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...
Published in: | Polish Polar Research |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Walter de Gruyter GmbH
2010
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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 |