河南安棚碱矿为一蒸发成因的始新世重碳钠盐矿床。自生方沸石和钠沸石广泛发育在含碱段地层中，越靠近碱层沸石含量越高。两种沸石矿物分别以不同的产状分布于不同的岩石中。沸石与火山物质没有直接的联系。沸石的产状特征表明：化学沉积和胶体转变是方沸石最可能的成因，主要为准同生和成岩早期的产物。钠沸石主要为成岩阶段后期或成岩期后的产物。安棚磁矿的佛石矿物组合简单，产状复杂，反映了其独特的形成条件和环境。 Henan Anpeng alkali deposit is an evaporite Eocene heavy carbon sodium salt deposit. Born zeolite and sodium zeolite widely developed in the alkali-bearing strata, the closer to the alkali layer the higher the content of zeolite. The two zeolites are distributed in different rocks in different forms. There is no direct relationship between zeolites and volcanic material. The characteristic features of zeolite show that chemical deposition and colloidal transition are the most likely genesis of analcime, which are mainly the products of quasi-syngenetic and early diagenesis. Sodium zeolite is mainly the product of late diagenetic stage or diagenetic stage. Anpeng Magong fossil minerals combination is simple, complex shape, reflecting its unique formation conditions and the environment.