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专辑
网络首发:1992-03-25,
纸质出版:1992
移动端阅览
本文在岩石学研究的基础上
应用阴极发光、氧碳稳定同位素、微量元素、混合染色的资料
详细地研究了鄂中上石炭统碳酸盐岩的成岩作用、成岩序列和孔隙演化
认为:填积作用、胶结作用、溶蚀作用、白云石化作用、压实、压溶作用
是控制鄂中上石炭统碳酸盐岩储集性能的主要因素
其中
白云石化作用、压溶作用、埋藏溶蚀作用是形成聚集期孔隙(油气运移、聚集时岩石的孔隙)的最为重要的因素。
Based on the study of petrology
using the data of cathodoluminescents
stable iso-topes of oxygen and carbon
trace elements and composite colouring
the diagenesis
diage-netic sequences and pore evolution of Upper Carboniferous carbonates in Central Hubei were studied in detail.The study shows that filling
cementation
solution
dolomitization
compaction and pressure-solution were the principal factors in controlling the reservoir properties of the Upper Carboniferous in Central Hubei
the most important of which were the dolomitization
solution in deep burial environment and pressure-solution in forming the pores of accumulation stage.
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