收稿日期: 2012-02-03
修回日期: 2012-06-15
网络出版日期: 2012-12-10
基金资助
四川省重点学科建设项目“矿产普查与勘探”(编号:SZD0414)资助.
Weathering Crust Karstification in Leikoupo Formation in Central Sichuan Area
Received date: 2012-02-03
Revised date: 2012-06-15
Online published: 2012-12-10
宋文燕,刘利清,甘学启,秦启荣,苏培东,范存辉 . 川中地区雷口坡组风化壳岩溶作用研究[J]. 天然气地球科学, 2012 , 23(6) : 1019 -1024 . DOI: 10.11764/j.issn.1672-1926.2012.06.1019
Through the investigation of 8 preferred geological sections, the lithology, corrosion holes and fractures growth conditions, growth layer and thickness of the weathering crust in the top of Leikoup Formation have been determined.The stratum analysis suggests that the lithology of the Leikoupo outcrop are mainly dolomite, dissolution collapse breccia and limestone.The corrosion holes are developed, and dominated by half-filling or no filling.In the range of the karstification depth, about 65m, karstification improved lithology, pore space, storage and permeability.It forms a good reservoir of ancient weathering crust.The research provides an important reference for the study of deep underground weathering crust reservoir and can provide a basis for the geological exploration and development of Sichuan Leikoupo weathering crust reservoir.
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