Fe2+-Mg2+ partition between coexisting cordierite and garnet - a discussion of the experimental data

Bernard J. Wood

doi:10.1007/BF00373789

Fe2+-Mg2+ partition between coexisting cordierite and garnet - a discussion of the experimental data

Bernard J. Wood^*

^*Corresponding author for this work

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

18 Citations (Scopus)

Abstract

The partition of iron and magnesium between cordierite and garnet depends on {Mathematical expression} as well as temperature. The apparently conflicting experimental data on the values of K_D may be reconciled by considering the {Mathematical expression} pertaining during the different experiments.

Original language	English
Pages (from-to)	253-258
Number of pages	6
Journal	Contributions to Mineralogy and Petrology
Volume	40
Issue number	3
DOIs	https://doi.org/10.1007/BF00373789
Publication status	Published - Sept 1973

Access to Document

10.1007/BF00373789

Cite this

@article{02e6d29dd7304cd8a07b09196d2c59fe,

title = "Fe2+-Mg2+ partition between coexisting cordierite and garnet - a discussion of the experimental data",

abstract = "The partition of iron and magnesium between cordierite and garnet depends on {Mathematical expression} as well as temperature. The apparently conflicting experimental data on the values of KD may be reconciled by considering the {Mathematical expression} pertaining during the different experiments.",

author = "Wood, {Bernard J.}",

year = "1973",

month = sep,

doi = "10.1007/BF00373789",

language = "English",

volume = "40",

pages = "253--258",

journal = "Contributions to Mineralogy and Petrology",

issn = "0010-7999",

publisher = "Springer, Springer Nature",

number = "3",

}

TY - JOUR

T1 - Fe2+-Mg2+ partition between coexisting cordierite and garnet - a discussion of the experimental data

AU - Wood, Bernard J.

PY - 1973/9

Y1 - 1973/9

N2 - The partition of iron and magnesium between cordierite and garnet depends on {Mathematical expression} as well as temperature. The apparently conflicting experimental data on the values of KD may be reconciled by considering the {Mathematical expression} pertaining during the different experiments.

AB - The partition of iron and magnesium between cordierite and garnet depends on {Mathematical expression} as well as temperature. The apparently conflicting experimental data on the values of KD may be reconciled by considering the {Mathematical expression} pertaining during the different experiments.

UR - http://www.scopus.com/inward/record.url?scp=0242688419&partnerID=8YFLogxK

U2 - 10.1007/BF00373789

DO - 10.1007/BF00373789

M3 - Article

AN - SCOPUS:0242688419

SN - 0010-7999

VL - 40

SP - 253

EP - 258

JO - Contributions to Mineralogy and Petrology

JF - Contributions to Mineralogy and Petrology

IS - 3

ER -

Fe2+-Mg2+ partition between coexisting cordierite and garnet - a discussion of the experimental data

Abstract

Access to Document

Other files and links

Fingerprint

Cite this