Classification and origin of tight sandstone reservoirs of the 3rd Member of Xujiahe Formation in central and western Sichuan Basin
JIN Hui1, CUI Junfeng1, YANG Guiru1, YANG Wei1, XIAO Dianshi2, WANG Zhihong1, WANG Min2, WU Xueqiong1, BO Dongmei1
1 PetroChina Research Institute of Petroleum Exploration and Development,Beijing 100083, China; 2 National Key Laboratory of Deep Oil and Gas,China University of Petroleum(East China),Shandong Qingdao 266580,China
Abstract Due to the complex rock composition and strong heterogeneity in pore throat structure of the Upper Triassic Xujiahe Formation in central and western Sichuan Basin,the gas content and productivity show rapid changes. Therefore, it is urgent to clarify the reservoir types,formation mechanisms,and their distribution characterization. Taking the tight sandstone reservoirs of the 3rd Member of the Xujiahe Formation as the object,this study conducts microscopic analysis of pore structure through thin section,physical properties,mercury intrusion,and nuclear magnetic resonance,establishes reservoir classification standards,and then reveals the control of diagenesis and rock composition on the formation of various reservoir types. The results show that there are five types of reservoir spaces developed in the 3rd Member of the Xujiahe Formation,including microcracks,primary intergranular pores,residual intergranular pores,dissolution pores,and intercrystalline pores,among which the development of the intergranular pore throats is the key to reservoir quality. Based on the fractal features,the pore throat system is divided into five intervals,and combined with parameters such as the proportion of meso to macro pore throats and main flow throat radius,four types of tight reservoirs are finely divided. Type Ⅰ reservoirs feature “weak compaction and strong dissolution”,which is related to high percentage of quartz particles,low percentage of mudstone and carbonate rock fragments,and moderate volcanic rock debris; Type Ⅱ reservoirs exhibit “strong compaction and strong dissolution”,with a large amount of impurities,low percentage of mudstone debris,and high percentage of feldspar particles as the material basis for their formation;Both Type Ⅲ and Type Ⅳ reservoirs have strong cementation characteristics,calcite cementation was developed due to the high content of calcareous rock debris in Type Ⅲ reservoirs,while significant reduction of pore size related to the matrix in Type Ⅳ reservoirs. This research can not only guide the study of the formation mechanism of tight reservoirs in the study area,but also provide certain reference for the correlation between the classification and genetic of tight reservoirs.
Fund:Co-funded by the National Natural Science Foundation of China(No. U22B6002),and CNPC Scientific Research and Technology Development Project(No.2021DJ0605)
Corresponding Authors:
CUI Junfeng,born in 1970,graduated from Northeast Petroleum University in 1996. He is now a senior engineer at PetroChina Research Institute of Petroleum Exploration and Development,and is mainly engaged in the research on comprehensive geological evaluation of oil and natural gas. E-mail: yjy_cjf@petroChina.com.cn.
About author: About the first author JIN Hui,born in 1970,graduated from China University of Geosciences(Beijing)in 2011 with her Ph.D. degree. She is now a senior engineer at PetroChina Research Institute of Petroleum Exploration and Development,and is mainly engaged in comprehensive research on natural gas exploration. E-mail: JH69@petroChina.com.cn.
Cite this article:
JIN Hui,CUI Junfeng,YANG Guiru et al. Classification and origin of tight sandstone reservoirs of the 3rd Member of Xujiahe Formation in central and western Sichuan Basin[J]. JOPC, 2024, 26(6): 1452-1466.
JIN Hui,CUI Junfeng,YANG Guiru et al. Classification and origin of tight sandstone reservoirs of the 3rd Member of Xujiahe Formation in central and western Sichuan Basin[J]. JOPC, 2024, 26(6): 1452-1466.
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