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The alteration of granitic biotite to chlorite.

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1985

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Abstract

Granitic biotite from SE Australia alters to a mixture of chlorite (65%), sphene (10%) and epidote (10%) through a hydrothermal (330-340oC) reaction in which two layers of biotite become one layer of chlorite. The overall reaction conserves Mg in the chlorite, and Ti + Fe + Al within the pseudomorphing chlorite-sphene-epidote assemblage. -J.A.Z.

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https://dspace-test.anu.edu.au/handle/1885/733723604

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DevOps Pure Testing

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American Mineralogist

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Article

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