Metamorphism on Chromite Ores from the Dobromirtsi Ultramafic Massif, Rhodope Mountains (SE Bulgaria)

Podiform chromitite bodies occur in highly serpentinized peridotites at Dobromirtsi Ultramafic Massif (Rhodope Mountains, southeastern Bulgaria). The ultramafic body is believed to represent a fragment of Palaeozoic ophiolite mantle. The ophiolite sequence is associated with greenschist - lower-temp...

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Bibliographic Details

Main Authors:	González-Jiménez, A., Kerestedjian, Thomas, Proenza Fernández, Joaquin Antonio, Gervilla Linares, Fernando
Format:	Article
Language:	English
Published:	Institut de Ciències de la Terra "Jaume Almera" 2009
Subjects:	Ophiolite Chromite Metamorphism Dobromirtsi Ultramafic Massif Bulgaria
Online Access:	https://dialnet.unirioja.es/servlet/oaiart?codigo=3088899
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