Thermal equation of state of synthetic orthoferrosilite at lunar pressures and temperatures

J. de Vries; J.M.G. Jacobs; A.P. van den Berg; M. Wehber; C. Lathe; C.A. McCammon; W. van Westrenen

doi:10.1007/s00269-013-0605-5

Thermal equation of state of synthetic orthoferrosilite at lunar pressures and temperatures

J. de Vries, J.M.G. Jacobs, A.P. van den Berg, M. Wehber, C. Lathe, C.A. McCammon, W. van Westrenen

Geology and Geochemistry

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Iron-rich orthopyroxene plays an important role in models of the thermal and magmatic evolution of the Moon, but its density at high pressure and high temperature is not well-constrained. We present in situ measurements of the unit-cell volume of a synthetic polycrystalline end-member orthoferrosilite (FeSiO

Original language	English
Pages (from-to)	691-703
Journal	Physics and Chemistry of Minerals
Issue number	40
DOIs	https://doi.org/10.1007/s00269-013-0605-5
Publication status	Published - 2013

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10.1007/s00269-013-0605-5

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abstract = "Iron-rich orthopyroxene plays an important role in models of the thermal and magmatic evolution of the Moon, but its density at high pressure and high temperature is not well-constrained. We present in situ measurements of the unit-cell volume of a synthetic polycrystalline end-member orthoferrosilite (FeSiO",

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AU - de Vries, J.

AU - Jacobs, J.M.G.

AU - van den Berg, A.P.

AU - Wehber, M.

AU - Lathe, C.

AU - McCammon, C.A.

AU - van Westrenen, W.

PY - 2013

Y1 - 2013

N2 - Iron-rich orthopyroxene plays an important role in models of the thermal and magmatic evolution of the Moon, but its density at high pressure and high temperature is not well-constrained. We present in situ measurements of the unit-cell volume of a synthetic polycrystalline end-member orthoferrosilite (FeSiO

AB - Iron-rich orthopyroxene plays an important role in models of the thermal and magmatic evolution of the Moon, but its density at high pressure and high temperature is not well-constrained. We present in situ measurements of the unit-cell volume of a synthetic polycrystalline end-member orthoferrosilite (FeSiO

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M3 - Article

SN - 0342-1791

SP - 691

EP - 703

JO - Physics and Chemistry of Minerals

JF - Physics and Chemistry of Minerals

IS - 40

ER -

Thermal equation of state of synthetic orthoferrosilite at lunar pressures and temperatures

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