1) epidiagenesis
表生成岩作用
2) epigenesis and burial diagenesis
表生和埋藏成岩作用
3) Epigenic karstification
表生岩溶作用
1.
Epigenic karstification(EK) and burial dissolution(BD) that are the most important diagenesis in carbonate rocks are similar in undergoing effect of the inner factors such as petrology and composition but great different in effect of the outer controlling factors.
塔里木盆地塔北地区主要发育表生岩溶作用;塔中地区西北部不具备发育大规模表生岩溶的地质条件,以发育埋藏溶蚀作用为主。
4) secondary diagenesis
次生成岩作用
5) later diagenesis
成岩后生作用
1.
Formation of volcanic rock reservoirs is divided into 2 stages,the initial diagenesis stage and the later diagenesis stage.
将火山岩储层形成划分为2个阶段:初始成岩作用阶段和成岩后生作用阶段。
6) supergenic metallogenesis
表生成矿作用
补充资料：表生成岩作用
见成岩作用。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条