GEOCHEMICAL STUDY OF GRAYWACKES AS A POSSIBLE STARTING MATERIAL OF PARA-AMPHIBOLITES

被引：13

作者：

RIVALENT.G

SIGHINOL.GP

机构：

[1] Istituto di Mineralogia, Università di Modena

来源：

CONTRIBUTIONS TO MINERALOGY AND PETROLOGY | 1969年 / 23卷 / 03期

关键词：

D O I：

10.1007/BF00371531

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 possibility of para-amphibolites originating from the metamorphic transformation of graywackes is investigated. A series of 35 samples of Vosges graywackes has been studied and the geochemical trends for major and trace elements have been determined to this end. The strong similarity of the geochemical characteristics of this group of graywackes to those of a series of para-amphibolites of the Western Alps conforms to the present hypothesis. By comparing sedimentary geochemical trends with igneous trends one is able to distinguish ortho- from para-derivatives. © 1969 Springer-Verlag.

引用

页码：173 / &

共 42 条

[1] THE LOGNORMAL DISTRIBUTION OF THE ELEMENTS (A FUNDAMENTAL LAW OF GEOCHEMISTRY AND ITS SUBSIDIARY) [J].