LEADER 04634nam 2200673 450 001 9910777006903321 005 20200520144314.0 010 $a0-231-50189-7 024 7 $a10.7312/karn12738 035 $a(CKB)1000000000445317 035 $a(SSID)ssj0000237947 035 $a(PQKBManifestationID)11213555 035 $a(PQKBTitleCode)TC0000237947 035 $a(PQKBWorkID)10222426 035 $a(PQKB)11042991 035 $a(MiAaPQ)EBC909214 035 $a(DE-B1597)458987 035 $a(OCoLC)60883152 035 $a(OCoLC)979752781 035 $a(DE-B1597)9780231501897 035 $a(Au-PeEL)EBL909214 035 $a(CaPaEBR)ebr11092216 035 $a(CaONFJC)MIL820206 035 $a(OCoLC)922903982 035 $a(EXLCZ)991000000000445317 100 $a20150907h20042004 uy 0 101 0 $aeng 135 $aurcnu|||||||| 181 $ctxt 182 $cc 183 $acr 200 00$aRheology and deformation of the lithosphere at continental margins /$fedited by Garry D. Karner [and three others] ; contributors, Dr. Gary Axen [and twenty one others] 210 1$aNew York :$cColumbia University Press,$d2004. 210 4$d©2004 215 $a1 online resource (367 pages) $cillustrations (some color), maps 225 1 $aMARGINS Theoretical and Experimental Earth Science Series 300 $aBibliographic Level Mode of Issuance: Monograph 311 $a0-231-12739-1 311 $a0-231-12738-3 320 $aIncludes bibliographical references at the end of each chapters and index. 327 $tFrontmatter -- $tContents -- $tContributors -- $tPreface -- $t1. Consequences of Asthenospheric Variability on Continental Rifting / $rBuck, W. Roger -- $t2. Velocity Fields, Faulting, and Strength on the Continents / $rJackson, James -- $t3. Mechanics of Low-Angle Normal Faults / $rAxen, Gary J. -- $t4. Depth-Dependent Lithospheric Stretching at Rifted Continental Margins / $rDavis, Mark / Kusznir, Nick -- $t5. Limits of the Seismogenic Zone / $rRuff, Larry J. -- $t6. Controls on Subduction Thrust Earthquakes: Downdip Changes in Composition and State / $rHyndman, R. D. -- $t7. Thermo-Mechanical Models of Convergent Orogenesis: Thermal and Rheologic Dependence of Crustal Deformation / $rWillett, Sean D. / Pope, Daniel C. -- $t8. Structure of Large-Displacement, Strike-Slip Fault Zones in the Brittle Continental Crust / $rChester, F. M. / Chester, J. S. / Kirschner, D. L. / Schulz, S. E. / Evans, J.P. -- $t9. The Strength of the San Andreas Fault: A Discussion / $rScholz, Christopher H. / Hanks, Thomas C. -- $t10. Deformation Behavior of Partially Molten Mantle Rocks / $rXu, Yaqin / Zimmerman, M. E. / Kohlstedt, D. L. -- $t11. Relations Among Porosity, Permeability, and Deformation in Rocks at High Temperatures / $rEvans, Brian / Bernabé, Yves / Hirth, Greg -- $tIndex 330 $aTraditionally, investigations of the rheology and deformation of the lithosphere (the rigid or mechanically strong outer layer of the Earth, which contains the crust and the uppermost part of the mantle) have taken place at one scale in the laboratory and at an entirely different scale in the field. Laboratory experiments are generally restricted to centimeter-sized samples and day- or year-length times, while geological processes occur over tens to hundreds of kilometers and millions of years. The application of laboratory results to geological systems necessitates extensive extrapolation in both temporal and spatial scales, as well as a detailed understanding of the dominant physical mechanisms. The development of an understanding of large-scale processes requires an integrated approach. This book explores the current cutting-edge interdisciplinary research in lithospheric rheology and provides a broad summary of the rheology and deformation of the continental lithosphere in both extensional and compressional settings. Individual chapters explore contemporary research resulting from laboratory, observational, and theoretical experiments. 410 0$aMARGINS theoretical and experimental earth science series. 606 $aRock deformation 606 $aContinental margins 607 $aEarth (Planet)$xCrust 607 $aEarth (Planet)$xMantle 615 0$aRock deformation. 615 0$aContinental margins. 676 $a551.8 702 $aKarner$b Garry D.$f1953- 702 $aAxen$b Gary 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910777006903321 996 $aRheology and deformation of the lithosphere at continental margins$93696485 997 $aUNINA