84566 6CC 0 0 31.40 32.36 HELM M 27 1 S RT SERPENTINITE 2 S % YOUNGER SERPENTINE (CHRYSOTILE) FILLS 3 S % CROSS-CUTTING VEINS, PROBABLY FORMED DURING 4 S % WEATHERING; 5 S TEX RIBBON; 6 S WS CLAST IN SERPENTINE-BRECCIA* 7 P OL TR 8 P CPX TR 9 P % EXSOLUTION LAMELLAE; 10 P SPINEL TR 11 P % CHROMITE; 12 P OPX TR BASTITE 13 P % BASTITES,PORPHYROCLASTIC TEXTURE* 14 G OL 15 G % MOST LIKELY MANTLE DUNITE-HARZBURGITE, 16 G % PROPHYROCLASTIC TEXTURE OPX, ALTERATION OF MAFIC 17 G % MINERALS TO SERPENTINE UNDER A HIGH STRESS RATIO, 18 G % CHROMITE SHOWS ALTERATION TO FE3O4, EVEN THE 19 G % MAGNETITE IS FOLIATED* 20 A BRUCITE TR 21 A MAGN 10 22 A ACTINOL 0 23 A TREMOL 0 24 A % NO SECONDARY METAMORPHIC MINERALS; 25 A SERP 90 26 A % TWO GENERATIONS* 27 84566 7 1 10 30 41.10 41.12 OGA M 13 1 S RT SERPENTINITE 2 S % ORIGINALLY HARZBURGITE; 3 S TEX GRANULAR* 4 P PLAG 0 5 P CPX 1 6 P % POSSIBLY AUGITE; 7 P SPINEL 1 8 P % CHROMSPINEL; 9 P OPX 13 10 P % POSSIBLY HYPERSTHENE; 11 P OP.MIN 5 12 A CARB TR 13 84566 7 1 20 0 41.10 41.12 BOU M 11 1 S RT SERPENTINITE* 2 P PLAG 0 3 P OL TR 4 P CPX TR 5 P SPINEL TR 6 P % CHROMITE* 7 G MAGN 10 8 G OPX 20 9 G % SERPENTINIZED* 10 A SERP 85 11