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首页|期刊导航|中国地球化学学报(英文版)|The Activity of H2O, Fugacity of O2 and Variation of Their Chemical Potential During Metamorphic Peak of the Granulite Complex Near Taipingzhai-Louzishan Region,East Hebei Province

The Activity of H2O, Fugacity of O2 and Variation of Their Chemical Potential During Metamorphic Peak of the Granulite Complex Near Taipingzhai-Louzishan Region,East Hebei Province

卢良兆 董永胜 周喜文

中国地球化学学报(英文版)2001,Vol.20Issue(2):97-107,11.
中国地球化学学报(英文版)2001,Vol.20Issue(2):97-107,11.

The Activity of H2O, Fugacity of O2 and Variation of Their Chemical Potential During Metamorphic Peak of the Granulite Complex Near Taipingzhai-Louzishan Region,East Hebei Province

The Activity of H2O, Fugacity of O2 and Variation of Their Chemical Potential During Metamorphic Peak of the Granulite Complex Near Taipingzhai-Louzishan Region,East Hebei Province

卢良兆 1董永胜 1周喜文1

作者信息

  • 1. College of Earth Sciences, Jilin University, Changchun 130061, China
  • 折叠

摘要

Abstract

The thermodynamic calculation of dehydration reacton suggests very low activity of H2O during metamorphic peak of the Archaean granulite complex in the region studied. The aH2o values for Al-rich gneiss and hypersthene biotite gneiss-granulite in the Taipingzhai region are usually between 0.10 and 0.20, and those in the Louzishan region are 0.15 - 0.25. The fugacity of O2 in terms of lgfo2 in the whole region ranges from - 8 to - 14. The average co- 1.60 respectively, and those in the Louzishan region are - 0. 364 and - 1. 420. The activity of H2O is very low in the whole region, but its values and other data mentioned above are considerably constant from place to place within a given region, even in rocks of different lithological characters. However, they show a certain gradient between different regions. Such characteristics are compatible with the genetic mechanism known as "carbonic metamorphism" put forward by Newton et al., i. e., the a H2o during the peak stage is controlled by permeation of pervasive CO2 influx of the mantle source, and shows features of external buffering.

关键词

activity of H2O/fugacity of O2/coefficient of chemical potential/granulite facies metamorphism/East Hebei Province

Key words

activity of H2O/fugacity of O2/coefficient of chemical potential/granulite facies metamorphism/East Hebei Province

分类

天文与地球科学

引用本文复制引用

卢良兆,董永胜,周喜文..The Activity of H2O, Fugacity of O2 and Variation of Their Chemical Potential During Metamorphic Peak of the Granulite Complex Near Taipingzhai-Louzishan Region,East Hebei Province[J].中国地球化学学报(英文版),2001,20(2):97-107,11.

基金项目

This research project was financially supported by the National Natural Science Foundation of China (Grant No. 49772144). (Grant No. 49772144)

中国地球化学学报(英文版)

2096-0956

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