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Shock compression of liquid silicates to 125 GPa: the anorthitediopside join
 

Summary: Shock compression of liquid silicates to 125 GPa: the
anorthitediopside join
as J. Ahrens Paul D. Asimow and Thom
Division of Geological and Planetary Sciences and
l Geophysics Lindhurst Laboratory of Experimenta
nology
/C 17025
California Institute of Tech
1200 E. California Blvd. M
Pasadena, CA 91125 USA
simow@gps.caltech.eduA
626)3954133, FAX (626)5680935 (

al Research November 17, 2009 Submitted to Journal of Geophysic
evision submitted June 8, 2010 R



Keywords: equation of state, magma, mantle, shock compression, silicate liquids
Index terms: 3944, 3919, 3621, 3619

  

Source: Asimow, Paul D. - Division of Geological and Planetary Sciences, California Institute of Technology,

 

Collections: Geosciences