中国非金属矿工业导刊Issue(1)：48-51,57,5.
新疆哈密横山冶镁用白云岩矿床地质特征及成因探讨
Geological Characteristics and Genesis of Dolomite Ore for Magnesium Smelting in Hengshan of Hami,Xinjiang
摘要
Abstract
Kawabulake Group strata of Jixian System was widely exposed in Weiya-Tianhu area of Hami,Xinjiang.Dolomite Ore for Magnesium Smelting is mainly produced in the third rock formation of the Kawabulake Group.The main mineral in Hengshan dolomite mining area is dolomite for magnesium smelting,and the symbiotic mineral is dolomite for flux.Four dolomite ore bodies for magnesium smelting have been delineated,with the main ore body k1 measuring 4430m in length and 18.60-165.23m in thickness,with an average thickness of approximately 122.04m.The main ore type is Finely crystalline dolomite.The main mineral composition is dolomite.Mineral deposits meet the requirements of magnesium smelting dolomite ore industry index.The genesis type of the deposit is shallow sea shelf sedimentary metamorphic carbonate rock deposit.关键词
冶镁用白云岩/矿床地质特征/矿床成因/哈密横山/新疆Key words
magnesium smelte dolomite/geological characteristics/sedimentary genesis/Hengshan of Hami/Xinjiang分类
天文与地球科学引用本文复制引用
黄同新,吴煜,王红军,马玉昊..新疆哈密横山冶镁用白云岩矿床地质特征及成因探讨[J].中国非金属矿工业导刊,2026,(1):48-51,57,5.基金项目
哈密市财政出资地质勘查基金项目"新疆哈密市横山白云岩矿普查"(编号:GYZB-HMKC2024-11). （编号:GYZB-HMKC2024-11）
