--> Sandstone Diagenesis of the Second Member of Xu Jiahe Formation in Yuanba Area, Northeast Sichuan Basin, China
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Previous HitSandstoneNext Hit Previous HitDiagenesisNext Hit of the Second Member of Xu Jiahe Formation in Yuanba Area, Northeast Sichuan Basin, China

Abstract

The second member of Xu Jiahe Formation (T3x2) of Upper Triassic, in Yuanba area, Northeast Sichuan Basin, is tight Previous HitsandstoneNext Hit gas interval. The Previous HitsandstoneNext Hit, distributed in the whole research area with an average thickness of 250 meters, is dominated by braided stream delta front. Much oil and gas have been extracted, indicating great resource, however why the Previous HitsandstoneNext Hit is so tight still remain unclear. This study is focused on Previous HitsandstoneNext Hit Previous HitdiagenesisNext Hit of T3x2 and discussions on the effects on poroperm characteristics. Fourty-five sample from eight wells are analyzed via petrographic study including core observation, optical microscopy, SEM technology, electron microprobe analysis, X-ray diffraction. The results are summarized to four points:(1)The lithology of T3x2 is dominated by fine to medium-grained lithic Previous HitsandstoneNext Hit and the porosity and permeability values range from 0.48 to 15.6%, 0.01mD to 8.3mD, with an average 3.6%, 0.38mD, respectively;(2)Six types of pores, including intergranular pore, intragranular dissolved pore, moldic pore, intercrystal micropore, grain-edge fractures, structure fractures, are identified; (3)Studies have showed that the Previous HitsandstoneNext Hit exist five types of Previous HitdiagenesisNext Hit, including compaction, cementation, metasomatism, dissolution and fracturing and each one has a significant Previous HitinfluenceNext Hit on the evolution of the pore in the Previous HitsandstoneNext Hit;(4)The effect of the main Previous HitdiagenesisNext Hit on reservoir quality is as follows: the initial porosity was rapidly decreased (from 35% to 10%) by compaction and cementation and then increased by selective dissolution of unstable grains and cement. Denudation, including acidic denudation and alkalic denudation, lead to increased porosity by 3%. The Previous HitinfluenceTop of metasomatism on reservoir physical property is not obvious. Fracturing or fault that connects the favorable source bed is another major factor especially the conductive facture. It can be inferred that reservoir quality of T3x2 is mainly damaged by the process of compaction and cementation, and improves slightly by denudation.