Osmium isotopic compositions of mantle xenoliths: a global perspective
The Re-Os isotopic systematics of spinel- and garnet-bearing mantle xenoliths from North and Central America, Europe, southern Africa, Asia, and the Pacific region were determined to define more precisely the isotopic composition of a hypothetical primitive upper mantle (PUM). When plotted against A...
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| Published in | Geochimica et cosmochimica acta Vol. 65; no. 8; pp. 1311 - 1323 |
|---|---|
| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier Ltd
01.04.2001
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| Online Access | Get full text |
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| Abstract | The Re-Os isotopic systematics of spinel- and garnet-bearing mantle xenoliths from North and Central America, Europe, southern Africa, Asia, and the Pacific region were determined to define more precisely the isotopic composition of a hypothetical primitive upper mantle (PUM). When plotted against Al
2O
3 or other melt depletion indicators, the
187Os/
188Os ratios of all xenolith suites display positive trends toward a uniform composition at a fertile mantle composition. A
187Os/
188Os value for PUM of 0.1296 ± 0.0008 (level of confidence 95%) was defined on the basis of 117 spinel-bearing xenoliths from this work and data from the literature, including data for massif peridotites. The
187Os/
188Os ratio of the PUM is similar to the range of compositions defined by ordinary and enstatite chondrites, not carbonaceous chondrites. Spinel-bearing mantle peridotites sampled by volcanism and peridotite massifs appear to have been extracted from a common fertile source (PUM) between 1 and 2 Ga ago. These peridotites now form part of the subcontinental lithospheric mantle underlying continental crust of similar or greater formation age. |
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| AbstractList | The Re-Os isotopic systematics of spinel- and garnet-bearing mantle xenoliths from North and Central America, Europe, southern Africa, Asia, and the Pacific region were determined to define more precisely the isotopic composition of a hypothetical primitive upper mantle (PUM). When plotted against Al
2O
3 or other melt depletion indicators, the
187Os/
188Os ratios of all xenolith suites display positive trends toward a uniform composition at a fertile mantle composition. A
187Os/
188Os value for PUM of 0.1296 ± 0.0008 (level of confidence 95%) was defined on the basis of 117 spinel-bearing xenoliths from this work and data from the literature, including data for massif peridotites. The
187Os/
188Os ratio of the PUM is similar to the range of compositions defined by ordinary and enstatite chondrites, not carbonaceous chondrites. Spinel-bearing mantle peridotites sampled by volcanism and peridotite massifs appear to have been extracted from a common fertile source (PUM) between 1 and 2 Ga ago. These peridotites now form part of the subcontinental lithospheric mantle underlying continental crust of similar or greater formation age. The Re-Os isotopic systematics of spinel- and garnet-bearing mantle xenoliths from North and Central America, Europe, southern Africa, Asia, and the Pacific region were determined to define more precisely the isotopic composition of a hypothetical primitive upper mantle (PUM). When plotted against Al2O3 or other melt depletion indicators, the Os-187/Os-188 ratios of all xenolith suites display positive trends toward a uniform composition at a fertile mantle composition. An Os-187/Os-188 value for PUM of 0.1296 +/- 0.0008 (level of confidence 95 percent) was defined on the basis of 117 spinel-bearing xenoliths from this work and data from the literature, including data for massif peridotites. The Os-Os-187/Os-188 ratio of the PUM is similar to the range of compositions defined by ordinary and enstatite chondrites, not carbonaceous chondrites. Spinel-bearing mantle peridotites sampled by volcanism and peridotite massifs appear to have been extracted from a common fertile source (PUM) between 1 and 2 Ga ago. These peridotites now form part of the subcontinental lithospheric mantle underlying continental crust of similar or greater formation age. (Author) |
| Author | Meisel, Thomas Irving, Anthony J Walker, Richard J Lorand, Jean-Pierre |
| Author_xml | – sequence: 1 givenname: Thomas surname: Meisel fullname: Meisel, Thomas email: meisel@unileoben.ac.at organization: General and Analytical Chemistry, University of Leoben, Franz-Josef-Strasse 18, A-8700 Leoben, Austria – sequence: 2 givenname: Richard J surname: Walker fullname: Walker, Richard J organization: Isotope Geochemistry Laboratory, Department of Geology, University of Maryland, College Park, MD 20742, USA – sequence: 3 givenname: Anthony J surname: Irving fullname: Irving, Anthony J organization: Department of Geological Sciences, University of Washington, Seattle, WA 98195, USA – sequence: 4 givenname: Jean-Pierre surname: Lorand fullname: Lorand, Jean-Pierre organization: Laboratoire de Minéralogie, Muséum National d’Histoire Naturelle, Paris, France |
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