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FORMATION OF EPIDOTE IN TANGANYIKA
Geological Society of America Bulletin, 1954Minerals of the epidote group in Tanganyika are commonly produced during cataclasis of lime-bearing rocks; invariable accession of the hydroxyl radical during dislocation assists their formation. Epidote minerals are not produced from plagioclase by the action of water, even at high temperatures and pressures; shearing stress or the presence of other ...
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Fluid Inclusions in Epidote Minerals and Fluid Development in Epidote-Bearing Rocks
Reviews in Mineralogy and Geochemistry, 2004The widespread occurrence of epidote minerals in metamorphic and igneous rocks as well as in many ore deposit types makes it a promising candidate for fluid inclusion studies. Apart from high- to very high-temperature and low- to intermediate-pressure conditions, epidote minerals are stable over a wide range of pressure and temperature in the ...
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Nature, 1960
A NUMBER of silicate minerals have proved difficult to synthesize by the commonly employed methods involving hydrothermal crystallization of glasses or reactive oxide mixes of suitable composition. Failure to synthesize a phase may be caused by the experimental conditions not being within the region where the phase is thermodynamically stable.
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A NUMBER of silicate minerals have proved difficult to synthesize by the commonly employed methods involving hydrothermal crystallization of glasses or reactive oxide mixes of suitable composition. Failure to synthesize a phase may be caused by the experimental conditions not being within the region where the phase is thermodynamically stable.
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Experimental study of epidote dissolution rates from pH 2 to 11 and temperatures from 25 to 200 °C
Geochimica Et Cosmochimica Acta, 2021Eric Oelkers +2 more
exaly