浊沸石相
- 网络laumontite facies
浊沸石相-
优质储层常出现在弱压实绿泥石薄膜胶结相和浊沸石长石溶蚀相的发育区，而其余四种成岩相发育区则物性差，常成为成岩致密带。
While rest four diagenesis facies developing zones have weak properties of matter and always turned into diagenetic tight zones .
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将研究区成岩相划分为五个相带类型：砂岩压实压溶相、砂岩弱压实绿泥石胶结相、砂岩绿泥石胶结长石溶蚀相、砂岩碳酸盐胶结相、浊沸石胶结溶蚀相长石溶蚀相。
ⅲ . The diagenetic facies in study area is divided into five types : compaction and pressure solution sandstone phase , weakly compacted sandstone chlorite cementation facies , chlorite cementation sandstone feldspar dissolution facies , carbonate cementation Sandstone facies , lomontite cementation dissolution facies Feldspar dissolution facies .