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一、概况陕西略阳白水江高岭石矿,位于秦岭褶皱系南秦岭加里东褶皱带的西北缘。矿区主要出露地层为中、上志留统大河店组浅变质的浅海相碎屑岩和碳酸盐岩及少量第三系紫红色砂砾岩不整合于大河店组之上。矿区仅有数条二长斑岩脉。该矿手选后的矿石可用于生产日用陶瓷和卫生陶瓷,有的可用于生产工艺美术品,质地细腻,色彩鲜艳,花纹美观,是一种新型
I. Overview Lüsanjiang kaolinite mine in Lueyang, Shaanxi is located in the northwestern margin of the Caledonian fold belt in the South Qinling Fold System in the Qinling Mountains. The main exposed strata in the mine area are middle-upper Shashi Formation of the Upper Silurian Formation metamorphic shallow marine clastic rocks and carbonate rocks and a small amount of Tertiary purplish red sandy conglomerate are not integrated in the Dahedian Formation. The mining area has only a few two long porphyry veins. The mine ore after the election can be used for the production of daily ceramics and sanitary ceramics, and some can be used for the production of arts and crafts, delicate texture, colorful, beautiful patterns, is a new type