--> ABSTRACT: Diagenetic Reservoir Facies and Diagenetic Evolutionary Sequences of Extra-Low Permeability Reservoir in the Upper Triassic Xujiahe Formation of Fenggu Structure, Western Sichuan Depression, China, by Lin, Yu; Xu, Zhangyou; Wu, Shenghe; #90142 (2012)
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Diagenetic Previous HitReservoirNext Hit Facies and Diagenetic Evolutionary Sequences of Extra-Low Permeability Previous HitReservoirNext Hit in the Upper Triassic Xujiahe Formation of Fenggu Structure, Western Sichuan Depression, China

Lin, Yu *1; Xu, Zhangyou 1; Wu, Shenghe 1
(1) China University of Petroleum-Beijing, Beijing, China.

Abstract: Diagenetic Previous HitreservoirNext Hit facies are the integration of some diagenesis and special Previous HitreservoirNext Hit spaces to describe Previous HitreservoirNext Hit properties. It is critical for Previous HitpredictingNext Hit the distribution of high-quality Previous HitreservoirNext Hit to analyze the evolutionary processes and sequences of different diagenetic Previous HitreservoirNext Hit facies and to explore Previous HitreservoirNext Hit forming mechanism. This study focuses on Previous HitreservoirNext Hit in the Upper Triassic Xujiahe Formation in Fenggu Structure of Western Sichuan Depression. They are buried deeply and classified as low Previous HitporosityNext Hit and extra-low permeability Previous HitreservoirNext Hit. After divided diagenesis stages, researched the diagenetic Previous HitreservoirNext Hit facies types and diagenetic evolutionary sequences based on the analysis of petrologic characteristic, sedimentary facies, diagenetic types, apparent compacting rate, apparent cementing rate, combination of Previous HitreservoirNext Hit spaces, Previous HitporosityNext Hit, permeability and some other parameters. The diagenetic Previous HitreservoirNext Hit facies are divided into 4 types, namely as, 1st, the residual intergranular pores-dissolved pores diagenetic Previous HitreservoirNext Hit facies with weak compaction and strong dissolution, 2nd, the dissolved pores diagenetic Previous HitreservoirNext Hit facies with compaction and dissolution, 3rd, the dissolved pores- microporosity diagenetic Previous HitreservoirNext Hit facies with middle to strong compaction and weak dissolution and 4th, the tight diagenetic Previous HitreservoirNext Hit facies with strong dissolution. The development of the relic primary intergranular pores and secondary dissolution pores is mainly controlled by the rock components, compaction of pores, the filling of authigenic minerals and the multi-stages dissolution and the injection of acid fluid. The effective diagenetic Previous HitreservoirNext Hit facies of the 4 types are respectively the residual intergranular pores-dissolved pores diagenetic Previous HitreservoirNext Hit facies with weak compaction and strong dissolution and the dissolved pores diagenetic Previous HitreservoirNext Hit facies with compaction and dissolution. They play an important role in the formation of the high-quality Previous HitreservoirTop of Xujiahe Formation.

 

AAPG Search and Discovery Article #90142 © 2012 AAPG Annual Convention and Exhibition, April 22-25, 2012, Long Beach, California