Journal
AMERICAN MINERALOGIST
Volume 95, Issue 1, Pages 144-147Publisher
MINERALOGICAL SOC AMER
DOI: 10.2138/am.2010.3143
Keywords
X-ray absorption method; peridotite melt; density; high pressure; equation of state
Categories
Funding
- Ministry of Education, Culture, Sports, Science, and Technology of the Japanese Government [16340164, 13440163, 16340170]
- Japan Society for the Promotion of Science
Ask authors/readers for more resources
The density of a peridotite magma was measured up to 2.5 GPa and 2300 K using an X-ray absorption method. The method allowed measurement of the density of a peridotite melt under seven different conditions and clarified the pressure and temperature dependence of the density. A fit of the pressure-density-temperature data to the high-temperature Birch-Mumaghan equation of state yielded the isothermal bulk modulus, K(T0) = 24.0 +/- 1.3 GPa. its pressure derivative, K(0)' = 7.3 +/- 0.8, and the derivative of bulk modulus (partial derivative K(T)/partial derivative T)(P) = -0.0027 +/- 0.0017 GPa/K at 2100 K. The large bulk modulus and its pressure derivative of the peridotite melt compared with that of basaltic melt is consistent with previous results from sink-float experiments.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available