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- W2183590112 abstract "The diversity of geologic environments in which the epidote minerals occur is consistent with the large P-J-foi stability range for this important mineral group. Both field and experimental evidence have led to acceptance of epidote as a magmatic phase in deep-seated granitic and granodiorite rocks. In regional metamorphic terranes and geothermal systems, epidote together with hematite may occur at temperatures as Iowas 170-200°C. Epidote is restricted to very low Xco2 environments. The maximum pressure limit of natural epidote is not known; however, epidote is believed to be stable with coesite in ultrahigh-pressure metamorphism as inclusions of coesite pseudomorphs in epidote occur in eclogitic rocks in central China. Compositional variation of epidote with increasing metamorphic grade is highly dependent on rock and fluid chemistry. Only the compositions of epidotes from low-variance assemblages vary systematically with intensive variables and are controlled by continuous reactions, hence can be used as P or T indicators." @default.
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- W2183590112 date "1993-01-01" @default.
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- W2183590112 title "Stabilities of Natural Epidotes" @default.
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