OXYGEN THERMOBAROMETRY OF ABYSSAL SPINEL PERIDOTITES - THE REDOX STATE AND C-O-H VOLATILE COMPOSITION OF THE EARTHS SUB-OCEANIC UPPER MANTLE

被引：184
作者：
BRYNDZIA, LT
WOOD, BJ
机构：
[1] NORTHWESTERN UNIV,DEPT GEOL SCI,EVANSTON,IL 60208
[2] UNIV BRISTOL,DEPT GEOL,BRISTOL BS8 1RJ,ENGLAND
来源：
AMERICAN JOURNAL OF SCIENCE | 1990年 / 290卷 / 10期
关键词：
D O I：
10.2475/ajs.290.10.1093
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
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
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页码：1093 / 1116
页数：24
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