石榴子石族矿物状态方程研究进展
Research Progress of the Equation of State for Garnet Minerals
查看参考文献64篇
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文摘
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石榴子石是重要的造岩矿物,是上地幔、地幔转换带以及(超)高压变质岩中最重要的造岩矿物之一,研究其状态方程对于约束地球内部物质组成和状态、正确理解大洋岩石圈俯冲板块和地幔动力学过程具有重要意义。文中综述了20世纪70年代以来石榴子石p-V(压强-晶胞体积)和p-V-T(压强-晶胞体积-温度)状态方程的研究进展,重点讨论高温高压条件下石榴子石的稳定性以及组分变化和含水对热弹性参数的影响。最后简略概括石榴子石状态方程研究存在的问题,并指出发展方向。 |
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其他语种文摘
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As an important rock-forming mineral of the rocks in the earth,garnet is one of the most important minerals in the upper mantle,transition zone and (ultra) high pressure metamorphic rocks.The study of its equation of state is therefore of great significance in laying a foundation for constraining the state and chemical composition of the earth interiors,and further understanding the geodynamical processes of the subducted oceanic lithosphere plate and Earth's mantle.This article summarized the recent advances in the studies of the p-V (pressure-cell volume) and p-V-T (pressure-cell volume-temperature) equation of state of the garnet,focusing on the phase stability,the effect of component and hydrogen on the thermal elastic parameters of the garnet at high pressure and high temperature.Finally,the existing problems and prospects of the garnet's equation of state studies were also evaluated. |
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来源
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高压物理学报
,2018,32(1):010101-1-010101-13 【核心库】
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DOI
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10.11858/gywlxb.20170597
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关键词
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高温高压
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状态方程
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石榴子石
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上地幔
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过渡带
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地址
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1.
中国科学院地球化学研究所, 中国科学院地球内部物质高温高压重点实验室, 贵州, 贵阳, 550081
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中国科学院大学, 北京, 100049
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贵州建设职业技术学院, 贵州, 贵阳, 551400
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语种
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中文 |
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文献类型
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综述型 |
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ISSN
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1000-5773 |
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学科
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物理学 |
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基金
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中国科学院战略性先导科技专项
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国家自然科学基金
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中国科学院"西部之光"人才培养引进计划"西部青年学者"A类项目
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中国科学院青年创新促进会项目
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文献收藏号
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CSCD:6152137
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