论砂岩储层次生孔隙的形成机制

ALKALINE DIAGENETIC SETTING CONTRIBUTES TO THE FORMATION OF SECONDARY PORES IN SANDSTOWE RESERVOIRS

本文提出了碱性成岩环境有助于砂岩储层次生孔隙发育这一全新的观点，并提出了单一成岩环境体系中的“酸—碱链式反应”模型。无疑，这会对储层演化和油气勘探提出新的思考。

In this Paper the author puts forward a whole new theoretical point that alkaline diagenetic setting contributes to the formation of secondary pores in sandstone reservoirs. In addition, an ideal “Acid Alkalinechain reaction” model is set up.