Chlorine and fluorine in granitic rocks from S.W. England

R. Fuge; G. M. Power

doi:10.1016/0016-7037(69)90035-0

Chlorine and fluorine in granitic rocks from S.W. England

R. Fuge^*, G. M. Power

^*Corresponding author for this work

Department of Geography & Earth Sciences

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

27 Citations (Scopus)

Abstract

Ninety unaltered granites from S.W. England show log-normal distributions for both Cl and F with mean Cl, 507 ppm and mean F 1395 ppm. Greisening increases F but kaolinisation and reddening reduce F. All these effects cause large decreases in Cl and altered granites form a separate log-normal population in this element.

Original language	English
Pages (from-to)	888-893
Number of pages	6
Journal	Geochimica et Cosmochimica Acta
Volume	33
Issue number	7
DOIs	https://doi.org/10.1016/0016-7037(69)90035-0
Publication status	Published - Jul 1969

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title = "Chlorine and fluorine in granitic rocks from S.W. England",

abstract = "Ninety unaltered granites from S.W. England show log-normal distributions for both Cl and F with mean Cl, 507 ppm and mean F 1395 ppm. Greisening increases F but kaolinisation and reddening reduce F. All these effects cause large decreases in Cl and altered granites form a separate log-normal population in this element.",

author = "R. Fuge and Power, \{G. M.\}",

year = "1969",

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doi = "10.1016/0016-7037(69)90035-0",

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TY - JOUR

T1 - Chlorine and fluorine in granitic rocks from S.W. England

AU - Fuge, R.

AU - Power, G. M.

PY - 1969/7

Y1 - 1969/7

N2 - Ninety unaltered granites from S.W. England show log-normal distributions for both Cl and F with mean Cl, 507 ppm and mean F 1395 ppm. Greisening increases F but kaolinisation and reddening reduce F. All these effects cause large decreases in Cl and altered granites form a separate log-normal population in this element.

AB - Ninety unaltered granites from S.W. England show log-normal distributions for both Cl and F with mean Cl, 507 ppm and mean F 1395 ppm. Greisening increases F but kaolinisation and reddening reduce F. All these effects cause large decreases in Cl and altered granites form a separate log-normal population in this element.

UR - https://www.scopus.com/pages/publications/4243947361

U2 - 10.1016/0016-7037(69)90035-0

DO - 10.1016/0016-7037(69)90035-0

M3 - Article

AN - SCOPUS:4243947361

SN - 0016-7037

VL - 33

SP - 888

EP - 893

JO - Geochimica et Cosmochimica Acta

JF - Geochimica et Cosmochimica Acta

IS - 7

ER -

Chlorine and fluorine in granitic rocks from S.W. England

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