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Logging evaluation of high quality Ordovician marine carbonate reservoir on the south slope of Central Uplift Belt, Tarim Basin |
DAI Peng1,2,3, DING Wen-Long1,2,3, CAO Zi-Cheng4, YU Teng-Xiao4, WANG Xin-Yu1,2,3, QIU Hua-Biao4 |
1. School of Energy Resources, China University of Geosciences, Beijing 100083, China;
2. Key Laboratory for Marine Reservoir Evolution and Hydrocarbon Abundance Mechanism, Ministry of Education, China University of Geosciences, Beijing 100083, China;
3. Key Laboratory for Shale Gas Exploitation and Assessment, Ministry of Land and Resources, China University of Geosciences, Beijing 100083, China;
4. Research Institute of Exploration and Development Company, Chinese Sinopec Northwest Oilfield Branch, Urumqi 830011, China |
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Abstract The lithological characteristics of Ordovician strata in the study area can be distinguished by crossplot of porosity logging series.Based on the data and results of conventional logging, FMI logging, core and microscope, the authors found three kinds of reservoirs on the south slope of Central Uplift Belt:fractured reservoir, vugular reservoir and fractured-vugular reservoir, which present different response characteristics.Ordovician carbonate reservoirs on the south slope of Central Uplift Belt in Tarim Basin can be classified into three types:type Ⅲ, consisting of fractured reservoir and vugular reservoir, is most developed in the study area, type Ⅱ, i.e., fractured-vugular reservoir, takes the second place, type Ⅰ, i.e., cave reservoir, is not typically developed.The authors' understanding is helpful to finding high quality Ordovician carbonate reservoir on the south slope of Central Uplift Belt, Tarim Basin.
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Received: 05 August 2015
Published: 10 April 2016
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