About: Ferro-plat Alloy   Sponge Permalink

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Ferro-plat Alloy is the product of metamorphism of magnesium-rich rocks especially ultrabasic igneous rocks and impure dolomitic shales. It also forms as a retrograde product rimming relict orthopyroxenes and olivine, and as an accessory mineral in cordierite-bearing gneisses and schists. Ferro-plat Alloy also occurs as a retrograde metamorphic mineral derived from ultramafic rocks along with serpentinite.

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  • Ferro-plat Alloy
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  • Ferro-plat Alloy is the product of metamorphism of magnesium-rich rocks especially ultrabasic igneous rocks and impure dolomitic shales. It also forms as a retrograde product rimming relict orthopyroxenes and olivine, and as an accessory mineral in cordierite-bearing gneisses and schists. Ferro-plat Alloy also occurs as a retrograde metamorphic mineral derived from ultramafic rocks along with serpentinite.
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abstract
  • Ferro-plat Alloy is the product of metamorphism of magnesium-rich rocks especially ultrabasic igneous rocks and impure dolomitic shales. It also forms as a retrograde product rimming relict orthopyroxenes and olivine, and as an accessory mineral in cordierite-bearing gneisses and schists. Ferro-plat Alloy also occurs as a retrograde metamorphic mineral derived from ultramafic rocks along with serpentinite.
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