The age and origin of megacrysts in the Jericho kimberlite (Nunavut, Canada) ...
Fourteen samples of megacrysts from Jericho kimberlite have been studied. The study includes petrography, geochemistry of major and minor elements, thermobarometry and Sr-Nd-Hf isotopic analyses. The purpose of the study is to determine the relationship between megacrysts and kimberlites (xenocrysta...
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University of British Columbia
2011
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ftdatacite:10.14288/1.0052569 2024-04-28T08:32:56+00:00 The age and origin of megacrysts in the Jericho kimberlite (Nunavut, Canada) ... Marković, Goran 2011 https://dx.doi.org/10.14288/1.0052569 https://doi.library.ubc.ca/10.14288/1.0052569 en eng University of British Columbia article-journal Text ScholarlyArticle 2011 ftdatacite https://doi.org/10.14288/1.0052569 2024-04-02T09:48:03Z Fourteen samples of megacrysts from Jericho kimberlite have been studied. The study includes petrography, geochemistry of major and minor elements, thermobarometry and Sr-Nd-Hf isotopic analyses. The purpose of the study is to determine the relationship between megacrysts and kimberlites (xenocrystal vs cognate) and shed light on the nature of melts parental to kimberlite megacrysts. The Jericho megacrysts include garnet, clinopyroxene, olivine, ilmenite and orthopyroxene. A unique feature of Jericho megacrysts is its gradual transition from discrete megacrysts to megacrystalline pyroxenites. Equilibrium temperatures and pressures were calculated for eight megacryst samples. All calculated P-T place megacrysts into deep garnet-bearing mantle, with T=1200-1280° C and P=60-71 kbar. The P-T estimates for orthopyroxene-bearing samples are identical to P-T estimates for orthopyroxene-free samples, with 195-230 km depth range. Thermobarometric data on Jericho megacrysts cannot give a definitive answer about their ... Text Nunavut DataCite Metadata Store (German National Library of Science and Technology) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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English |
description |
Fourteen samples of megacrysts from Jericho kimberlite have been studied. The study includes petrography, geochemistry of major and minor elements, thermobarometry and Sr-Nd-Hf isotopic analyses. The purpose of the study is to determine the relationship between megacrysts and kimberlites (xenocrystal vs cognate) and shed light on the nature of melts parental to kimberlite megacrysts. The Jericho megacrysts include garnet, clinopyroxene, olivine, ilmenite and orthopyroxene. A unique feature of Jericho megacrysts is its gradual transition from discrete megacrysts to megacrystalline pyroxenites. Equilibrium temperatures and pressures were calculated for eight megacryst samples. All calculated P-T place megacrysts into deep garnet-bearing mantle, with T=1200-1280° C and P=60-71 kbar. The P-T estimates for orthopyroxene-bearing samples are identical to P-T estimates for orthopyroxene-free samples, with 195-230 km depth range. Thermobarometric data on Jericho megacrysts cannot give a definitive answer about their ... |
format |
Text |
author |
Marković, Goran |
spellingShingle |
Marković, Goran The age and origin of megacrysts in the Jericho kimberlite (Nunavut, Canada) ... |
author_facet |
Marković, Goran |
author_sort |
Marković, Goran |
title |
The age and origin of megacrysts in the Jericho kimberlite (Nunavut, Canada) ... |
title_short |
The age and origin of megacrysts in the Jericho kimberlite (Nunavut, Canada) ... |
title_full |
The age and origin of megacrysts in the Jericho kimberlite (Nunavut, Canada) ... |
title_fullStr |
The age and origin of megacrysts in the Jericho kimberlite (Nunavut, Canada) ... |
title_full_unstemmed |
The age and origin of megacrysts in the Jericho kimberlite (Nunavut, Canada) ... |
title_sort |
age and origin of megacrysts in the jericho kimberlite (nunavut, canada) ... |
publisher |
University of British Columbia |
publishDate |
2011 |
url |
https://dx.doi.org/10.14288/1.0052569 https://doi.library.ubc.ca/10.14288/1.0052569 |
genre |
Nunavut |
genre_facet |
Nunavut |
op_doi |
https://doi.org/10.14288/1.0052569 |
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1797589952141197312 |