Diagenetic Reactions in Reservoir Strata and Geochemical Properties of Pore Fluid and Its Origin in Songliao Basin  

作　　者：楼章华 韩喜球 蔡希源 

机构地区：[1]DepartmentofEarthSciences,ZhejiangUniversity,Hangzhou310027

出　　处：《Chinese Journal Of Geochemistry》1998年第4期346-355,共10页中国地球化学学报

摘　　要：The reservoirs of the Songliao Basin are Composed of typical unstable sandstones,with high percentages of volcanic fragments and feldspar. In the course of sedimentation andburying, a series of physical and chemical reactions took place between minerals and pete waterand water-rock reactions and ion exchange caused changes in ion assemblage of pore water. Hydration-hydrolysis, dissolution and the albitization of feldspar made many ions free from theirframework and inter into the pore water, and induced the precipitation of a large amount of authigenic minerals such as smectite and chlorite. DUring the diagenesis of sandstone, diageneticreactions involved several stages with increasing depth, and so did the precipitation of authigenic minerals and the transformation of minerals. The migration of ions is related with theprecipitation, transformation and dissolution of authigenic minerals. Thus, to deepen our studyon sandstone diagenesis is an important link for the analysis of ion migration in the evolution ofpore water. The origin and evolution of Pore water could be tracked in terms of the geochemistry of fluid inclusions in authigenic minerals. And the isotopic composition of the authigenicmineral calcite can provide its genetic information.The reservoirs of the Songliao Basin are Composed of typical unstable sandstones,with high percentages of volcanic fragments and feldspar. In the course of sedimentation andburying, a series of physical and chemical reactions took place between minerals and pete waterand water-rock reactions and ion exchange caused changes in ion assemblage of pore water. Hydration-hydrolysis, dissolution and the albitization of feldspar made many ions free from theirframework and inter into the pore water, and induced the precipitation of a large amount of authigenic minerals such as smectite and chlorite. DUring the diagenesis of sandstone, diageneticreactions involved several stages with increasing depth, and so did the precipitation of authigenic minerals and the transformation of minerals. The migration of ions is related with theprecipitation, transformation and dissolution of authigenic minerals. Thus, to deepen our studyon sandstone diagenesis is an important link for the analysis of ion migration in the evolution ofpore water. The origin and evolution of Pore water could be tracked in terms of the geochemistry of fluid inclusions in authigenic minerals. And the isotopic composition of the authigenicmineral calcite can provide its genetic information.

关 键 词：同位素 方解石 成岩作用 水库 孔隙水 地球化学 地层 松辽盆地 

分 类 号：P588.2[天文地球—岩石学] P59[天文地球—地质学]