陈义林, 李壮福, 秦勇. 鄂尔多斯盆地双山地区太原组砂岩次生孔隙形成机制[J]. 煤田地质与勘探, 2011, 39(1): 11-15. DOI: 10.3969/j.issn.1001-1986.2011.01.003
引用本文: 陈义林, 李壮福, 秦勇. 鄂尔多斯盆地双山地区太原组砂岩次生孔隙形成机制[J]. 煤田地质与勘探, 2011, 39(1): 11-15. DOI: 10.3969/j.issn.1001-1986.2011.01.003
CHEN Yilin, LI Zhuangfu, QIN Yong. The mechanism of secondary porosity in Taiyuan sandstone, at Shuangshan region, Ordos basin[J]. COAL GEOLOGY & EXPLORATION, 2011, 39(1): 11-15. DOI: 10.3969/j.issn.1001-1986.2011.01.003
Citation: CHEN Yilin, LI Zhuangfu, QIN Yong. The mechanism of secondary porosity in Taiyuan sandstone, at Shuangshan region, Ordos basin[J]. COAL GEOLOGY & EXPLORATION, 2011, 39(1): 11-15. DOI: 10.3969/j.issn.1001-1986.2011.01.003

鄂尔多斯盆地双山地区太原组砂岩次生孔隙形成机制

The mechanism of secondary porosity in Taiyuan sandstone, at Shuangshan region, Ordos basin

  • 摘要: 鄂尔多斯盆地双山地区太原组砂岩的储集空间存在多种类型的次生孔隙。为指导本区天然气的勘探开发,通过岩心观察和铸体薄片鉴定分析方法,探讨了该区太原组砂岩次生孔隙的形成机制。研究认为,双山地区太原组砂岩次生孔隙的形成机制主要受被溶蚀组分的物质基础、酸碱溶蚀性流体与被溶组分之间的溶解反应、溶蚀后自生矿物的充填以及构造压裂缝4个因素的影响。其中,酸性溶蚀方式及自生矿物的充填对次生孔隙的发育起到主导作用。

     

    Abstract: There are various types of secondary porosity in Taiyuan sandstone at Shuangshan region, Ordos basin.Based on the observation of drilling cores and measurement of identification of casting thin sections under microscope, the paper discusses the mechanism of secondary porosity, so as to guide the exploration of natural gas. The mechanism of secondary porosity in Taiyuan sandstone was discussed from four factors including corroded material foundation. acidic and alkalic fluid dissolution, infilling of authigenic minerals and tectonic fracture, the acidic dissolution and infilling of authigenic minerals play a leading role in the area.

     

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