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Zhu Xiaodong, Shi Bingwen, Zhu Dakui. A New Sediment Grain Size Index Designed for Sedimentological Study of Microfossils—— With Demonstrations of Foraminifera in Jiangsu Coast, China[J]. Acta Sedimentologica Sinica, 1997, 15(3): 145-149.
Citation: Shi Ji'an, Jin Huijuan, Xue Lianhua. Annnalysis on Mechanism of Feldspar Dissolution and Its Influencing Factors in Feldspar-rich Sandstone Reservoir[J]. Acta Sedimentologica Sinica, 1994, 12(3): 67-75.

Annnalysis on Mechanism of Feldspar Dissolution and Its Influencing Factors in Feldspar-rich Sandstone Reservoir

  • Publish Date: 1994-09-10
  • Porosity formed by the dissolution of unstable framework grains is one of the most important genetic types of secondary porosity,and feldspar is found to be the most extensive ones of the unstable framework grains. Songliao and Liaohe basins are two large petroliferous inland basins of Mesozoic and Cenozoic,in which has been constructed a clastic rock formation with great thickness.In sandstone there is above 20% unstable feldspar fragments,which is the requisite condition for the development of the secondary porosity. But it has been studied that the FGD of the grains, may not cause the increase of the reservoir permeability of the sandstone(Siebert,1984). The dissolution of a unit volume of feldspar may produce 0. 66 volume of Kaolinite and 0. 33 volume of quartz (Sullivan,1991).Therefore.only when the dissolved materials are transferred after dissolution the porosity of the sandstone can be effectively increased. This paper is based on analyzing the state of thermodynamics of feldspar dissolution process.The SEM,X一diffraction,oxygen and carbon stable isotopes, etc. analytical methods are adopted in research of the controlling factors of feldspar dissolution in Cretaceous sandstone in the region of Songliao basin and Palaeogene sandstone in the Liaohe basin. Through research,the author indicates that favors to development degree of feldspar dissolution are dependent on:(1)the organic and inorganic reaction time;(2)the characteristics and fluid condition of pore water;(3)the primary porosity of sandstone,and(4)the temperature and pressure,etc. These factors play different roles in different types of feldspar. The most important parameters are fluid condition,type and abundance of organic acid in fluid .which were closely related with the evolution of clay mineral and organic material in the diagenesis of mudstone.
  • [1] 周书欣,卓胜广,1991,松辽盆地北部中一深层砂岩的次生孔隙研究,地质科学,(1):48~59,
    [2] 郑浚茂,庞明编著,1989,碎屑储集岩的成岩作用研究,中国地质大学出版社。
    [3] Stoessell, R. K.,and E. D. Pittman,1990,Secondary porosity revited;the chemistry of feldspar dissolution by carboxylic acids and anions;AAPG Bulletin.75. 1795~1805.
    [4] Sullivan,K. B.,and Earle F. McBride, 1991,Diagenesis of sandstones at shale contacts and diagenetic heterogeneity, Frio formation, Texas : AAPG Bulletin, 75, 121~138.
    [5] Surdam, R. C., L. J. Crssey, E. S. Hagen, and H. P. Heasler, 1989, organic一inorganic interactions and sandstone diagenesis;AAPG Bulletin.73.3~16.
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  • Published:  1994-09-10

Annnalysis on Mechanism of Feldspar Dissolution and Its Influencing Factors in Feldspar-rich Sandstone Reservoir

Abstract: Porosity formed by the dissolution of unstable framework grains is one of the most important genetic types of secondary porosity,and feldspar is found to be the most extensive ones of the unstable framework grains. Songliao and Liaohe basins are two large petroliferous inland basins of Mesozoic and Cenozoic,in which has been constructed a clastic rock formation with great thickness.In sandstone there is above 20% unstable feldspar fragments,which is the requisite condition for the development of the secondary porosity. But it has been studied that the FGD of the grains, may not cause the increase of the reservoir permeability of the sandstone(Siebert,1984). The dissolution of a unit volume of feldspar may produce 0. 66 volume of Kaolinite and 0. 33 volume of quartz (Sullivan,1991).Therefore.only when the dissolved materials are transferred after dissolution the porosity of the sandstone can be effectively increased. This paper is based on analyzing the state of thermodynamics of feldspar dissolution process.The SEM,X一diffraction,oxygen and carbon stable isotopes, etc. analytical methods are adopted in research of the controlling factors of feldspar dissolution in Cretaceous sandstone in the region of Songliao basin and Palaeogene sandstone in the Liaohe basin. Through research,the author indicates that favors to development degree of feldspar dissolution are dependent on:(1)the organic and inorganic reaction time;(2)the characteristics and fluid condition of pore water;(3)the primary porosity of sandstone,and(4)the temperature and pressure,etc. These factors play different roles in different types of feldspar. The most important parameters are fluid condition,type and abundance of organic acid in fluid .which were closely related with the evolution of clay mineral and organic material in the diagenesis of mudstone.

Zhu Xiaodong, Shi Bingwen, Zhu Dakui. A New Sediment Grain Size Index Designed for Sedimentological Study of Microfossils—— With Demonstrations of Foraminifera in Jiangsu Coast, China[J]. Acta Sedimentologica Sinica, 1997, 15(3): 145-149.
Citation: Shi Ji'an, Jin Huijuan, Xue Lianhua. Annnalysis on Mechanism of Feldspar Dissolution and Its Influencing Factors in Feldspar-rich Sandstone Reservoir[J]. Acta Sedimentologica Sinica, 1994, 12(3): 67-75.
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