P-V-T equation of state of CaCO 3 aragonite to 29 GPa and 1673 K: In situ X-ray diffraction study-Reference-Cited by-同舟云学术

P-V-T equation of state of CaCO 3 aragonite to 29 GPa and 1673 K: In situ X-ray diffraction study

Published:2017-04 Issue: Volume:265 Page:82-91
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Litasov Konstantin D.,Shatskiy Anton,Gavryushkin Pavel N.,Bekhtenova Altyna E.,Dorogokupets Peter I.,Danilov Boris S.,Higo Yuji,Akilbekov Abdirash T.,Inerbaev Talgat M.

Funder

Russian Science Foundation

Ministry of Education and Science of the Russian Federation

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

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5. Temperature dependence of the structural parameters in the transformation of aragonite to calcite, as determined from in situ synchrotron powder X-ray-diffraction data;Antao;Can. Mineral.,2010

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