Reconstruction of mantle sections beneath Yakutian kimberlite pipes using monomineral thermobarometry
Four original monomineral methods for mantle peridotite associations are used to reconstruct P – T conditions beneath the kimberlite pipes of Yakutia. The clinopyroxene Jd–Di method gives the closest coincidence with Opx barometry in accord with all physico-chemical boundaries. Garnet thermometers c...
Main Authors: | , , , , , , , , , , , , , |
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Format: | Dataset |
Language: | unknown |
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Geological Society of London
2016
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Online Access: | https://dx.doi.org/10.6084/m9.figshare.3454502 https://geolsoc.figshare.com/articles/dataset/Reconstruction_of_mantle_sections_beneath_Yakutian_kimberlite_pipes_using_monomineral_thermobarometry/3454502 |