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青河石(Qingheiite)是一种磷酸盐的新矿物。发现于我国新疆维吾尔自治区青河县西北部的白云母伟晶岩中,以地名命名。标本现存地质部地质博物馆和武汉地质学院北京研究生部地质陈列馆。 一、地质概况 新矿物产出地区属于东准噶尔优地槽褶皱带北缘(晚加里东褶皱与海西褶皱)。出露的地层主要属奥陶系、志留系的变质复理式建造,其次是泥盆系的火山碎屑岩和石炭系的砂岩、砂页岩、变砂岩、灰岩和板岩等。海西期岩浆活动强烈,花岗岩、混合花岗岩及与之有
Qingheiite is a phosphate new mineral. It is found in the muscovite pegmatite from the northwestern part of Qinghe County, Xinjiang Uygur Autonomous Region in China, and is named after the place name. Geological specimens of the Ministry of Geological Museum and Geological Institute of Wuhan Graduate School of Geology Gallery. First, the geological overview The new mineral production area belongs to the East Junggar gifted Trough fold belt North margin (Late Caledonian fold and Hercynian fold). The exposed strata mainly belong to metamorphic and emplacement type of Ordovician and Silurian, followed by Devonian pyroclastic and Carboniferous sandstone, sand shale, sandstone, limestone and slate. Hercynian magmatic activity is intense, granite, mixed granite and with it