Transmission  electron  microscope study of  biotite  weathering

J. F. Banfield; R. A. Eggleton

doi:10.1346/CCMN.1988.0360107

Transmission electron microscope study of biotite weathering

J. F. Banfield, R. A. Eggleton

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Abstract

TEM suggests that biotite transforms to vermiculite primarily by direct structural modification, involving the replacement of K+ by hydrated interlayer cations, and only minor reorganization of the 2:1 layer. -from Authors

Original language	English
Pages (from-to)	47-60
Number of pages	14
Journal	Clays and Clay Minerals
Volume	36
Issue number	1
DOIs	https://doi.org/10.1346/CCMN.1988.0360107
Publication status	Published - 1988
Externally published	Yes

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title = "Transmission electron microscope study of biotite weathering",

abstract = "TEM suggests that biotite transforms to vermiculite primarily by direct structural modification, involving the replacement of K+ by hydrated interlayer cations, and only minor reorganization of the 2:1 layer. -from Authors",

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T1 - Transmission electron microscope study of biotite weathering

AU - Banfield, J. F.

AU - Eggleton, R. A.

PY - 1988

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N2 - TEM suggests that biotite transforms to vermiculite primarily by direct structural modification, involving the replacement of K+ by hydrated interlayer cations, and only minor reorganization of the 2:1 layer. -from Authors

AB - TEM suggests that biotite transforms to vermiculite primarily by direct structural modification, involving the replacement of K+ by hydrated interlayer cations, and only minor reorganization of the 2:1 layer. -from Authors

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DO - 10.1346/CCMN.1988.0360107

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VL - 36

SP - 47

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JO - Clays and Clay Minerals

JF - Clays and Clay Minerals

IS - 1

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Transmission electron microscope study of biotite weathering

Abstract

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