Characteristics and Main Controlling Factors of Chang-6 Reservoir of Triassic Yanchang Formation in Dalugou Area,Ordos Basin
Haikun Ji
Abstract
Haikun Ji
Abstract
Based on outcrop observation,core description,geophysical logging interpration and other test datum,the petrologic characteristic,pore structure and the physical properties of Chang-6 reservoir of Yanchang formation in the Dalugou exploration area are studied.The result shows that: the Chang-6 reservoir of Yanchang formation in this area is feldspar sandstone with low porosity and permeability;the sandstones can be compositionally classified as immature and high structural maturity;the pores of the reservoir are mostly intergranular pores,intraparticle dissolution pores and moldic pores or relic moldic pores;the characteristics of the pore structure are minor pores and microcrystals;the reservoir is formed by interaction among original terrestrial composition,sedimentary facies and diagenesis;the structure and amount of original terrestrial composition are direct factors leading to good physical property;sedimentary facies is the basic factor that controls the final distribution and space characteristics of reservoir;submerged distributary channels in delta fronts are the favorable sedimentary environment for the formation and development of reservoir;diagenesis plays!cardinal role in the quality of reservoir,compaction and cementation mainly led to the tight reservoir and poor physical property, while dissolution makes the reservoir become good.
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Based on outcrop observation,core description,geophysical logging interpration and other test datum,the petrologic characteristic,pore structure and the physical properties of Chang-6 reservoir of Yanchang formation in the Dalugou exploration area are studied.The result shows that: the Chang-6 reservoir of Yanchang formation in this area is feldspar sandstone with low porosity and permeability;the sandstones can be compositionally classified as immature and high structural maturity;the pores of the reservoir are mostly intergranular pores,intraparticle dissolution pores and moldic pores or relic moldic pores;the characteristics of the pore structure are minor pores and microcrystals;the reservoir is formed by interaction among original terrestrial composition,sedimentary facies and diagenesis;the structure and amount of original terrestrial composition are direct factors leading to good physical property;sedimentary facies is the basic factor that controls the final distribution and space characteristics of reservoir;submerged distributary channels in delta fronts are the favorable sedimentary environment for the formation and development of reservoir;diagenesis plays!cardinal role in the quality of reservoir,compaction and cementation mainly led to the tight reservoir and poor physical property, while dissolution makes the reservoir become good.
Key concepts: Geology, Diagenesis, Facies, Sedimentary rock, Feldspar, Compaction, Cementation (geology), Petrology