Features, origin and distribution of microbial dolomite reservoirs: A case study of 4th Member of Sinian Dengying Formation in Sichuan Basin, SW China
Based on the drilling cores and slice observations, single well data and geochemical analysis, this paper analyzed features, origin and distribution of the 4th Member reservoirs of Sinian Dengying Formation (Z2dn4) in the Sichuan Basin. It is demonstrated that the main reservoir is a set of microbia...
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| Published in | Petroleum exploration and development Vol. 44; no. 5; pp. 745 - 757 |
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| Main Authors | , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier B.V
01.10.2017
KeAi Communications Co., Ltd |
| Subjects | |
| Online Access | Get full text |
| ISSN | 1876-3804 1876-3804 |
| DOI | 10.1016/S1876-3804(17)30085-X |
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| Abstract | Based on the drilling cores and slice observations, single well data and geochemical analysis, this paper analyzed features, origin and distribution of the 4th Member reservoirs of Sinian Dengying Formation (Z2dn4) in the Sichuan Basin. It is demonstrated that the main reservoir is a set of microbial dolomites. The discovery of spherical dolomite has revealed that the dolomitization was related to the microbial action, belonging to the early protodolomite of low-temperature precipitation; the primary matrix pores and the penecontemporaneous eroded pores constituted the subject of the reservoir space, which was not due to the interlayer karst process related to the Tongwan Movement and burial-hydrothermal dissolutional process. The microbial mound-shoal complex and penecontemporaneous dissolution mainly control the development and distribution of the scaled reservoirs in Z2dn4. The microbial dolomite reservoir surrounding the intracratonic rift had a large thickness, good continuity and high quality, and was an important target of the survey. |
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| AbstractList | Based on the drilling cores and slice observations, single well data and geochemical analysis, this paper analyzed features, origin and distribution of the 4th Member reservoirs of Sinian Dengying Formation (Z2dn4) in the Sichuan Basin. It is demonstrated that the main reservoir is a set of microbial dolomites. The discovery of spherical dolomite has revealed that the dolomitization was related to the microbial action, belonging to the early protodolomite of low-temperature precipitation; the primary matrix pores and the penecontemporaneous eroded pores constituted the subject of the reservoir space, which was not due to the interlayer karst process related to the Tongwan Movement and burial-hydrothermal dissolutional process. The microbial mound-shoal complex and penecontemporaneous dissolution mainly control the development and distribution of the scaled reservoirs in Z2dn4. The microbial dolomite reservoir surrounding the intracratonic rift had a large thickness, good continuity and high quality, and was an important target of the survey. Based on the drilling cores and slice observations, single well data and geochemical analysis, this paper analyzed features, origin and distribution of the 4th Member reservoirs of Sinian Dengying Formation (Z2dn4) in the Sichuan Basin. It is demonstrated that the main reservoir is a set of microbial dolomites. The discovery of spherical dolomite has revealed that the dolomitization was related to the microbial action, belonging to the early protodolomite of low-temperature precipitation; the primary matrix pores and the penecontemporaneous eroded pores constituted the subject of the reservoir space, which was not due to the interlayer karst process related to the Tongwan Movement and burial-hydrothermal dissolutional process. The microbial mound-shoal complex and penecontemporaneous dissolution mainly control the development and distribution of the scaled reservoirs in Z2dn4. The microbial dolomite reservoir surrounding the intracratonic rift had a large thickness, good continuity and high quality, and was an important target of the survey. Key words: Sichuan Basin, Sinian, Dengying Formation, microbial dolomite, mound-shoal complex, spherical dolomite, penecontemporaneous corrosion, intracratonic rift |
| Author | ZHANG, Jie CHEN, Yana SHEN, Anjiang PAN, Liyin WANG, Xiaofang |
| Author_xml | – sequence: 1 givenname: Yana surname: CHEN fullname: CHEN, Yana email: chenyn_hz@petrochina.com.cn organization: Petrochina Hangzhou Research Institute of Geology, Hangzhou 310023, China – sequence: 2 givenname: Anjiang surname: SHEN fullname: SHEN, Anjiang organization: Petrochina Hangzhou Research Institute of Geology, Hangzhou 310023, China – sequence: 3 givenname: Liyin surname: PAN fullname: PAN, Liyin organization: Petrochina Hangzhou Research Institute of Geology, Hangzhou 310023, China – sequence: 4 givenname: Jie surname: ZHANG fullname: ZHANG, Jie organization: Petrochina Hangzhou Research Institute of Geology, Hangzhou 310023, China – sequence: 5 givenname: Xiaofang surname: WANG fullname: WANG, Xiaofang organization: Petrochina Hangzhou Research Institute of Geology, Hangzhou 310023, China |
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| Cites_doi | 10.1306/05220605164 10.1016/S1876-3804(14)60034-3 10.1007/s11430-015-5442-1 10.2307/3514674 10.2307/3515160 10.1130/G25013A.1 10.1016/S1876-3804(15)60003-9 10.1306/122001720559 10.1016/j.palaeo.2007.02.028 10.1046/j.1365-3091.2000.00003.x 10.1038/377220a0 10.1016/S1876-3804(15)30055-0 10.1016/S1876-3804(14)60038-0 |
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| Keywords | Sichuan Basin Sinian spherical dolomite intracratonic rift microbial dolomite Dengying Formation penecontemporaneous corrosion mound-shoal complex |
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| Title | Features, origin and distribution of microbial dolomite reservoirs: A case study of 4th Member of Sinian Dengying Formation in Sichuan Basin, SW China |
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