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彰武罗锅沟丝光沸石矿产于侏罗系上统建昌组上部层位的基性—酸性喷发火山岩系组成的半拉门—后新秋向斜北东翼次级缓倾斜向斜盆地中。沸石矿的生成与酸性火山熔岩及酸性火山碎屑熔岩有关。矿床由7个大小不等的扁豆状或透镜状矿体组成。矿石矿物主要为丝光沸石,其次有斜发沸石;伴生有蒙脱石、玉髓等。矿石的沸石含量一般在60%以上,蒙脱石含量大多在10%以下。矿石类型为块状、珍珠角砾状和安山角砾状。矿床是在火山活动晚期的热气液作用下形成的。
The Changwuluogou molybdenite mineral is produced in the upper part of the upper Jurassic system of the Jianchang Formation, a basal-acidic eruption volcanic series consisting of a half-sluice-post-New Qiuke syncline in the northeastern subgrade of the gently inclined syncline basin. The formation of zeolites is related to acidic volcanic lava and acidic volcaniclastic lava. The deposit consists of seven lenticular or lenticular ore bodies of varying sizes. Ore minerals are mainly mordenite, followed by clinoptilolite; associated with montmorillonite, chalcedony and so on. Ore ore zeolite content is generally above 60%, montmorillonite content mostly below 10%. Ore types are massive, pearl breccia and Anshan pebbles. The deposit was formed in the late period of volcanic activity by the action of hot gas and liquid.