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Anisotropic thermal expansion of calcite at high pressures; an in situ X-ray diffraction study in a hydrothermal diamond-anvil cell

Lattice parameters of calcite were measured at simultaneous high P and T at up to 10 kbar and 500°C.

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Published in:The American mineralogist 1995-10, Vol.80 (9-10), p.941-946
Main Authors: Wu, Tzy-Chung, Shen, Andy H, Weathers, Maura S, Bassett, William A, Chou, I-Ming
Format: Article
Language:English
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cited_by cdi_FETCH-LOGICAL-a379t-de7ac3e50442a8ffde3a65b4b0bcdb0f94d2a7a41ab8833c69967dbb5e102dad3
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container_end_page 946
container_issue 9-10
container_start_page 941
container_title The American mineralogist
container_volume 80
creator Wu, Tzy-Chung
Shen, Andy H
Weathers, Maura S
Bassett, William A
Chou, I-Ming
description Lattice parameters of calcite were measured at simultaneous high P and T at up to 10 kbar and 500°C.
doi_str_mv 10.2138/am-1995-9-1010
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ispartof The American mineralogist, 1995-10, Vol.80 (9-10), p.941-946
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source Full-Text Journals in Chemistry (Open access)
subjects anisotropy
anvil cells
Calcite
carbonates
high pressure
hydrothermal conditions
lattice parameters
Mineralogy
Minerals
nonsilicates
physicochemical properties
pressure
Thermal expansion
Thermodynamics
X-ray diffraction
X-ray diffraction data
X-rays
title Anisotropic thermal expansion of calcite at high pressures; an in situ X-ray diffraction study in a hydrothermal diamond-anvil cell
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