Rapid Kimberlite Ascent and the Significance of Ar-Ar Ages in Xenolith Phlogopites

Kimberlite eruptions bring exotic rock fragments and minerals, including diamonds, from deep within the mantle up to the surface. Such fragments are rapidly absorbed into the kimberlite magma so their appearance at the surface implies rapid transport from depth. High spatial resolution Ar-Ar age dat...

Full description

Bibliographic Details
Published in:Science
Main Authors: Kelley, S. P., Wartho, J-A.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2000
Subjects:
Online Access:http://dx.doi.org/10.1126/science.289.5479.609
https://www.science.org/doi/pdf/10.1126/science.289.5479.609
id craaas:10.1126/science.289.5479.609
record_format openpolar
spelling craaas:10.1126/science.289.5479.609 2024-09-15T18:16:58+00:00 Rapid Kimberlite Ascent and the Significance of Ar-Ar Ages in Xenolith Phlogopites Kelley, S. P. Wartho, J-A. 2000 http://dx.doi.org/10.1126/science.289.5479.609 https://www.science.org/doi/pdf/10.1126/science.289.5479.609 en eng American Association for the Advancement of Science (AAAS) Science volume 289, issue 5479, page 609-611 ISSN 0036-8075 1095-9203 journal-article 2000 craaas https://doi.org/10.1126/science.289.5479.609 2024-09-05T04:01:17Z Kimberlite eruptions bring exotic rock fragments and minerals, including diamonds, from deep within the mantle up to the surface. Such fragments are rapidly absorbed into the kimberlite magma so their appearance at the surface implies rapid transport from depth. High spatial resolution Ar-Ar age data on phlogopite grains in xenoliths from Malaita in the Solomon Islands, southwest Pacific, and Elovy Island in the Kola Peninsula, Russia, indicate transport times of hours to days depending upon the magma temperature. In addition, the data show that the phlogopite grains preserve Ar-Ar ages recorded at high temperature in the mantle, 700°C above the conventional closure temperature. Article in Journal/Newspaper kola peninsula AAAS Resource Center (American Association for the Advancement of Science) Science 289 5479 609 611
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Kimberlite eruptions bring exotic rock fragments and minerals, including diamonds, from deep within the mantle up to the surface. Such fragments are rapidly absorbed into the kimberlite magma so their appearance at the surface implies rapid transport from depth. High spatial resolution Ar-Ar age data on phlogopite grains in xenoliths from Malaita in the Solomon Islands, southwest Pacific, and Elovy Island in the Kola Peninsula, Russia, indicate transport times of hours to days depending upon the magma temperature. In addition, the data show that the phlogopite grains preserve Ar-Ar ages recorded at high temperature in the mantle, 700°C above the conventional closure temperature.
format Article in Journal/Newspaper
author Kelley, S. P.
Wartho, J-A.
spellingShingle Kelley, S. P.
Wartho, J-A.
Rapid Kimberlite Ascent and the Significance of Ar-Ar Ages in Xenolith Phlogopites
author_facet Kelley, S. P.
Wartho, J-A.
author_sort Kelley, S. P.
title Rapid Kimberlite Ascent and the Significance of Ar-Ar Ages in Xenolith Phlogopites
title_short Rapid Kimberlite Ascent and the Significance of Ar-Ar Ages in Xenolith Phlogopites
title_full Rapid Kimberlite Ascent and the Significance of Ar-Ar Ages in Xenolith Phlogopites
title_fullStr Rapid Kimberlite Ascent and the Significance of Ar-Ar Ages in Xenolith Phlogopites
title_full_unstemmed Rapid Kimberlite Ascent and the Significance of Ar-Ar Ages in Xenolith Phlogopites
title_sort rapid kimberlite ascent and the significance of ar-ar ages in xenolith phlogopites
publisher American Association for the Advancement of Science (AAAS)
publishDate 2000
url http://dx.doi.org/10.1126/science.289.5479.609
https://www.science.org/doi/pdf/10.1126/science.289.5479.609
genre kola peninsula
genre_facet kola peninsula
op_source Science
volume 289, issue 5479, page 609-611
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.289.5479.609
container_title Science
container_volume 289
container_issue 5479
container_start_page 609
op_container_end_page 611
_version_ 1810454946840051712