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西藏中南部各类花岗岩中磁铁矿标型特征的研究
引用本文:丁孝石. 西藏中南部各类花岗岩中磁铁矿标型特征的研究[J]. 岩石矿物学杂志, 1986, 5(1): 53-68
作者姓名:丁孝石
作者单位:中国地质科学院矿床地质研究所
摘    要:磁铁矿是最常见的贯通矿物之一,各种地质体中均可见到。不同成因的磁铁矿,其化学成分,内部结构和物理性质等是有差异的。因此,根据磁铁矿的某些特征来探讨其岩体成因是有一定意义的。


Study of Typomorphic Characteristics of Magnetite in Various Types of Granites of Central-South :Kizang (Tibet)
Abstract:In studying the characteristics of magnetite and other accessory minerals''in various granitic rocks of Central-South Xizang, the author found that magibetites from different types of granites formed under different geological con-dlitions and of different ages have distinctly different characteristic features.The content and chemical composition of magnetite as well as the mineralassemblage and rare-earth pattern in the granite all reflect either the man-tle or crustal origin of the rock. It is concluded that the granodiorite in theGangdise belt is characterized by mantle origin and the muscovite-biotitegranite and tourmaline granite in Nielamu district are of crustal origin.
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