PHASE-EQUILIBRIA IN CARBONIC SYSTEMS, AND THEIR APPLICATION TO FREEZING STUDIES OF FLUID INCLUSIONS

被引:139
作者
SWANENBERG, HEC
机构
[1] Geologisch Instituut, Rijksuniversiteit Utrecht, PL Utrecht, 3511
关键词
D O I
10.1007/BF00371552
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Addition of CH4 to CO2 lowers the temperatures at which phase changes occur with respect to those in the unary system CO2. At high density and high {Mathematical expression} a melting interval of solid CO2 can be expected. Rearrangement of currently available theoretical and experimental data permits bulk compositions of carbonic fluid inclusions to be determined from the final melting temperature of CO2 and the degree of filling at that temperature. Homogenization temperatures of CO2-CH4 inclusions can be expressed in terms of equivalent CO2-densities, permitting estimates of P-T relations using isochores in the unary system CO2. © 1979 Springer-Verlag.
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页码:303 / 306
页数:4
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