His analyses are used in the tabulation. The garnet cores are little zoned, but locally the cores have overgrowths of garnet with more Ti, less Cr, and less Fe. The core-overgrowth boundaries are sharp and convolute, suggestive of resorption, and oscillatory zoning is present in the garnet overgrowth. Some late garnet in the groundmass has numerous opx inclusions and appears poikiloblastic. No zoning of opx porphyroclasts was detected.
Phlogopite is later than the shearing.
Fe-Ni sulfide in the groundmass has overgrowths of djerfisherite, and apparently independent grains of both sulfides were also observed. The garnet and orthopyroxene cores probably represent an equilibrium assemblage. The garnet rim - neoblast assemblage may not represent equilibrium. Note that this rock has a large range of orthopyroxene compositions and is thus exceptional. The steepness of the gradients in the garnet rim and the oscillatory zoning there are also remarkable.