burial dissolution and the distribution of mound-shoal complex. The bedded algal framework solution-pores or caves, intercrystalline pores and intercrystalline dissolved pores constituted the main reservoir space of the 4th member. It's partially filled with asphalt and quartz, without any dolosparite fillings in the pores and caves. The pore connectivity is good. Most of the 4th member reservoirs had medium-low porosity and low permeability, and, locally, medium-high porosity and medium permeability. Affected by the development of mound-shoal complex and heterogeneous dissolution, the platform margin along Ningqiang, Guangyuan, Jiange and Langzhong is the most favorable region for reservoir development. Deep buried Dengying Formation in the guangyuan and langzhong areas should be the most important hydrocarbon target for the future exploration. Key words: Sichuan Basin, northern Sichuan area, Sinian, Dengying Formation, mound-shoal complex, supergene karst, burial dissolution, reservoir
url http://www.sciencedirect.com/science/article/pii/S1876380419300059
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