Geological Characteristics and Exploration Prospect of Black Shale in the Dongyuemiao Member of Lower Jurassic, the Eastern Sichuan Basin, China

China has yielded huge commercial production from the marine organic-rich shale but shows a slow exploration process in the lacustrine organic-rich shale. Multiple lacustrine shales in the Lower Jurassic of the eastern Sichuan Basin, rich in organic matters, are potential targets for shale hydrocarb...

Full description

Bibliographic Details
Main Authors: Guodong Wei, Wei Wang, Liang Feng, Xiucheng Tan, Chuan Yu, Hualian Zhang, Zhiping Zhang, Shengxiu Wang
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-11-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.765568/full
_version_ 1828957870765375488
author Guodong Wei
Guodong Wei
Guodong Wei
Wei Wang
Wei Wang
Liang Feng
Xiucheng Tan
Chuan Yu
Chuan Yu
Hualian Zhang
Hualian Zhang
Zhiping Zhang
Zhiping Zhang
Shengxiu Wang
Shengxiu Wang
author_facet Guodong Wei
Guodong Wei
Guodong Wei
Wei Wang
Wei Wang
Liang Feng
Xiucheng Tan
Chuan Yu
Chuan Yu
Hualian Zhang
Hualian Zhang
Zhiping Zhang
Zhiping Zhang
Shengxiu Wang
Shengxiu Wang
author_sort Guodong Wei
collection DOAJ
description China has yielded huge commercial production from the marine organic-rich shale but shows a slow exploration process in the lacustrine organic-rich shale. Multiple lacustrine shales in the Lower Jurassic of the eastern Sichuan Basin, rich in organic matters, are potential targets for shale hydrocarbon exploration and development. An investigation of the Dongyuemiao member, Lower Jurassic, was firstly conducted utilizing the macroscopic and microscopic analyses on outcrops and drilling cores to reveal the characteristics of sedimentary subfacies, mineral compositions, organic matter content and types, thermal maturity level, and reservoir quality. The dark shales in the Dongyuemiao member can be grouped into four general categories: shore, shallow, semi-deep, and deep lacustrine shales. The semi-deep and deep lacustrine shales generally have higher values in thickness (>20 m), average total organic carbon (TOC) content (>1.5 wt.%), and average porosity (>2%) relative to shore and shallow lacustrine shales. All four categories of shales primarily consist of type II kerogen and have thermal maturity levels exceeding the vitrinite reflectance value of 0.9–1.0% (or the Tmax of ∼440°C). Thermally powered pore generation generally promoted the pore system as indicated by the positive correlation between porosity and Tmax. Notably, the semi-deep lacustrine shale in the vicinity of the Qiyueshan Fault Zone shows abnormally high porosity and low oil saturation index (OSI) at Tmax>∼465°C potentially due to the promoted hydrocarbon expulsion through multiscale fractures. Except for the vicinity of the Qiyueshan Fault Zone, the semi-deep and deep lacustrine shales generally show the better exploration prospect relative to the shore and shallow lacustrine shales. Additionally, the high content of clay minerals (>40 wt%) reduced the brittleness of the semi-deep and deep lacustrine shales which may challenge the artificial hydraulic fracturing.
first_indexed 2024-12-14T08:38:17Z
format Article
id doaj.art-ca79ba6145974176a32c3701d3a527fd
institution Directory Open Access Journal
issn 2296-6463
language English
last_indexed 2024-12-14T08:38:17Z
publishDate 2021-11-01
publisher Frontiers Media S.A.
record_format Article
series Frontiers in Earth Science
spelling doaj.art-ca79ba6145974176a32c3701d3a527fd2022-12-21T23:09:22ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-11-01910.3389/feart.2021.765568765568Geological Characteristics and Exploration Prospect of Black Shale in the Dongyuemiao Member of Lower Jurassic, the Eastern Sichuan Basin, ChinaGuodong Wei0Guodong Wei1Guodong Wei2Wei Wang3Wei Wang4Liang Feng5Xiucheng Tan6Chuan Yu7Chuan Yu8Hualian Zhang9Hualian Zhang10Zhiping Zhang11Zhiping Zhang12Shengxiu Wang13Shengxiu Wang14Key Laboratory of Shale Gas Exploration, Ministry of Natural Resources, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaNational and Local Joint Engineering Research Center of Shale Gas Exploration and Development, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaSchool of Geoscience and Technology, Southwest Petroleum University, Chengdu, ChinaKey Laboratory of Shale Gas Exploration, Ministry of Natural Resources, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaNational and Local Joint Engineering Research Center of Shale Gas Exploration and Development, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaChongqing Gas Field, PetroChina Southwest Oil and Gas Field Company, Chongqing, ChinaSchool of Geoscience and Technology, Southwest Petroleum University, Chengdu, ChinaKey Laboratory of Shale Gas Exploration, Ministry of Natural Resources, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaNational and Local Joint Engineering Research Center of Shale Gas Exploration and Development, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaKey Laboratory of Shale Gas Exploration, Ministry of Natural Resources, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaNational and Local Joint Engineering Research Center of Shale Gas Exploration and Development, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaKey Laboratory of Shale