LEADER 02324nam 2200565 a 450 001 9910139039203321 005 20200520144314.0 010 $a1-118-52951-0 010 $a1-78539-375-8 010 $a1-118-52949-9 010 $a1-299-40224-0 010 $a1-118-52952-9 035 $a(CKB)2550000001017841 035 $a(EBL)1160767 035 $a(OCoLC)836405255 035 $a(MiAaPQ)EBC1160767 035 $a(DLC) 2013006464 035 $a(Au-PeEL)EBL1160767 035 $a(CaPaEBR)ebr10680768 035 $a(CaONFJC)MIL471474 035 $a(PPN)183764889 035 $a(EXLCZ)992550000001017841 100 $a20130213d2013 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $2rdacontent 182 $2rdamedia 183 $2rdacarrier 200 00$aPhysics and chemistry of the deep Earth$b[electronic resource] /$fedited by Shun-Ichiro Karato 210 $aHoboken, N.J. $cJohn Wiley & Sons Inc.$d2013 215 $a1 online resource (807 p.) 300 $aDescription based upon print version of record. 311 $a0-470-65914-9 320 $aIncludes bibliographical references and index. 327 $apt. 1. Materials' properties -- pt. 2. Compositional models -- pt. 3. Geophysical observations and models of material circulation. 330 $aThough the deep interior of the Earth (and other terrestrial planets) is inaccessible to humans, we are able to combine observational, experimental and computational (theoretical) studies to begin to understand the role of the deep Earth in the dynamics and evolution of the planet. This book brings together a series of reviews of key areas in this important and vibrant field of studies. A range of material properties, including phase transformations and rheological properties, influences the way in which material is circulated within the planet. This circulation re-distributes key mat 606 $aGeophysics 606 $aGeochemistry 607 $aEarth$xCore 615 0$aGeophysics. 615 0$aGeochemistry. 676 $a551.1/2 701 $aKarato$b Shun'ichiro?$f1949-$0770827 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910139039203321 996 $aPhysics and chemistry of the deep Earth$92010288 997 $aUNINA