Chemical weathering signatures from Mt. Achernar Moraine, Central Transantarctic Mountains I: Subglacial sediments compared with underlying rock
In order to determine chemical weathering rates on the subglacial land surface of Antarctica, we compare the composition and mineralogy of freshly emerging fine sediments to that of the underlying bedrock, as represented by glacially derived cobble-sized clasts. Samples were collected from Mt. Acher...
Main Authors: | , , , |
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Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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Elsevier
2020
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Subjects: | |
Online Access: | https://hdl.handle.net/1805/27724 |