Journal article
OXYGEN THERMOBAROMETRY OF ABYSSAL SPINEL PERIDOTITES - THE REDOX STATE AND C-O-H VOLATILE COMPOSITION OF THE EARTHS SUB-OCEANIC UPPER MANTLE
- Abstract:
- We have applied the spinel peridotite oxygen barometer to abyssal spinel peridotites from the mid-Atlantic, central Indian, southwest Indian and American-Antarctic ocean ridge systems. The results indicate that the oxygen fugacity (fO2) of the suboceanic mantle is on average 0.9 ± 0.7 (n = 33; ± 1sd) log units below the Fayalite-Magnetite-Quartz (FMQ) fO2 buffer. Suboceanic mantle is more reduced than the subcontinental mantle. -from Authors
- Publication status:
- Published
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Authors
- Journal:
- AMERICAN JOURNAL OF SCIENCE More from this journal
- Volume:
- 290
- Issue:
- 10
- Pages:
- 1093-1116
- Publication date:
- 1990-12-01
- DOI:
- ISSN:
-
0002-9599
- Pubs id:
-
pubs:172884
- UUID:
-
uuid:25dbe951-b660-49ff-9f52-9dbe8b38ccfe
- Local pid:
-
pubs:172884
- Source identifiers:
-
172884
- Deposit date:
-
2012-12-19
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- Copyright date:
- 1990
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