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估算上地幔温压条件与氧化状态的最新热力学方法
引用本文:马鸿文.估算上地幔温压条件与氧化状态的最新热力学方法[J].地质科技情报,1992,11(2):29-37.
作者姓名:马鸿文
作者单位:中国地质大学 北京100083
摘    要:上地幔的温压条件与氧化状态,对于了解上地幔的热结构、物态与相关系、深部地质作用、特别是岩浆起源及超镁铁岩的成因具有重要的意义。本文概述了近年来新提出的估算尖晶石、石榴石二辉橄榄岩相矿物平衡的温度、压力和氧逸度的热力学方法,对于从事金伯利岩、蛇绿岩和上地幔橄榄岩包体的研究具有重要的实用价值。

关 键 词:上地幔  温压条件  氧化状态  热力学

NEW GEOTHERMOBAROMETERS APPLICABLE TO THE MANTLE ROCKS
Ma Hongwen.NEW GEOTHERMOBAROMETERS APPLICABLE TO THE MANTLE ROCKS[J].Geological Science and Technology Information,1992,11(2):29-37.
Authors:Ma Hongwen
Abstract:During the recent years several series of phase equilibrium experiments on spinel, garnet therzolites have been done to calibrate the geothermobarometers, which are of critical importance for constructing T-p-fo2 regime of the upper mantle, and for understanding the mantle's magmatic processes. This paper gives a review to these thermodynamical methods, with particularly emphases on the T-p-composition limitations of the methods and the petro-genetical interpretations in practical applications.
Keywords:the upper mantle  T-p-fo2 regime  thermodynamical method
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