Oxygen thermobarometry of abyssal spinel peridotites:the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle
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 (f O2 ) of the suboceanic mantle is on average 0.9 ± 0.7 (n = 33; ± 1...
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1990
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/e79f262a-37ea-4523-b6c5-14335f88114e 2024-11-03T14:50:53+00:00 Oxygen thermobarometry of abyssal spinel peridotites:the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle Bryndzia, L. T. Wood, B. J. 1990 https://researchers.mq.edu.au/en/publications/e79f262a-37ea-4523-b6c5-14335f88114e http://www.scopus.com/inward/record.url?scp=0025523388&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Bryndzia , L T & Wood , B J 1990 , ' Oxygen thermobarometry of abyssal spinel peridotites : the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle ' , American Journal of Science , vol. 290 , no. 10 , pp. 1093-1116 . article 1990 ftmacquarieunicr 2024-10-10T00:34:43Z 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 (f O2 ) of the suboceanic mantle is on average 0.9 ± 0.7 (n = 33; ± 1sd) log units below the Fayalite-Magnetite-Quartz (FMQ) f O2 buffer. Suboceanic mantle is more reduced than the subcontinental mantle. -from Authors Article in Journal/Newspaper Antarc* Antarctic Antarctic Ocean Macquarie University Research Portal Antarctic Antarctic Ocean Indian |
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Open Polar |
collection |
Macquarie University Research Portal |
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ftmacquarieunicr |
language |
English |
description |
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 (f O2 ) of the suboceanic mantle is on average 0.9 ± 0.7 (n = 33; ± 1sd) log units below the Fayalite-Magnetite-Quartz (FMQ) f O2 buffer. Suboceanic mantle is more reduced than the subcontinental mantle. -from Authors |
format |
Article in Journal/Newspaper |
author |
Bryndzia, L. T. Wood, B. J. |
spellingShingle |
Bryndzia, L. T. Wood, B. J. Oxygen thermobarometry of abyssal spinel peridotites:the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle |
author_facet |
Bryndzia, L. T. Wood, B. J. |
author_sort |
Bryndzia, L. T. |
title |
Oxygen thermobarometry of abyssal spinel peridotites:the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle |
title_short |
Oxygen thermobarometry of abyssal spinel peridotites:the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle |
title_full |
Oxygen thermobarometry of abyssal spinel peridotites:the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle |
title_fullStr |
Oxygen thermobarometry of abyssal spinel peridotites:the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle |
title_full_unstemmed |
Oxygen thermobarometry of abyssal spinel peridotites:the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle |
title_sort |
oxygen thermobarometry of abyssal spinel peridotites:the redox state and c-o-h volatile composition of the earth's sub-oceanic upper mantle |
publishDate |
1990 |
url |
https://researchers.mq.edu.au/en/publications/e79f262a-37ea-4523-b6c5-14335f88114e http://www.scopus.com/inward/record.url?scp=0025523388&partnerID=8YFLogxK |
geographic |
Antarctic Antarctic Ocean Indian |
geographic_facet |
Antarctic Antarctic Ocean Indian |
genre |
Antarc* Antarctic Antarctic Ocean |
genre_facet |
Antarc* Antarctic Antarctic Ocean |
op_source |
Bryndzia , L T & Wood , B J 1990 , ' Oxygen thermobarometry of abyssal spinel peridotites : the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle ' , American Journal of Science , vol. 290 , no. 10 , pp. 1093-1116 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1814718985133883392 |