高压物理学报2018，Vol.32Issue(1)：1-13,13.DOI:10.11858/gywlxb.20170597
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
摘要
Abstract
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.关键词
高温高压/状态方程/石榴子石/上地幔/过渡带Key words
high-pressure and high-temperature/equation of state/garnet/upper mantle/transition zone分类
数理科学引用本文复制引用
范大伟,李博,陈伟,许金贵,匡云倩,叶之琳,周文戈,谢鸿森..石榴子石族矿物状态方程研究进展[J].高压物理学报,2018,32(1):1-13,13.基金项目
中国科学院战略性先导科技专项(B类)(XDB18010401) （B类）
国家自然科学基金(41274105,41374107,U1632112) （41274105,41374107,U1632112）
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 （）
中国科学院青年创新促进会专项基金 （）