Gas Exploration, Ministry of Natural Resources, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaNational and Local Joint Engineering Research Center of Shale Gas Exploration and Development, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaKey Laboratory of Shale Gas Exploration, Ministry of Natural Resources, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaNational and Local Joint Engineering Research Center of Shale Gas Exploration and Development, Chongqing Institute of Geology and Mineral Resources, Chongqing, ChinaChina has yielded huge commercial production from the marine organic-rich shale but shows a slow exploration process in the lacustrine organic-rich shale. Multiple lacustrine shales in the Lower Jurassic of the eastern Sichuan Basin, rich in organic matters, are potential targets for shale hydrocarbon exploration and development. An investigation of the Dongyuemiao member, Lower Jurassic, was firstly conducted utilizing the macroscopic and microscopic analyses on outcrops and drilling cores to reveal the characteristics of sedimentary subfacies, mineral compositions, organic matter content and types, thermal maturity level, and reservoir quality. The dark shales in the Dongyuemiao member can be grouped into four general categories: shore, shallow, semi-deep, and deep lacustrine shales. The semi-deep and deep lacustrine shales generally have higher values in thickness (>20 m), average total organic carbon (TOC) content (>1.5 wt.%), and average porosity (>2%) relative to shore and shallow lacustrine shales. All four categories of shales primarily consist of type II kerogen and have thermal maturity levels exceeding the vitrinite reflectance value of 0.9–1.0% (or the Tmax of ∼440°C). Thermally powered pore generation generally promoted the pore system as indicated by the positive correlation between porosity and Tmax. Notably, the semi-deep lacustrine shale in the vicinity of the Qiyueshan Fault Zone shows abnormally high porosity and low oil saturation index (OSI) at Tmax>∼465°C potentially due to the promoted hydrocarbon expulsion through multiscale fractures. Except for the vicinity of the Qiyueshan Fault Zone, the semi-deep and deep lacustrine shales generally show the better exploration prospect relative to the shore and shallow lacustrine shales. Additionally, the high content of clay minerals (>40 wt%) reduced the brittleness of the semi-deep and deep lacustrine shales which may challenge the artificial hydraulic fracturing.https://www.frontiersin.org/articles/10.3389/feart.2021.765568/fullshale porosityoil saturation indexlacustrine shaleDongyuemiao membersichuan basin
spellingShingle Guodong Wei
Guodong Wei
Guodong Wei
Wei Wang
Wei Wang
Liang Feng
Xiucheng Tan
Chuan Yu
Chuan Yu
Hualian Zhang
Hualian Zhang
Zhiping Zhang
Zhiping Zhang
Shengxiu Wang
Shengxiu Wang
Geological Characteristics and Exploration Prospect of Black Shale in the Dongyuemiao Member of Lower Jurassic, the Eastern Sichuan Basin, China
Frontiers in Earth Science
shale porosity
oil saturation index
lacustrine shale
Dongyuemiao member
sichuan basin
title Geological Characteristics and Exploration Prospect of Black Shale in the Dongyuemiao Member of Lower Jurassic, the Eastern Sichuan Basin, China
title_full Geological Characteristics and Exploration Prospect of Black Shale in the Dongyuemiao Member of Lower Jurassic, the Eastern Sichuan Basin, China
title_fullStr Geological Characteristics and Exploration Prospect of Black Shale in the Dongyuemiao Member of Lower Jurassic, the Eastern Sichuan Basin, China
title_full_unstemmed Geological Characteristics and Exploration Prospect of Black Shale in the Dongyuemiao Member of Lower Jurassic, the Eastern Sichuan Basin, China
title_short Geological Characteristics and Exploration Prospect of Black Shale in the Dongyuemiao Member of Lower Jurassic, the Eastern Sichuan Basin, China
title_sort geological characteristics and exploration prospect of black shale in the dongyuemiao member of lower jurassic the eastern sichuan basin china
topic shale porosity
oil saturation index
lacustrine shale
Dongyuemiao member
sichuan basin
url https://www.frontiersin.org/articles/10.3389/feart.2021.765568/full
work_keys_str_mv AT guodongwei geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT guodongwei geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT guodongwei geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT weiwang geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT weiwang geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT liangfeng geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT xiuchengtan geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT chuanyu geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT chuanyu geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT hualianzhang geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT hualianzhang geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT zhipingzhang geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT zhipingzhang geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT shengxiuwang geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina
AT shengxiuwang geologicalcharacteristicsandexplorationprospectofblackshaleinthedongyuemiaomemberoflowerjurassictheeasternsichuanbasinchina