Spinel lherzolite of the Northern Kraka Massif (Southern Urals): Relics of the least transformed matter of the upper mantle

During the last twenty years a large body of material on estimation of the redox state of harzburgite-lherzolite series (HLS) by modern methods of oxythermobarometry has been accumulated. These series are abundant in different tectonic environments of continents and oceans, namely in massifs of root...

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Published in:Doklady earth sciences 2010-04, Vol.431 (2), p.462-465
Main Authors: Chashchukhin, I. S., Votyakov, S. L.
Format: Article
Language:English
Subjects:
Analysis
Earth
Earth and Environmental Science
Earth Sciences
Geochemistry
Geophysics
Inclusions
Kimberlite
Mantle
Mid-ocean ridges
Mineralogy
Oceans
Plate tectonics
Rocks, Igneous
Spinel group
Temperature
Transform faults
Upper mantle
Volcanic rocks
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Votyakov, S. L.
description During the last twenty years a large body of material on estimation of the redox state of harzburgite-lherzolite series (HLS) by modern methods of oxythermobarometry has been accumulated. These series are abundant in different tectonic environments of continents and oceans, namely in massifs of root zones, ophiolites, mid-ocean ridges, and transform faults, and they compose xenoliths in alkaline volcanic rocks and kimberlite as well.
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ispartof Doklady earth sciences, 2010-04, Vol.431 (2), p.462-465
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1531-8354
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subjects Analysis
Earth
Earth and Environmental Science
Earth Sciences
Geochemistry
Geophysics
Inclusions
Kimberlite
Mantle
Mid-ocean ridges
Mineralogy
Oceans
Plate tectonics
Rocks, Igneous
Spinel group
Temperature
Transform faults
Upper mantle
Volcanic rocks
title Spinel lherzolite of the Northern Kraka Massif (Southern Urals): Relics of the least transformed matter of the upper mantle
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