Oxygen isotope changes during mica alteration.

S. Komarneni; M. L. Jackson; D. R. Cole

doi:10.1346/CCMN.1985.0330307

Oxygen isotope changes during mica alteration.

S. Komarneni, M. L. Jackson, D. R. Cole

Research output: Contribution to journal › Article › peer-review

6 Scopus citations

Abstract

The extent of oxygen isotope-exchange in structural layers during the weathering of micas to expanding layer silicates has been investigated. Results suggest that oxygen isotope ratios can be used to determine the nature of chemical transformation in such weathering.-D.F.B. Materials Research Lab., Pennsylvania State Univ., University Park, PA 16802, USA.

Original language	English (US)
Pages (from-to)	214-218
Number of pages	5
Journal	Clays & Clay Minerals
Volume	33
Issue number	3
DOIs	https://doi.org/10.1346/CCMN.1985.0330307
State	Published - 1985

All Science Journal Classification (ASJC) codes

Water Science and Technology
Soil Science
Geochemistry and Petrology
Earth and Planetary Sciences (miscellaneous)

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10.1346/CCMN.1985.0330307

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title = "Oxygen isotope changes during mica alteration.",

abstract = "The extent of oxygen isotope-exchange in structural layers during the weathering of micas to expanding layer silicates has been investigated. Results suggest that oxygen isotope ratios can be used to determine the nature of chemical transformation in such weathering.-D.F.B. Materials Research Lab., Pennsylvania State Univ., University Park, PA 16802, USA.",

author = "S. Komarneni and Jackson, {M. L.} and Cole, {D. R.}",

year = "1985",

doi = "10.1346/CCMN.1985.0330307",

language = "English (US)",

volume = "33",

pages = "214--218",

journal = "Clays & Clay Minerals",

issn = "0009-8604",

publisher = "Cambridge University Press",

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T1 - Oxygen isotope changes during mica alteration.

AU - Komarneni, S.

AU - Jackson, M. L.

AU - Cole, D. R.

PY - 1985

Y1 - 1985

N2 - The extent of oxygen isotope-exchange in structural layers during the weathering of micas to expanding layer silicates has been investigated. Results suggest that oxygen isotope ratios can be used to determine the nature of chemical transformation in such weathering.-D.F.B. Materials Research Lab., Pennsylvania State Univ., University Park, PA 16802, USA.

AB - The extent of oxygen isotope-exchange in structural layers during the weathering of micas to expanding layer silicates has been investigated. Results suggest that oxygen isotope ratios can be used to determine the nature of chemical transformation in such weathering.-D.F.B. Materials Research Lab., Pennsylvania State Univ., University Park, PA 16802, USA.

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U2 - 10.1346/CCMN.1985.0330307

DO - 10.1346/CCMN.1985.0330307

M3 - Article

AN - SCOPUS:0022265096

SN - 0009-8604

VL - 33

SP - 214

EP - 218

JO - Clays & Clay Minerals

JF - Clays & Clay Minerals

IS - 3

ER -

Oxygen isotope changes during mica alteration.

Abstract

All Science Journal Classification (ASJC) codes

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