European Geosciences Union General Assembly 2015 - Garnet Classification slide image

European Geosciences Union General Assembly 2015 - Garnet Classification

5 peridotite groups - Groups IV-V Groups IV-V contain: ā†’ Garnets with low concentration of TiO, and mildly (Group IV) to humped (Group V) "sinusoidal" Cl-normalized REE patterns with a maximum at Nd-Sm and a minimum at Dy-Ho; these garnets are comparable with G9 and G10 garnets accordingly and have depleted peridotite origin by [Griffin et al., 1999]; ā†’ Clinopyroxenes (Group IV) have the highest degrees of REE profiles with flat pattern for LREE and depleted in Ti. 100 Gar / C1 (Sun & McDonough, 1989) 10 10 1 0.1 0.01 IV Megacrysts TiO2 < 0.2 wt.% Group IV garnet La Ce Pr Nd Pm Sm Eu Gd Tb Dy Ho Er Tm Yb Lu 100 10 V Gar / C1 (Sun & McDonough, 1989) T EUROPEAN GEOSCIENCES UN Assembly General! 2015 0.01 Megacrysts TiO2 <0.2 wt.% Group V garnet La Ce Pr Nd Pm Sm Eu Gd Tb Dy Ho Er Tm Yb Lu 100 Cpx / C1 (Sun & McDonough, 1989) 10 = 10 La/Ybn - 32-176 IV 0,1 0,01 TiO, < 0.25 wt.% Group IV clinopyroxene La Ce Pr Nd Pm Sm Eu Gd Tb Dy Ho Er Tm Yb Lu [email protected] CC BY 13
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