Experimental study of \(T - X_{CO_2 } \)boundaries of metamorphic zeolite facies
作者： I. P. Ivanov , L. P. Gurevich
DOI: 10.1007/BF00402454
关键词:
摘要: The \(T - X_{CO_2 } \) conditions of reactions: Lom = Pr + Mont Qz H2O and CO2=Ca limiting the laumontite stability field that represents zeolite facies regional metamorphism have been experimentally studied at Ps=1000 bars. has confirmed very low carbon dioxide contents in solution. boundaries metamorphic were thermodynamically found to be (to a first approximation): temperature range ∼200–270 ° C, maximum total pressure (Ps) up 2500 bars, 40
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