On the Quantitative Evaluation of Metamorphic Fluid Composition: Verification of the Results of Physicochemical Simulations for Water-Mineral-Rock Reactions

被引：1

作者：

Khudolozhkin, V. O. ^{[1
]}

机构：

[1] Russian Acad Sci, Far E Div, Far E Geol Inst, Vladivostok 690022, Russia

来源：

RUSSIAN JOURNAL OF PACIFIC GEOLOGY | 2007年 / 1卷 / 03期

关键词：

solubility; verification; physicochemical simulation; composition of metamorphic fluid;

D O I：

10.1134/S1819714007030086

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

This paper reports the results of a comparison of the qualitative physicochemical simulations (by the Winsel program complex) of the composition of the reacting fluid with experimental data on the water-electrolyte (NaCl, HCl, NaOH, and KOH)-mineral (quartz, corundum, microcline, and plagioclase) system and the water-electrolyte-rock (granite and pelite) system at 400-800 degrees C and 1-10 kbar. Constraints are proposed for the temperature, pressure, and the composition of the electrolyte at which the simulation results are consistent with the experimental data.

引用

页码：290 / 301

页数：12