Cryogenic Weathering of Granite, Northern Victoria Land, Antarctica

Cavernous weathering phenomena (‘tafoni’) are well developed on the granitic and gneissic metasedimentary rock of the Northern Foothills region of Antarctica. Thin sections of weathered bedrock indicate that physical disintegration is associated with the preferential micro‐fracturing of quartz miner...

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Bibliographic Details
Main Authors: H. M. French, M. Guglielmin
Format: Article in Journal/Newspaper
Language:unknown
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Online Access:https://doi.org/10.1002/1099-1530(200012)11:43.0.CO;2-T