论文部分内容阅读
科伊塔什硅灰石矿床分部在北努拉钦山脉的南坡,在西乌兹别克泽拉夫森—土尔克斯坦和土尔克斯垣—阿菜建造带的范围内。该矿床产于科伊塔什侵入体(C_3—P_1)与海西构造期(C_2—C_3)的沉积变质岩系地层的南部接触带。由于侵入体热量和岩浆期后溶液的影响,喷发—沉积杂岩遭受了巨大的变质改造,结果形成了各种接触变质岩石及接触交代岩石。热变质作用在科伊塔什矿田的南部碳酸
The Koitash wollastonite deposit is located on the southern slope of the northern Nulaqin mountain range, within the Zieuzze-Turku and Western Tupye-A-cab belt of Western Uzbekistan. The deposit was produced in the southern contact zone of the sedimentary metamorphic strata of the Coitacea intrusive body (C_3-P_1) and the Hercynian structural period (C_2-C_3). Due to the heat of the invaded body and the influence of the solution after the magmatic period, the eruption-sedimentary complex underwent a tremendous metamorphism and alteration, resulting in various types of contact metamorphic rocks and contact metasomatism rocks. Thermal metamorphism occurs in the southern carbonic acid of the Coittham field