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Cited by 419

The DOI matches its Crossref record; 4 of the 4 references it cites were found in a registry or an index.

Oxygen isotope partitioning among the minerals in igneous and metamorphic rocks

Bottinga, Y., Javoy, M.·1975·Reviews of Geophysics

Abstract

Using data on naturally occurring oxygen isotope fractionation among coexisting minerals in igneous and metamorphic rocks and previously derived relations, the authors deduce expressions for the temperature dependence of the isotopic disproportionation among the minerals quartz, feldspar, pyroxene, olivine, garnet, muscovite, biotite, amphibole, ilmenite, and magnetite. The expressions are only valid at temperatures greater than about 500°C. Oxygen isotope analyses on separated minerals (quartz, feldspar, pyroxene, olivine, garnet, muscovite, biotite, amphibole, ilmenite, magnetite) published prior to 1974 are reviewed and listed. The great majority of igneous and metamorphic rock samples for which three or more coexisting minerals have been analyzed separately has conserved a state of oxygen isotopic exchange equilibrium. Retrograde effects are common in plutonic and acidic volcanic rocks.

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Crossref · 10.1029/rg013i002p00401

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Metadata

Authors
Bottinga, Y., & Javoy, M.
Venue
Reviews of Geophysics
Published
1975-05
Volume
13
Issue
2
Pages
401-418
ISSN
  • 0096-1043 (ISSN-L)
  • 8755-1209
  • 1944-9208
OpenAlex
W2106537927
Cited by
419
References
4
FWCI
6.78
Type
journal article
Language
en
Open access
closed

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