Diagenesis and porosity-permeability evolution of low permeability reservoirs: A case study of Jurassic Sangonghe Formation in Block 1, central Junggar Basin, NW China
Based on core observation, thin section examination, cathode luminescence analysis, scanning electron microscopy, fluid inclusions, carbon and oxygen isotope, mercury penetration, porosity-permeability test and other analytical methods, combined with the histories of burial evolution, organic matter...
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KeAi Communications Co., Ltd.
2015-08-01
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doaj-3735ee9cbd894c98a7483b93c1805ac22021-02-02T04:47:07ZengKeAi Communications Co., Ltd.Petroleum Exploration and Development1876-38042015-08-01424475485Diagenesis and porosity-permeability evolution of low permeability reservoirs: A case study of Jurassic Sangonghe Formation in Block 1, central Junggar Basin, NW ChinaKelai XI0Yingchang CAO1Yanzhong WANG2Beyene Girma HAILE3Xiangxiang ZHANG4Jianghua ZHANG5Jiehua JIN6School of Geosciences, China University of Petroleum, Qingdao 266580, China; Department of Geosciences, University of Oslo, Oslo 0316, NorwaySchool of Geosciences, China University of Petroleum, Qingdao 266580, China; Corresponding authorSchool of Geosciences, China University of Petroleum, Qingdao 266580, ChinaDepartment of Geosciences, University of Oslo, Oslo 0316, NorwayPetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, ChinaXinchun Oil Production Plant of Shengli Oilfield, Sinopec, Dongying 257015, ChinaSchool of Geosciences, China University of Petroleum, Qingdao 266580, ChinaBased on core observation, thin section examination, cathode luminescence analysis, scanning electron microscopy, fluid inclusions, carbon and oxygen isotope, mercury penetration, porosity-permeability test and other analytical methods, combined with the histories of burial evolution, organic matter thermal evolution and hydrocarbon charge, the diagenesis and porosity-permeability evolution are studied of low-permeability reservoirs of Jurassic Sangonghe Formation in Block 1 of central Junggar Basin. The matching relation between reservoir porosity-permeability evolution and hydrocarbon accumulation history is analyzed. The diagenetic environment evolution of the reservoir in the study area is early alkaline, interim acid and late alkaline, forming the diagenetic sequence of chlorite membrane precipitation, early calcite cementation, feldspar dissolution accompanied by quartz overgrowth and authigenic kaolinite precipitation, anhydrite cementation, late period ferrocalcite and ankerite cementation, a small amount of pyrite cementation. Generally, compaction occurs throughout the whole burial process. According to the matching relation between reservoir porosity-permeability evolution and hydrocarbon accumulation history, the Jurassic Sangonghe Formation has three genetic types of low permeability reservoirs: densification after hydrocarbon accumulation, with the best exploration potential; densification during the hydrocarbon accumulation, with medium exploration potential; densification before the hydrocarbon accumulation, with the poorest exploration potential. Key words: low permeability reservoir, diagenesis, porosity-permeability evolution, hydrocarbon accumulation history, Junggar Basinhttp://www.sciencedirect.com/science/article/pii/S1876380415300409 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Kelai XI Yingchang CAO Yanzhong WANG Beyene Girma HAILE Xiangxiang ZHANG Jianghua ZHANG Jiehua JIN |
spellingShingle |
Kelai XI Yingchang CAO Yanzhong WANG Beyene Girma HAILE Xiangxiang ZHANG Jianghua ZHANG Jiehua JIN Diagenesis and porosity-permeability evolution of low permeability reservoirs: A case study of Jurassic Sangonghe Formation in Block 1, central Junggar Basin, NW China Petroleum Exploration and Development |
author_facet |
Kelai XI Yingchang CAO Yanzhong WANG Beyene Girma HAILE Xiangxiang ZHANG Jianghua ZHANG Jiehua JIN |
author_sort |
Kelai XI |
title |
Diagenesis and porosity-permeability evolution of low permeability reservoirs: A case study of Jurassic Sangonghe Formation in Block 1, central Junggar Basin, NW China |
title_short |
Diagenesis and porosity-permeability evolution of low permeability reservoirs: A case study of Jurassic Sangonghe Formation in Block 1, central Junggar Basin, NW China |
title_full |
Diagenesis and porosity-permeability evolution of low permeability reservoirs: A case study of Jurassic Sangonghe Formation in Block 1, central Junggar Basin, NW China |
title_fullStr |
Diagenesis and porosity-permeability evolution of low permeability reservoirs: A case study of Jurassic Sangonghe Formation in Block 1, central Junggar Basin, NW China |
title_full_unstemmed |
Diagenesis and porosity-permeability evolution of low permeability reservoirs: A case study of Jurassic Sangonghe Formation in Block 1, central Junggar Basin, NW China |
title_sort |
diagenesis and porosity-permeability evolution of low permeability reservoirs: a case study of jurassic sangonghe formation in block 1, central junggar basin, nw china |
publisher |
KeAi Communications Co., Ltd. |
series |
Petroleum Exploration and Development |
issn |
1876-3804 |
publishDate |
2015-08-01 |
description |
Based on core observation, thin section examination, cathode luminescence analysis, scanning electron microscopy, fluid inclusions, carbon and oxygen isotope, mercury penetration, porosity-permeability test and other analytical methods, combined with the histories of burial evolution, organic matter thermal evolution and hydrocarbon charge, the diagenesis and porosity-permeability evolution are studied of low-permeability reservoirs of Jurassic Sangonghe Formation in Block 1 of central Junggar Basin. The matching relation between reservoir porosity-permeability evolution and hydrocarbon accumulation history is analyzed. The diagenetic environment evolution of the reservoir in the study area is early alkaline, interim acid and late alkaline, forming the diagenetic sequence of chlorite membrane precipitation, early calcite cementation, feldspar dissolution accompanied by quartz overgrowth and authigenic kaolinite precipitation, anhydrite cementation, late period ferrocalcite and ankerite cementation, a small amount of pyrite cementation. Generally, compaction occurs throughout the whole burial process. According to the matching relation between reservoir porosity-permeability evolution and hydrocarbon accumulation history, the Jurassic Sangonghe Formation has three genetic types of low permeability reservoirs: densification after hydrocarbon accumulation, with the best exploration potential; densification during the hydrocarbon accumulation, with medium exploration potential; densification before the hydrocarbon accumulation, with the poorest exploration potential. Key words: low permeability reservoir, diagenesis, porosity-permeability evolution, hydrocarbon accumulation history, Junggar Basin |
url |
http://www.sciencedirect.com/science/article/pii/S1876380415300409 |
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