OXYGEN FUGACITY ACROSS TECTONIC SETTINGS-Reference-Cited by-同舟云学术

OXYGEN FUGACITY ACROSS TECTONIC SETTINGS

Published:2021-10-13 Issue: Volume: Page:
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Author:

Cottrell Elizabeth¹^ORCID,Birner Suzanne²^ORCID,Brounce Maryjo³^ORCID,Davis Fred⁴^ORCID,Waters Laura⁵^ORCID,Kelley Katherine⁶^ORCID

Affiliation:

1. National Museum of Natural History, Smithsonian Institution

2. Berea College

3. University of California Riverside

4. University of Minnesota Duluth

5. New Mexico Institute of Mining and Technology

6. University of Rhode Island, Graduate School of Oceanography

Funder

Lyda Hill Foundation

Publisher

Wiley

Reference227 articles.

1. n=435 n=98 n=33

2. (all expts compiled by [Borisov et al. 2018]) ("terrestrial" lavas) ("MORB-like" lavas)

3. Kress & Carmichael 1991 0.56 0.59 0.53

4. Hugh St C. O'Neill et al. 2018 0.58 0.79 0.8

5. Borisov et al. 2018 0.38 0.53 0.49 in fO 2 relative to QFM is owing to the differences in ΔV of the QFM reaction and the reaction underlying the spinel oxybarometer (fayalite-ferrosilite-magnetite).

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