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Phase relation among serpentine, brucite and forsterite from 200 to 500atm water pressure.

Teiichi Ueno, Yukihiro Furuta, Takako Koyama, Takeo Imada

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Abstract

Phase relation among serpentine, brucite and forsterite was examined by test-tube type hydrothermal synthetic experiments at water pressures from 200 to 500 atm. It was confirmed that the tie line change reaction curve of serpentine + brucite ←→ forsterite + water passes through the points of 200±20 atm and 310±20°C, 300±20 atm and 325±20°C, and 500±20 atm and 350±20°C.

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Phase relation among serpentine, brucite and forsterite was examined by test-tube type hydrothermal synthetic experiments at water pressures from 200 to 500 atm. It was confirmed that the tie line change reaction curve of serpentine + brucite ←→ forsterite + water passes through the points of 200±20 atm and 310±20°C, 300±20 atm and 325±20°C, and 500±20 atm and 350±20°C.

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Available abstract

Phase relation among serpentine, brucite and forsterite was examined by test-tube type hydrothermal synthetic experiments at water pressures from 200 to 500 atm. It was confirmed that the tie line change reaction curve of serpentine + brucite ←→ forsterite + water passes through the points of 200±20 atm and 310±20°C, 300±20 atm and 325±20°C, and 500±20 atm and 350±20°C.

Key concepts: Brucite, Forsterite, Hydrothermal circulation, Phase (matter), Geology, Mineralogy, Materials science, Chemistry

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