Authigenic pyrite framboids in sedimentary facies of the Mount Wawel Formation (Eocene), King George Island, West Antarctica

Authigenic pyrite framboids in sedimentary facies of the Mount Wawel Formation (Eocene), King George Island, West Antarctica Pyrite framboids occur in loose blocks of plant-bearing clastic rocks related to volcano-sedimentary succession of the Mount Wawel Formation (Eocene) in the Dragon and Wanda g...

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Bibliographic Details
Published in:Polish Polar Research
Main Author: Mozer, Anna
Format: Article in Journal/Newspaper
Language:unknown
Published: Walter de Gruyter GmbH 2010
Subjects:
Online Access:http://dx.doi.org/10.2478/v10183-010-0004-2
https://content.sciendo.com/view/journals/popore/31/3/article-p255.xml
https://www.degruyter.com/view/j/popore.2010.31.issue-3/v10183-010-0004-2/v10183-010-0004-2.pdf