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The most characteristic infrared (IR) spectral \nshape of shock-annealed sub-grained pyroxene was identified: \nthe strongest peak occurs at 860 cm−1 with a smaller shoulder \nat 837−840 cm−1, and small bands are at 686, 635−638, and \n1,044−1,050 cm−1. The appearance of forbidden bands in \npyroxene and shift of band positions to a lower wave number \nin olivines clearly demonstrate the crystal lattice \ndisordering due to shock metamorphism. The shock annealing \nproduced mixed dark melt along fractures, which consists of \nfeldspar−pyroxene and olivine−pyroxene melt. The dark shock \nmelt at sub-grain boundaries of shocked pyroxenes and along \nfracture of pyroxenes is characterized by elevated Ca, Na, \nand Al content relative to its environment, detected by \nelement mapping. So far, shock deformation of pyroxene and \nolivine was not studied by IR spectroscopy; this method has \nturned out to be a powerful tool in identifying the mixed \ncomposition of shock melt minerals. 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