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橄榄石高温高压含水效应与光学性质实验研究
引用本文:顾芷娟,孙天泽,张虹.橄榄石高温高压含水效应与光学性质实验研究[J].地球物理学进展,2000,15(4):36-40.
作者姓名:顾芷娟  孙天泽  张虹
作者单位:1. 中国地震局地质研究所,北京,100029
2. 中国科学院地质与地球物理研究所,北京,100101
基金项目:国家自然科学基金项目 !(4 97742 2 6 )
摘    要:高温高压下橄榄石(多晶)含水效应实验表明,水不但可进入矿物孔隙,且能进入其晶格中。从而与原(干)样相比,橄榄石显示了特有的光学性质和红外吸收谱带,矿物比重也下降约0.02。这些变化可能是上地幔低速层成因的构成因素。

关 键 词:橄榄石  高温高压含水效应  光学性质  矿物孔隙

EXPERINMENT ON AQUIFEROUS EFFECT AND OPTICAL PROPERTY OF OLIVINE UNDER HIGH TEMPERATURE-PRESSURE
GU Zhi-juan,SUN Tian-Ze,ZHANG Hong.EXPERINMENT ON AQUIFEROUS EFFECT AND OPTICAL PROPERTY OF OLIVINE UNDER HIGH TEMPERATURE-PRESSURE[J].Progress in Geophysics,2000,15(4):36-40.
Authors:GU Zhi-juan  SUN Tian-Ze  ZHANG Hong
Abstract:Exprtiment on aquiferous effect of olivine under high temperature pressure indicates that, water not only enters mineral's void but its lattic. Thus, compared with dry sample, the olivine manifested characterstic in respect to optical rroperty and in frared absorption bands, spccific gravity drop off about 0.02. These chang maybe certain reasons for low velocity layer forination in Upper mantle.
Keywords:Olivine  aquiferous effect under high temperature and high pressure  Optical property
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