Calcite deformation twins in Pohorje marbles

Marbles in Pohorje occur in lenses and smaller bodies in the southern and southeastern part of the massif. Marbles are very pure, predominantly calcitic and rarely calcitic-dolomitic, containing a maximum of 5 % of non-carbonate mineral phases. The latter comprise pyroxenes (diopside), amphiboles...

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Bibliographic Details
Published in:	Geologija
Main Authors:	Mirijam Vrabec, Nastja Rogan Šmuc, Marko Vrabec
Format:	Article
Language:	English
Published:	Geological Survey of Slovenia 2018-11-01
Subjects:	calcite marble deformation twins paleotemperature Pohorje Eastern Alps
Online Access:	http://www.geologija-revija.si/dokument.aspx?id=1332

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