新疆黄山镁铁—超镁铁杂岩体化学成分特征及其与含矿性关系  

The Features of Chemical Compostitions of Huangshan Mafic—ultramafic Complex and Their Relationsto to Ore—bearing Polential in Xinjiang

作　　者：傅学明[1] 郭原生[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3期213-221,共9页Journal of Lanzhou University(Natural Sciences)

摘　　要：黄山岩体是含有较大型铜镍硫化矿床的镁铁—超镁铁杂岩体。本文通过岩体主要造岩元素、微量元素及稀土元素特征的研究,较深入地探讨了岩体化学成分特征与含矿性间的关系。The Huangshan pluton is a mafic—ultramafic complez coptaioning a larger—scale Cu—Ni sulfide. This paper studied the features of petrogenetic elements, trace elements and rare earth elements, and a correlative matrix analysis was male, On this basis, the relations between the characteristics of chemical compositions of pluton and thd orebearing potential are discussed extensively.

关 键 词：超基性岩 稀土族 含矿性 微量元素 

分 类 号：P588.125[天文地球—岩石学]