The Paragenesis of Swedish Glacial Clays
作者:
MalcolmJ. McNamara,
期刊:
Geologiska Föreningen i Stockholm Förhandlingar
(Taylor Available online 1966)
卷期:
Volume 87,
issue 4
页码: 441-454
ISSN:0016-786X
年代: 1966
DOI:10.1080/11035896609448315
出版商: Taylor & Francis Group
数据来源: Taylor
摘要:
The feldspars in Swedish glacial clays include K-feldspar, low albite and intermediate plagioclases, but not peristerites. The hydrolysis of K-feldspar leads to the formation of illite under glacial conditions of P, T and μmobile components; chlorite is the stable ferromagnesian mineral in the unweathered clays. Illite + albite + quartz represents a lower energy assemblage than K-feldspar + Na-montmorillonite + quartz.
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