热液沸石化常见于许多中、基性火山活动地区。在现代热液矿床中,沸石往往占到新生矿物体积的50％。沸石形成在没有明显金属矿化的热液作用的低温阶段,多半是最后阶段。因此,В.П.罗果娃关于浊沸石化作为一种新的近矿蚀变类型和铀呈矿现象的普查标志的报道是很有意义的。根据她的资料,浊沸石化晕发育在中生代的花岗岩类和其上覆的沉积岩(细砾岩和砂岩)中。 Hydrothermal zeolite is common in many, basic volcanic activity areas. In modern hydrothermal deposits, zeolites often account for up to 50% of the volume of nascent minerals. Zeolite formation in the absence of significant metal mineralization hydrothermal role in the low-temperature stage, mostly in the final stage. Therefore, it is of interest that В.П. 罗娃娃 on the report of lazolinization as a census mark of a new near-ores alteration type and uranium mineralization phenomenon. According to her sources, lazeite fusilis develops in Mesozoic granitoids and their overlying sedimentary rocks (fine conglomerates and sandstone).