Diamond Exploration Potential of the Northern East European Platform

In this study, we assess the diamond exploration potential of the northern East European Platform based on aeromagnetic survey results and the morphologic and geochemical analysis of 1513 grains of kimberlite indicator minerals (KIMs), such as purple pyrope garnet, olivine, and Cr-diopside. These mi...

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Main Authors: Elena V. Shchukina, Vladimir S. Shchukin
Format: Article
Language:English
Published: MDPI AG 2018-05-01
Series:Minerals
Subjects:
Online Access:http://www.mdpi.com/2075-163X/8/5/189
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spelling doaj-cf675d32b9ba47798939abb4c00680142020-11-24T21:56:32ZengMDPI AGMinerals2075-163X2018-05-018518910.3390/min8050189min8050189Diamond Exploration Potential of the Northern East European PlatformElena V. Shchukina0Vladimir S. Shchukin1Sobolev Institute of Geology and Mineralogy, Siberian Branch Russian Academy of Sciences, 630090 Novosibirsk, RussiaProex Service Ltd., 163071 Arkhangelsk, RussiaIn this study, we assess the diamond exploration potential of the northern East European Platform based on aeromagnetic survey results and the morphologic and geochemical analysis of 1513 grains of kimberlite indicator minerals (KIMs), such as purple pyrope garnet, olivine, and Cr-diopside. These minerals were recovered from samples collected from modern river and stream sediments in four areas located in the north-eastern (within the Arkhangelsk Diamondiferous Province) and south-western (hundreds of kilometers outside of the Arkhangelsk Diamondiferous Province) parts of the Arkhangelsk region in the European part of Russia. All the studied areas are located within ancient cratons, including the Kola, Karelian, and Shenkursk cratons. Based on the major element compositions of the KIMs and thermobarometric calculations, this study confirms that the lithospheric mantle beneath the studied areas is suitable for the formation and preservation of diamonds. The high percentage of KIMs with primary magmatic grain surface morphologies is evidence of the presence of local kimberlite sources within all of the studied areas. The significant amount of diamond-associated KIMs indicates that the potential sources are diamondiferous. Hence, the results suggest that the studied areas can be recommended for further diamond prospecting activity with a high probability of discovering new diamondiferous kimberlites.http://www.mdpi.com/2075-163X/8/5/189diamondexplorationkimberlite indicator mineralgeochemistrymorphologyEast European PlatformArkhangelsk region
collection DOAJ
language English
format Article
sources DOAJ
author Elena V. Shchukina
Vladimir S. Shchukin
spellingShingle Elena V. Shchukina
Vladimir S. Shchukin
Diamond Exploration Potential of the Northern East European Platform
Minerals
diamond
exploration
kimberlite indicator mineral
geochemistry
morphology
East European Platform
Arkhangelsk region
author_facet Elena V. Shchukina
Vladimir S. Shchukin
author_sort Elena V. Shchukina
title Diamond Exploration Potential of the Northern East European Platform
title_short Diamond Exploration Potential of the Northern East European Platform
title_full Diamond Exploration Potential of the Northern East European Platform
title_fullStr Diamond Exploration Potential of the Northern East European Platform
title_full_unstemmed Diamond Exploration Potential of the Northern East European Platform
title_sort diamond exploration potential of the northern east european platform
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2018-05-01
description In this study, we assess the diamond exploration potential of the northern East European Platform based on aeromagnetic survey results and the morphologic and geochemical analysis of 1513 grains of kimberlite indicator minerals (KIMs), such as purple pyrope garnet, olivine, and Cr-diopside. These minerals were recovered from samples collected from modern river and stream sediments in four areas located in the north-eastern (within the Arkhangelsk Diamondiferous Province) and south-western (hundreds of kilometers outside of the Arkhangelsk Diamondiferous Province) parts of the Arkhangelsk region in the European part of Russia. All the studied areas are located within ancient cratons, including the Kola, Karelian, and Shenkursk cratons. Based on the major element compositions of the KIMs and thermobarometric calculations, this study confirms that the lithospheric mantle beneath the studied areas is suitable for the formation and preservation of diamonds. The high percentage of KIMs with primary magmatic grain surface morphologies is evidence of the presence of local kimberlite sources within all of the studied areas. The significant amount of diamond-associated KIMs indicates that the potential sources are diamondiferous. Hence, the results suggest that the studied areas can be recommended for further diamond prospecting activity with a high probability of discovering new diamondiferous kimberlites.
topic diamond
exploration
kimberlite indicator mineral
geochemistry
morphology
East European Platform
Arkhangelsk region
url http://www.mdpi.com/2075-163X/8/5/189
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