Hornblende granulite subfacies is a transitional coexistence region of anhydrous and hydrated ferromagnesian minerals, so the above-mentioned isograds mark the boundary with " pyroxene granulite subfacies " facies with completely anhydrous mineral assemblages.
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Hornblende granulite subfacies is a transitional coexistence region of anhydrous and hydrated ferromagnesian minerals, so the above-mentioned isograds mark the boundary with " pyroxene granulite subfacies " facies with completely anhydrous mineral assemblages.
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