MINERALOGICAL CHANGES OF THE RESIDUAL SOLID AND TRACE-ELEMENT FRACTIONATION DURING PARTIAL INCONGRUENT MELTING

被引：4

作者：

BENITOGARCIA, R ^{[1
]}

LOPEZRUIZ, J ^{[1
]}

机构：

[1] CSIC,MUSEO NACL CIENCIAS NAT,DEPT GEOL,E-28006 MADRID,SPAIN

来源：

GEOCHIMICA ET COSMOCHIMICA ACTA | 1992年 / 56卷 / 10期

关键词：

D O I：

10.1016/0016-7037(92)90163-D

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

The mathematical expressions presented by HERTOGEN and GIJBELS ( 1 976) to treat incongruent melting processes are extended to a more general case where the breakdown of the phases (alpha) takes the form alpha1 + alpha2 + . . . + alpha(n) = beta + delta + gamma + Liq. This modification provides model trace-element fractionation in melts derived from metapelitic rocks, in which muscovite and biotite are always present.

引用

页码：3705 / 3710

页数：6

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