Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth?
Nd and Sr isotopic data from diamond-bearing eclogites found in the Udachnaya kimberlite, Yakutia, Siberia, are interpreted as indicating an early ([ges] 4 Ga) differentiation event, whereby the mantle split into complementary depleted and enriched reservoirs. Reconstructed whole-rock 87Sr/86Sr rati...
Published in: | Earth and Planetary Science Letters |
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ftumdeepblue:oai:deepblue.lib.umich.edu:2027.42/30700 2023-08-20T04:10:20+02:00 Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth? Snyder, Gregory A. Jerde, Eric A. Taylor, Lawrence A. Halliday, Alexander N. Sobolev, Vladimir N. Sobolev, Nikolai V. Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, USA Department of Geological Sciences, University of Tennessee, Knoxville, TN 37996, USA Institute of Mineralogy and Petrography, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia 1993-07 821029 bytes 3118 bytes application/pdf text/plain https://hdl.handle.net/2027.42/30700 http://www.sciencedirect.com/science/article/B6V61-47251VV-1W/2/c26fa91062d2a8af0e093f61b20adc9e https://doi.org/10.1016/0012-821X(93)90161-2 en_US eng Elsevier Snyder, Gregory A., Jerde, Eric A., Taylor, Lawrence A., Halliday, Alex N., Sobolev, Vladimir N., Sobolev, Nikolai V. (1993/07)."Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth?." Earth and Planetary Science Letters 118(1-4): 91-100. <http://hdl.handle.net/2027.42/30700> http://www.sciencedirect.com/science/article/B6V61-47251VV-1W/2/c26fa91062d2a8af0e093f61b20adc9e https://hdl.handle.net/2027.42/30700 http://dx.doi.org/10.1016/0012-821X(93)90161-2 Earth and Planetary Science Letters IndexNoFollow Geology and Earth Sciences Science Article 1993 ftumdeepblue https://doi.org/10.1016/0012-821X(93)90161-2 2023-07-31T21:13:57Z Nd and Sr isotopic data from diamond-bearing eclogites found in the Udachnaya kimberlite, Yakutia, Siberia, are interpreted as indicating an early ([ges] 4 Ga) differentiation event, whereby the mantle split into complementary depleted and enriched reservoirs. Reconstructed whole-rock 87Sr/86Sr ratios (present-day) range from 0.70151 to 0.70315 and are consistent with a mantle origin for these rocks. The Nd isotopic evolution lines of four samples (U-5, U-37, U-41 and U-79) converge at 2.2-2.7 Ga. Sample U-5 is unique in exhibiting the most enriched signature of any of the samples yet analyzed (present-day [epsilon]Nd of -20), and this sample points unequivocally to an old, enriched component. A complementary depleted mantle component is suggested by two of the eclogite samples, U-86 and U-25, which yield [epsilon]Nd values (at 2.2 Ga) of + 13 and + 7, respectively. The two mantle reservoirs possibly formed prior to 4 Ga and evolved separately until 2.2-2.7 Ga. At that time, the reservoirs were melted forming eclogites both as residues (from the enriched reservoir) and as partial melts of peridotite (from the depleted reservoir), resulting in demonstrably different histories for eclogites from the same locality. Peer Reviewed http://deepblue.lib.umich.edu/bitstream/2027.42/30700/1/0000345.pdf Article in Journal/Newspaper Yakutia Siberia University of Michigan: Deep Blue Earth and Planetary Science Letters 118 1-4 91 100 |
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English |
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Geology and Earth Sciences Science |
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Geology and Earth Sciences Science Snyder, Gregory A. Jerde, Eric A. Taylor, Lawrence A. Halliday, Alexander N. Sobolev, Vladimir N. Sobolev, Nikolai V. Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth? |
topic_facet |
Geology and Earth Sciences Science |
description |
Nd and Sr isotopic data from diamond-bearing eclogites found in the Udachnaya kimberlite, Yakutia, Siberia, are interpreted as indicating an early ([ges] 4 Ga) differentiation event, whereby the mantle split into complementary depleted and enriched reservoirs. Reconstructed whole-rock 87Sr/86Sr ratios (present-day) range from 0.70151 to 0.70315 and are consistent with a mantle origin for these rocks. The Nd isotopic evolution lines of four samples (U-5, U-37, U-41 and U-79) converge at 2.2-2.7 Ga. Sample U-5 is unique in exhibiting the most enriched signature of any of the samples yet analyzed (present-day [epsilon]Nd of -20), and this sample points unequivocally to an old, enriched component. A complementary depleted mantle component is suggested by two of the eclogite samples, U-86 and U-25, which yield [epsilon]Nd values (at 2.2 Ga) of + 13 and + 7, respectively. The two mantle reservoirs possibly formed prior to 4 Ga and evolved separately until 2.2-2.7 Ga. At that time, the reservoirs were melted forming eclogites both as residues (from the enriched reservoir) and as partial melts of peridotite (from the depleted reservoir), resulting in demonstrably different histories for eclogites from the same locality. Peer Reviewed http://deepblue.lib.umich.edu/bitstream/2027.42/30700/1/0000345.pdf |
author2 |
Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, USA Department of Geological Sciences, University of Tennessee, Knoxville, TN 37996, USA Institute of Mineralogy and Petrography, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia |
format |
Article in Journal/Newspaper |
author |
Snyder, Gregory A. Jerde, Eric A. Taylor, Lawrence A. Halliday, Alexander N. Sobolev, Vladimir N. Sobolev, Nikolai V. |
author_facet |
Snyder, Gregory A. Jerde, Eric A. Taylor, Lawrence A. Halliday, Alexander N. Sobolev, Vladimir N. Sobolev, Nikolai V. |
author_sort |
Snyder, Gregory A. |
title |
Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth? |
title_short |
Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth? |
title_full |
Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth? |
title_fullStr |
Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth? |
title_full_unstemmed |
Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth? |
title_sort |
nd and sr isotopes from diamondiferous eclogites, udachnaya kimberlite pipe, yakutia, siberia: evidence of differentiation in the early earth? |
publisher |
Elsevier |
publishDate |
1993 |
url |
https://hdl.handle.net/2027.42/30700 http://www.sciencedirect.com/science/article/B6V61-47251VV-1W/2/c26fa91062d2a8af0e093f61b20adc9e https://doi.org/10.1016/0012-821X(93)90161-2 |
genre |
Yakutia Siberia |
genre_facet |
Yakutia Siberia |
op_relation |
Snyder, Gregory A., Jerde, Eric A., Taylor, Lawrence A., Halliday, Alex N., Sobolev, Vladimir N., Sobolev, Nikolai V. (1993/07)."Nd and Sr isotopes from diamondiferous eclogites, Udachnaya Kimberlite Pipe, Yakutia, Siberia: Evidence of differentiation in the early Earth?." Earth and Planetary Science Letters 118(1-4): 91-100. <http://hdl.handle.net/2027.42/30700> http://www.sciencedirect.com/science/article/B6V61-47251VV-1W/2/c26fa91062d2a8af0e093f61b20adc9e https://hdl.handle.net/2027.42/30700 http://dx.doi.org/10.1016/0012-821X(93)90161-2 Earth and Planetary Science Letters |
op_rights |
IndexNoFollow |
op_doi |
https://doi.org/10.1016/0012-821X(93)90161-2 |
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Earth and Planetary Science Letters |
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118 |
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1-4 |
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91 |
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100 |
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1774724454389121024 |