新疆黄山镁铁-超镁铁杂岩体矿物化学成分特征及与含矿(Ni)性关系  

On the Relations between the Characteristics of Chemical Compositions of Minerals and the Characteristics of Ore-bearing Potential(Ni)of Huangshan Mafic-ultramafic Complex in Xinjing

作　　者：傅学明[1] 郭原生[1] 刘凤山[1] 张铭杰[1] 孙淑荣[1] 

机构地区：[1]兰州大学地质系,兰州730000

出　　处：《兰州大学学报（自然科学版）》1993年第4期236-240,共5页Journal of Lanzhou University(Natural Sciences)

摘　　要：本文对新疆黄山镁铁—超镁铁杂岩体中主要造岩矿物橄榄石,斜方辉石,单斜辉石及角闪石化学成分特征作了比较深入的研究.在此基础上,分析了岩体含矿(Ni)性与矿物化学成分间的关系,得出了岩体含矿的主要矿物化学标志.This paper has made a penetrating study on the characteristics of chemicalcompositions of olivine,orthopyroxene,clino-augite,and hornblende,the chieb rock-forming minerals of Huangshan mafic-ultramafic complex in Xinjing.Based on the abovestudy,the relations between ore-bearing Potential(Ni)of the pluton and the chemicalcompositions,of those minerals have been analyzed,and the chemical signs of the chiefrock-forming minerals in plutons havebeen found out.

关 键 词：橄榄石 斜方辉石 基性岩 超基性岩 

分 类 号：P588.12[天文地球—岩石学]