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浙江上虞梁岙地开石——高岭石矿床,规模大,矿石质量好。产于上侏罗系火山碎屑岩和正常沉积岩内。作者通过野外工作、室内境下鉴定及x光、红外、差热、扫描电镜、化学分析等研究,认为该矿床是一个职阶段多成因的层控矿床,矿床的形成经历了沉积成岩、淋滤和后期改造等作用。这一观点的提出,对于该矿床的我矿勘探具有指导意义,并已在生产中得到验证。
The stone-kaolinite deposit in Shangyuliang, Zhejiang, has a large scale and good ore quality. Produced in the Upper Jurassic volcanic clastic rocks and normal sedimentary rocks. Based on field work, indoor environment identification, and x-ray, infrared, differential thermal, scanning electron microscopy, chemical analysis, and other studies, the author believes that this deposit is a multi-caused layered ore deposit of a professional stage. The deposit has undergone sedimentary diagenesis and leaching. And later transformation and other effects. The proposal of this point of view has guiding significance for the prospecting of our mine and has been verified in production.