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...

Full description

Bibliographic Details
Main Authors: I. V. Ashchepkov, N. P. Pokhilenko, N. V. Vladykin, A. Y. Rotman, V. P. Afanasiev, A. M. Logvinova, S. I. Kostrovitsky, L. N. Pokhilenko, M. A. Karpenko, S. S. Kuligin, E. V. Malygina, Y. B. Stegnitsky, N. A. Alymova, O. S. Khmelnikova
Format: Dataset
Language:unknown
Published: Geological Society of London 2016
Subjects:
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