闽西基性脉岩成岩方式的判别

The Magma Process of Mafic Dikes in Western Fujian

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作者张贵山温汉捷胡瑞忠裘愉卓杨光树

机构地区中国科学院地球化学研究所

出处《矿物岩石地球化学通报》 CAS CSCD 2004年第1期62-67,共6页 Bulletin of Mineralogy, Petrology and Geochemistry

基金 ~~

关键词基性脉岩成岩方式微量元素部分熔融分离结晶

参考文献7

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3[8]石林,黄智龙.岩浆作用过程的一种有效判别方法--1/Ci1/Cj和(或)lgCi-lgCj图解法[J].矿物学报,1997,17(2):142-148.Shi Lin, Huang Zhilong. An effective discrminant approach of magmatic processes: Graphic interpretaion of 1/Ci- 1/Cj and (or) lgCi-lgCj[J]. Acta Mineralogica Sinica, 1997, 17(2):142-148. (in Chinese with English abstract)
4汪云亮,王旺章.The Law of Element Abundance Relationships in Igneous Rocks Petrogenetically Associated with Fractional Crystallization[J].Chinese Journal Of Geochemistry,1991,10(3):217-231. 被引量：2
5[14]Allegre C J, Minster J F. Quantitative models of element be havior in magmatic processes [J]. EPSL, 1978,38: 1-25.
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矿物岩石地球化学通报

2004年第1期

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