The laumontite occurs in the gabbroporphyrite bodies intruding concordantly strata of Chengzihe Formation of Jixi Basin.
浊沸石产于鸡西盆地城子河组顺层侵入的辉长玢岩体中,呈放射状集合体并富集成条带,用X射线衍射、红外吸收光谱、电子探针3种方法对样品进行分析测定。
