High-Pressure Physical and Chemical Behaviors of Minerals and Rocks

The Key Laboratory of High-temperature and High-pressure Study of the Earth's Interior belongs to the Institute of Geochemistry, Chinese Academy of Sciences, China. It is a unique and authoritative key laboratory at the provincial and ministerial levels. The Key High-Pressure Laboratory is prim...

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Other Authors: Dai, Lidong (Editor), Hu, Haiying (Editor), Jiang, Jianjun (Editor)
Format: Electronic Book Chapter
Language:English
Published: Basel MDPI - Multidisciplinary Digital Publishing Institute 2023
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Online Access:DOAB: download the publication
DOAB: description of the publication
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520 |a The Key Laboratory of High-temperature and High-pressure Study of the Earth's Interior belongs to the Institute of Geochemistry, Chinese Academy of Sciences, China. It is a unique and authoritative key laboratory at the provincial and ministerial levels. The Key High-Pressure Laboratory is primarily focused on the high-temperature and high-pressure experimental sciences, in combination with filed geophysical observation, theoretical calculation and advanced analysis tests in order to explore the chemical composition, cycling structure, geological state, material circulation, etc., of deep Earth. The mainstream research subjects of the Laboratory mainly include: research and development of experimental platforms and measurement techniques at high temperatures and high pressures; high-pressure material synthesis and hot-pressed sintering techniques; physical and chemical characterizations (e.g. electrical conductivity, thermal conductivity, ultrasonic wave velocity, etc.) of minerals and rocks at conditions of high pressure and different oxygen fugacities by virtue of representative high-pressure apparatus, including autoclaves, piston cylinders, multi-anvil presses, diamond anvil cells and shock waves; high-pressure physiochemical behavior and storage states in the geological fluid and melt of deep Earth interior; high-pressure theoretical calculations; and high-pressure applications in the service of national economical and societal development. 
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653 |a diopside 
653 |a thermodynamic properties 
653 |a eclogite model 
653 |a adiabatic temperature gradient 
653 |a adiabatic geotherm 
653 |a laser shock compression 
653 |a sound velocity 
653 |a high-pressure 
653 |a quartz 
653 |a Grüneisen parameter 
653 |a super-earth 
653 |a rock porosity 
653 |a high isostatic pressure 
653 |a sample holder 
653 |a sandstone 
653 |a electrical conductivity 
653 |a impedance spectroscopy 
653 |a water 
653 |a titanium-bearing olivine 
653 |a epidote 
653 |a amphibole 
653 |a kaolinite 
653 |a high pressure 
653 |a pyrite 
653 |a Raman spectroscopy 
653 |a high temperature 
653 |a gabbro 
653 |a mineralogical proportions 
653 |a differential stress 
653 |a coesite 
653 |a phase transition 
653 |a calcite 
653 |a crystallinity 
653 |a mineralogy 
653 |a electronic transition 
653 |a hydrothermal 
653 |a trace elements 
653 |a zircon 
653 |a reidite 
653 |a high P-T experiment 
653 |a diamond anvil cell 
653 |a in situ Raman spectroscopy 
653 |a density functional theory 
653 |a phase diagram 
653 |a structural phase transition 
653 |a brucite 
653 |a atomistic simulations 
653 |a high pressures 
653 |a high temperatures 
653 |a structural properties 
653 |a elastic properties 
653 |a bulk modulus 
653 |a vibrational spectra 
653 |a n/a 
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