论文部分内容阅读
叶蜡石,又称青田石,寿山石,是以叶蜡石为主要组分,伴生有高岭石、地开石、绢云母和石英等矿物组成的。矿石一般为黄、黄绿和白色,具蜡状光泽隐晶质块状集合体。矿石主要作耐火材料、陶瓷、玻璃工业原料以及橡胶、塑料、造纸工业填料,农业上用作杀虫剂载体,质优的矿石可用作化装品填料,优质块状矿石是传统的雕刻石。由于以往所发现的叶蜡石矿床,大多数产于火山岩分布地区,因此,多数研究者认为,叶蜡石矿床的成因与火山作用和侵入作用有关,并冠以“热液型”或“火山热液型”矿床。
Pyrophyllite, also known as Qingtian stone, Shoushan stone, pyrophyllite is the main component, accompanied by kaolinite, dickite, sericite and quartz and other minerals. Ore is generally yellow, yellowish green and white, with a waxy cryptocrystalline massive agglomeration. The ore is mainly used as refractories, ceramics, glass industrial raw materials and rubber, plastic, paper industry filler, agricultural insecticide carrier, high quality ore can be used as packing material, high quality lump ore is the traditional carved stone. Since most of the previously discovered pyrophyllite deposits were found in volcanic rocks, most researchers believe that the genesis of the pyrophyllite deposits is related to volcanism and intrusions and is characterized by “hydrothermal” or “volcanic Hydrothermal ”deposit.