Lacustrine carbonates in the southwest margin of the Qikou Sag, Huanghua Depression, Bohai Bay Basin

The southwest margin of the Qikou Sag is a flexural gentle slope formed by the deformation of a drape structure due to its underlying basement lifting. The sedimentary period of the Lower Member 1 of Shahejie Formation is the maximum extensional time of the Paleogene lacustrine basin. Debris from so...

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Main Authors: Xiugang Pu, Lihong Zhou, Dunqing Xiao, Shuangjun Hua, Changwei Chen, Xuanjun Yuan, Guomeng Han, Wei Zhang
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2011-04-01
Series:Petroleum Exploration and Development
Online Access:http://www.sciencedirect.com/science/article/pii/S1876380411600220
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author Xiugang Pu
Lihong Zhou
Dunqing Xiao
Shuangjun Hua
Changwei Chen
Xuanjun Yuan
Guomeng Han
Wei Zhang
author_facet Xiugang Pu
Lihong Zhou
Dunqing Xiao
Shuangjun Hua
Changwei Chen
Xuanjun Yuan
Guomeng Han
Wei Zhang
author_sort Xiugang Pu
collection DOAJ
description The southwest margin of the Qikou Sag is a flexural gentle slope formed by the deformation of a drape structure due to its underlying basement lifting. The sedimentary period of the Lower Member 1 of Shahejie Formation is the maximum extensional time of the Paleogene lacustrine basin. Debris from source areas is in shortage. In the broad littoral shallow lake, hundreds of square kilometers of lacustrine carbonates are deposited and distributed stably. The main lithologies of the sediments are biolithite and dolomite (micritic dolomite and dolomitic limestone), and the dolomites are mainly middle late buried dolomite and penecontemporaneous dolomite. Their distribution area is more than 1 650 m2, the cumulative thickness is between 5 and 25 meters, and the average thickness is about 10 meters. Intercrystal pores, intergranular pores, corrosion pores and frequent fissures are developed in the medium porosity and low permeability dolomite reservoirs. The dolomites alternate with oil shale and dark mudstone, favorable for the charge of low mature hydrocarbons and the formation of large scale accumulations. Drilling exploration practices show that the lacustrine dolomite reservoirs are characterized by medium burial depth and regional petroleum accumulation and are a new exploration area for Paleogene oil and gas. Key words: Qikou Sag, Shahejie Formation Lower Member 1, lacustrine carbonates, lithofacies, lacustrine dolomite reservoir, hydrocarbon exploration, Bohai Bay Basin
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spelling doaj.art-98f175597d514b9ca768cde4d5d2ddde2022-12-21T20:30:11ZengKeAi Communications Co., Ltd.Petroleum Exploration and Development1876-38042011-04-01382136144Lacustrine carbonates in the southwest margin of the Qikou Sag, Huanghua Depression, Bohai Bay BasinXiugang Pu0Lihong Zhou1Dunqing Xiao2Shuangjun Hua3Changwei Chen4Xuanjun Yuan5Guomeng Han6Wei Zhang7PetroChina Dagang Oilfield Company, Tianjin 300280, China; Corresponding authorPetroChina Dagang Oilfield Company, Tianjin 300280, ChinaPetroChina Dagang Oilfield Company, Tianjin 300280, ChinaPetroChina Dagang Oilfield Company, Tianjin 300280, ChinaPetroChina Dagang Oilfield Company, Tianjin 300280, ChinaPetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, ChinaPetroChina Dagang Oilfield Company, Tianjin 300280, ChinaPetroChina Dagang Oilfield Company, Tianjin 300280, ChinaThe southwest margin of the Qikou Sag is a flexural gentle slope formed by the deformation of a drape structure due to its underlying basement lifting. The sedimentary period of the Lower Member 1 of Shahejie Formation is the maximum extensional time of the Paleogene lacustrine basin. Debris from source areas is in shortage. In the broad littoral shallow lake, hundreds of square kilometers of lacustrine carbonates are deposited and distributed stably. The main lithologies of the sediments are biolithite and dolomite (micritic dolomite and dolomitic limestone), and the dolomites are mainly middle late buried dolomite and penecontemporaneous dolomite. Their distribution area is more than 1 650 m2, the cumulative thickness is between 5 and 25 meters, and the average thickness is about 10 meters. Intercrystal pores, intergranular pores, corrosion pores and frequent fissures are developed in the medium porosity and low permeability dolomite reservoirs. The dolomites alternate with oil shale and dark mudstone, favorable for the charge of low mature hydrocarbons and the formation of large scale accumulations. Drilling exploration practices show that the lacustrine dolomite reservoirs are characterized by medium burial depth and regional petroleum accumulation and are a new exploration area for Paleogene oil and gas. Key words: Qikou Sag, Shahejie Formation Lower Member 1, lacustrine carbonates, lithofacies, lacustrine dolomite reservoir, hydrocarbon exploration, Bohai Bay Basinhttp://www.sciencedirect.com/science/article/pii/S1876380411600220
spellingShingle Xiugang Pu
Lihong Zhou
Dunqing Xiao
Shuangjun Hua
Changwei Chen
Xuanjun Yuan
Guomeng Han
Wei Zhang
Lacustrine carbonates in the southwest margin of the Qikou Sag, Huanghua Depression, Bohai Bay Basin
Petroleum Exploration and Development
title Lacustrine carbonates in the southwest margin of the Qikou Sag, Huanghua Depression, Bohai Bay Basin
title_full Lacustrine carbonates in the southwest margin of the Qikou Sag, Huanghua Depression, Bohai Bay Basin
title_fullStr Lacustrine carbonates in the southwest margin of the Qikou Sag, Huanghua Depression, Bohai Bay Basin
title_full_unstemmed Lacustrine carbonates in the southwest margin of the Qikou Sag, Huanghua Depression, Bohai Bay Basin
title_short Lacustrine carbonates in the southwest margin of the Qikou Sag, Huanghua Depression, Bohai Bay Basin
title_sort lacustrine carbonates in the southwest margin of the qikou sag huanghua depression bohai bay basin
url http://www.sciencedirect.com/science/article/pii/S1876380411600220
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