European Geosciences Union General Assembly 2015 - Garnet Classification slide image

European Geosciences Union General Assembly 2015 - Garnet Classification

Evolution of metasomatic agent for Group III-V In the mantle peridotite xenoliths suit we have a nature example of this model: A zoned garnet crystal, which has progressive change of composition from relict zone with "sinusoidal"- harzburgitic REE profiles to megacryst-like REE profiles for the latest zone. Ziberna et al., 2013: Plate model numerical simulation Gar / C1 (Sun & McDonough, 1989) 100 V 10 0.1 0.01 EUROPEAN O 466-2 rim GEOSCIENCES UN General Assembly 2015 466-2 core Group V La Ce Pr Nd Pm Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Grt/CI 100 (c) 10 1 cell, Grt Z4-3 (group B) 0.1 14th cell Grt Z4-8 (group C) 0.01 Grt Z5-14 (group C) Grt in the ambient peridotite (from Grt Z4-11) CC 0.001 Ο BY La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu 100 мт [email protected] 100μm 18
View entire presentation