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Evaluation of Chang 2 reservoir in Zichang Area, Ordos Basin

Journal of Geoscience and Environment Protection 2024年第4期12卷 1-11页

作者： Zhiwei Du Zhaoyong Ping Feng Chen School of Earth Science and Engineering Xi&#8217an Shiyou University Xi&#8217an China Key Laboratory of Hydrocarbon Accumulation of Shaanxi Province Xi’an Shiyou University Xi’an China

In this paper, the Chang 2 reservoir in Zichang Area of Ordos Basin, the second largest sedimentary basin in China, is classified and evaluated by using logging and core data, thin section identification and electron microscopy. The main sedimentary microfacies of Chang 213 is braided river delta sedimentary system in geological history, and there are three main sedimentary microfacies types: swamp microfacies, distributary channel microfacies and natural embankment microfacies on land. The heterogeneity in the study area is as follows: Chang 212 formation has the strongest heterogeneity, followed by Chang 211 formation with strong heterogeneity, and finally Chang 213 formation with medium heterogeneity. The reservoirs of Chang 2 member in the study area are dominated by IIIa, IIb and IIIb, and the reservoirs are mainly composed of ultra-low porosity and low permeability reservoirs and low porosity and low permeability reservoirs.

关键词： Zichang Area Sedimentary Microfacies reservoir assessment Ordos Basin

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reservoir Characteristics and Controlling Factors of Silurian Lower Kepingtage Formation in Tahe Area, Tarim Basin, NW China

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Journal of Earth Science 2017年第6期28卷 1135-1144页

作者： Ruohan Liu Zaixing Jiang Ming Wang Weili Yang Jingxiang Guo Minghao Wu Yi Gao Shanyazi Wei Zhihong Nie Hong He School of Energy Resources China University of Geosciences Beijing 100083 China Institute of Earth Sciences China University of Geosciences Beijing 100083 China Exploration and Production Research Institute SINOPEC Beijing 100083 China Geophysical-China Oilfield Services Limited Tianjin 300451 China PetroChina Coalbed Methane Company Limited Beijing 100028 China

With the breakthrough of exploration in Well TP16-1, the lower Kepingtage Formation becomes a key target for petroleum exploration of deep clastic reservoir in Tahe area. In this paper we focused on the research of the reservoir characteristics and its controlling factors in two sub-member formations（S1k11 and S1k13）. Based on X-ray diffraction, conventional physical properties data（porosity and permeability） and reservoir storage space data（casting thin section and scanning electron microscope）, we determined that the S1k1 Formation belongs to extra-low porosity and permeability reservoir, although the upper S1k13 Formation shows relative better physical characteristic than the lower S1k11 Formation. The development of storage space in the study area is controlled by sedimentary microfacies, diagenesis process. reservoirs in S1k1 Formation are mainly located in channel（S1k11 sandstones） and sand flat（S1k13 sandstones）. The sand flat sediments with a more coarse grain size compared with the channel. In diagenesis, compaction is the major controlling factor for reducing the porosity, followed by cementation. Dissolution of diagenesis is the major controlling factor in enhancing the reservoir porosities. Compared with channel（S1k11） sandstones, sand flat sandstones（S1k13） have better reservoir quality for its weaker compaction, cementation and stronger dissolution. On the basis of sedimentary characteristics（grain size and subfacies）, physical property（porosity and permeability） and reservoir storage space, we divide the S1k1 reservoir into three categories（I, II and III）. Type I reservoir is high quality reservoir. It is mainly distributed in the south area of S1k11 and S1k13 reservoir. Type II is moderate reservoir. It is located in the middle of S1k11 reservoir and in the north of S1k13 reservoir. Type III is the poor reservoir. It is only located in the north of S1k11 reservoir.

关键词： reservoir characteristics controlling factors reservoir assessment lower Kepingtage Formation Tahe area Tarim Basin

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