(1.武漢化工學(xué)院資源工程系, 武漢430073;
2.武漢冶金科技大學(xué)資源工程系, 武漢 430081)
摘 要: 以東秦嶺松樹溝超鎂鐵巖體的產(chǎn)狀和鉻鐵礦的產(chǎn)出特征為背景，結(jié)合鉻鐵礦 的組分特征, 對副礦物鉻鐵礦和不同礦石類型鉻鐵礦的穆斯堡爾譜進(jìn)行成礦特征方面的 解釋；并通過與鉻鐵礦形成有關(guān)的宏觀和微觀地質(zhì)現(xiàn)象分析，指出鉻鐵礦體是地幔巖高度熔融形成的富鉻和鎂的極端部分。
關(guān)鍵字: 超鎂鐵巖 鉻鐵礦 穆斯堡爾譜 地幔巖
(
（1.Wuhan Instistute of Chemical Technology, Wuhan 430073 ;
2.Wuhan Metallurgy University of Science and Technology,Wuhan 430081）
Abstract:Based on the occurrence of Dongchinling-shonshugou ultramafic rock and the characteristics of the chromite mineralization as well as the mineral components, a comprehensive explanation of the mineralization characteristics of the various chromites, such as those of being as the accessory minerals and those of different types of ore, has been proposed through the analyses of Mossbaur spectra. In addition, the macroscopic and microscopic gelogical analyses of the mineralizatin of chromite leads to conclusion that the chromite ore body is actually the extreme portions of rich chrome and rich magnesium formed by the highly-melted pyrolite.
Key words: ultramafic rock chromite Mossbaur spectra pyrolite
