Titlebook: Amphiboles; Crystal Chemistry Ph W. G. Ernst Book 1968 Springer-Verlag New York Inc. 1968 Substitution.chemistry.classification.mineral.min

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書目名稱Amphiboles影響因子(影響力)




書目名稱Amphiboles影響因子(影響力)學(xué)科排名




書目名稱Amphiboles網(wǎng)絡(luò)公開度




書目名稱Amphiboles網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Amphiboles被引頻次




書目名稱Amphiboles被引頻次學(xué)科排名




書目名稱Amphiboles年度引用




書目名稱Amphiboles年度引用學(xué)科排名




書目名稱Amphiboles讀者反饋




書目名稱Amphiboles讀者反饋學(xué)科排名

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Hydrothermal Phase Equilibration and Natural Stability,ters will summarize experimentally determined stability relationships involving double-chain silicates; an attempt also will be made to apply these data to appropriate natural occurrences. Hydrothermal methods and equilibration techniques are discussed briefly in this section, as well as disparities

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Experimental Phase Relations and Occurrence of the Iron-Magnesium Amphiboles, these authors were unable to demonstrate a stability field for anthophyllite and suggested that its production might depend on the absence of H.O-rich fluid. Y. (1952) experienced similar results in his investigation of the system MgO-Al.O.-SiO.-H.O, and advanced the concept of the “water deficient

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Experimental Phase Relations and Occurrence of the Calcic Amphiboles,ns, P. = P.. The starting material in this study consisted of roughly equal proportions of synthetic tremolite and the synthetic high temperature assemblage of equivalent bulk composition, enstatite + diopside + quartz + fluid; stability fields were deduced on the basis of recognizing the contrastin

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Book 1968, published by Springer-Verlag. The voluminous results arising from recent progress in pure and applied re- search increase the need for authoritative reviews but the standard scientific journals are unable to provide the space for them. By their very nature, text-books are unable to consider specif

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https://doi.org/10.1007/978-3-642-91674-8d En.Di._.. B. 1959 paper was the first to provide experimental P-T diagrams involving synthetic amphibole equilibria. Tremolite is stable up to surprisingly high temperatures, 835° C at 1000 bars fluid pressure, but substitution of Fe. for Mg lowers the maximum thermal stability as shown by later studies.