Velocity crossover between hydrous and anhydrous forsterite at high pressures

Earth and Planetary Science Letters

Volumn 293, Issue 3-4, 2010, Pages 250-258

  Mao, Z ^a   Jacobsen, S D ^b   Jiang, F ^a   Smyth, J R ^c   Holl, C M ^a,b   Frost, D J ^d   Duffy, T S ^a  

^a PRINCETON UNIVERSITY   (United States)

^b NORTHWESTERN UNIVERSITY   (United States)

^c UNIVERSITY OF COLORADO   (United States)

^d UNIVERSITÄT BAYREUTH   (Germany)

Author keywords

Brillouin scattering; Elasticity; Hydrous forsterite; Velocity crossover

Indexed keywords

410-KM DISCONTINUITY; AMBIENT PRESSURES; ANHYDROUS PHASE; AZIMUTHAL ANISOTROPY; BULK MODULUS; COMPRESSIONAL; CURRENT DATA; EARTH'S MANTLE; ELASTIC PROPERTIES; FORSTERITES; FUNCTION OF PRESSURE; HIGH PRESSURE; HYDROUS FORSTERITE; P WAVES; PRESSURE DERIVATIVES; S VELOCITY; S-WAVE SPLITTING; SEISMIC VELOCITIES; SHEAR MODULUS; TEMPERATURE DERIVATIVES; WADSLEYITE;

BRILLOUIN SCATTERING; ELASTIC MODULI; ELASTICITY; FINANCIAL DATA PROCESSING; HYDRATION; SCATTERING; SILICON COMPOUNDS; ULTRASONICS; VELOCITY; WATER CONTENT;

OLIVINE;

ELASTICITY; ESTIMATION METHOD; FORSTERITE; HIGH PRESSURE; HYDRATION; HYDROUS MINERAL; MANTLE STRUCTURE; P-WAVE; S-WAVE; SEISMIC VELOCITY; SPECTROSCOPY; WADSLEYITE;

EID: 77951299310     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2010.02.025     Document Type: Article

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