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贵池铜山岩体岩石化学与地球化学特征
引用本文:俞沧海,袁小明.贵池铜山岩体岩石化学与地球化学特征[J].安徽地质,1999(3).
作者姓名:俞沧海  袁小明
作者单位:铜陵有色设计院!安徽铜陵244000(俞沧海),铜陵有色地质队!安徽铜陵244000(袁小明)
摘    要:通过岩石化学、微量元素地球化学、稀土元素地球化学、铅同位素地球化学特征研究表明, 铜山石英闪长岩、花岗闪长岩、二长花岗岩是同一岩浆源同一时期( 燕山早期) 三个侵入阶段的产物, 铜山岩体幔壳同熔型的复式岩体, 属太平洋钙碱性岩石系列。铜山铜矿床的形成与铜山复式岩体的岩浆充分演化分异有关。

关 键 词:复式岩体  钙碱性  岩石化学  地球化学  铜山

THE PETROCHEMICAL AND GEOCHEMICAL CHARACTERISICSOF THE TONGSHAN INTRUSIVE,GUICHI
Yu Canghai ,Yuan Xiaoming.THE PETROCHEMICAL AND GEOCHEMICAL CHARACTERISICSOF THE TONGSHAN INTRUSIVE,GUICHI[J].Geology of Anhui,1999(3).
Authors:Yu Canghai  Yuan Xiaoming
Institution:Yu Canghai 1,Yuan Xiaoming 2
Abstract:Study on the petrochmical,trace element chemical,REE geochemical and Pb isotopic geochemical characteristics of the Tongshan intrusive indicates that the quartz diorite,granodiorite and adamellite are products of three stages of the same period(early Yanshanian)from only one magmatic source.The Tongshan intrusive is a composite one of mantle-crust syntectic type and belongs to Pacific type calc-alkali rock series.The formation of the Tongshan copper deposit is related to the complete magmatic evolution and differentiation of the Tongshan composite intrusive.
Keywords:composite intrusive  calc-alkali  petrochemistry  geochemistry  Tongshan  
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