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Problems of pressure estimation in high temperature experiments using solid media apparatus; pressure calibration with reference to breakdown of albite and quartz-coesite transformation; Part II



Problems of pressure estimation in high temperature experiments using solid media apparatus; pressure calibration with reference to breakdown of albite and quartz-coesite transformation; Part II



Journal of Earth System Science 99(1): 133-140



The high albite (Ab)jadeite (Jd)+quartz(Q) reaction (1) and the quartz(Q)coesite (Cs) transformation (2) have been determined within the temperature range of 1000–1100°C and 1000–1400°C respectively under variable pressures using an anvil-with-hole apparatus. The equilibrium curves for the two reactions as a function ofP andT are as follows:

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Accession: 019800472

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DOI: 10.1007/bf02871901


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