LEADER 03251nam 2200625Ia 450 001 9910437793703321 005 20200520144314.0 010 $a1-283-91086-1 010 $a94-007-5545-7 024 7 $a10.1007/978-94-007-5545-1 035 $a(CKB)2670000000309538 035 $a(EBL)1083586 035 $a(OCoLC)822029243 035 $a(SSID)ssj0000811364 035 $a(PQKBManifestationID)11442091 035 $a(PQKBTitleCode)TC0000811364 035 $a(PQKBWorkID)10847203 035 $a(PQKB)10508593 035 $a(DE-He213)978-94-007-5545-1 035 $a(MiAaPQ)EBC1083586 035 $a(PPN)168341212 035 $a(EXLCZ)992670000000309538 100 $a20121219d2013 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 10$aMaterials science for structural geology /$fMervyn S. Paterson 205 $a1st ed. 2013. 210 $aDordrecht ;$aNew York $cSpringer$dc2013 215 $a1 online resource (254 p.) 225 1 $aSpringer geochemistry/mineralogy 300 $aDescription based upon print version of record. 311 $a94-017-8300-4 311 $a94-007-5544-9 320 $aIncludes bibliographical references and index. 327 $aFrom the Contents: The Nature of Rocks and Minerals as Materials -- Thermodynamics -- Rate Processes -- Mechanical Fundamentals ? Macroscopic -- Deformation Mechanisms - Atomic Transfer Flow -- Deformation Mechanisms - Crystal Plasticity -- Deformation Mechanisms - Granular Flow. 330 $aThis book sets out the basic materials science needed for understanding the plastic deformation of rocks and minerals.  Although at atmospheric pressure or at relatively low environmental pressures, these materials tend to be brittle, that is, to fracture with little prior plastic deformation when non-hydrostatically stressed, they can undergo substantial permanent strain when stressed under environmental conditions of high confining pressure and high temperature, such as occur geologically in the Earth?s crust and upper mantle.  Thus the plastic deformation of rocks and minerals is of fundamental interest in structural geology and geodynamics.  In mountain-building processes and during convective stirring in the Earth?s mantle, rocks can undergo very large amounts of plastic flow, accompanied by substantial changes in microstructure.  These changes in microstructure remain in the rocks as evidence of the past deformation history.  There are a number of types of physical processes whereby rock and minerals can undergo deformation under geological conditions.  The physics of these processes is set out in this book. 410 0$aSpringer geochemistry/mineralogy. 606 $aGeology, Structural 606 $aMaterials science 606 $aCrystals$xPlastic properties 615 0$aGeology, Structural. 615 0$aMaterials science. 615 0$aCrystals$xPlastic properties. 676 $a550.24624 700 $aPaterson$b M. S$01755457 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910437793703321 996 $aMaterials science for structural geology$94192237 997 $aUNINA