Weathering and Hydrothermal Alteration of Mica Minerals.
Yoshihiro Kuwahara
Abstract
Yoshihiro Kuwahara
Abstract
The alteration of trioctahedral micas (biotite, phlogopite, etc.) have been the subject of many studies on weathering and hydrothermal alteration, because they are common rock-forming minerals and act as an important source of soluble K in soil. In this paper, the dissolution process of micas and the formation mechanism of alteration products such as vermiculite, chlorite and kaolinite in the alteration process of micas are reviewed briefly.
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The alteration of trioctahedral micas (biotite, phlogopite, etc.) have been the subject of many studies on weathering and hydrothermal alteration, because they are common rock-forming minerals and act as an important source of soluble K in soil. In this paper, the dissolution process of micas and the formation mechanism of alteration products such as vermiculite, chlorite and kaolinite in the alteration process of micas are reviewed briefly.
Key concepts: Mica, Weathering, Biotite, Hydrothermal circulation, Phlogopite, Geochemistry, Chlorite, Kaolinite