LEADER 04043nam 2200733 450 001 9910452356203321 005 20200520144314.0 010 $a0-262-29377-3 010 $a1-282-09877-2 010 $a9786612098772 010 $a0-262-27484-1 010 $a1-4294-7713-X 035 $a(CKB)1000000000472982 035 $a(SSID)ssj0000256644 035 $a(PQKBManifestationID)11203973 035 $a(PQKBTitleCode)TC0000256644 035 $a(PQKBWorkID)10224012 035 $a(PQKB)10089609 035 $a(MiAaPQ)EBC3338702 035 $a(CaBNVSL)mat06267398 035 $a(IDAMS)0b000064818b43d6 035 $a(IEEE)6267398 035 $a(OCoLC)144569747$z(OCoLC)646927137$z(OCoLC)648325673$z(OCoLC)764480038$z(OCoLC)815776571$z(OCoLC)961527569$z(OCoLC)962582540$z(OCoLC)988455190$z(OCoLC)991999857$z(OCoLC)992105882$z(OCoLC)1037460712$z(OCoLC)1037917625$z(OCoLC)1038627762$z(OCoLC)1055408084$z(OCoLC)1058145252$z(OCoLC)1066584558$z(OCoLC)1081189257 035 $a(OCoLC-P)144569747 035 $a(MaCbMITP)6703 035 $a(Au-PeEL)EBL3338702 035 $a(CaPaEBR)ebr10190447 035 $a(CaONFJC)MIL209877 035 $a(OCoLC)144569747 035 $a(EXLCZ)991000000000472982 100 $a20151223d2007 uy 101 0 $aeng 135 $aurcn||||||||| 181 $ctxt 182 $cc 183 $acr 200 10$aTectonic faults $eagents of change on a dynamic Earth /$fedited by Mark R. Handy, Greg Hirth, and Niels Hovius 210 1$aCambridge, Massachusetts :$cMIT Press,$dc2007. 210 2$a[Piscataqay, New Jersey] :$cIEEE Xplore,$d[2007] 215 $axiii, 446 p. $cill. (some col.), maps 225 1 $aDahlem workshop reports ;$v95 300 $a"Report of the 95th Dahlem Workshop on the Dynamics of Fault Zones, Berlin, January 16-21, 2005"--P. facing t.p. 300 $aSeries statement from jacket. 311 $a0-262-08362-0 320 $aIncludes bibliographical references and indexes. 330 $aTectonic faults are sites of localized motion, both at the Earth's surface and within its dynamic interior. Faulting is directly linked to a wide range of global phenomena, including long-term climate change and the evolution of hominids, the opening and closure of oceans, and the rise and fall of mountain ranges. In Tectonic Faults, scientists from a variety of disciplines explore the connections between faulting and the processes of the Earth's atmosphere, surface, and interior. They consider faults and faulting from many different vantage points--including those of surface analysts, geochemists, material scientists, and physicists--and in all scales, from seismic fault slip to moving tectonic plates. They address basic issues, including the imaging of faults from Earth's surface to the base of the lithosphere and deeper, the structure and rheology of fault rocks, and the role of fluids and melt on the physical properties of deforming rock. They suggest strategies for understanding the interaction of faulting with topography and climate, predicting fault behavior, and interpreting the impacts on the rock record and the human environment. Using an Earth Systems approach, Tectonic Faults provides a new understanding of feedback between faulting and Earth's atmospheric, surface, and interior processes, and recommends new approaches for advancing knowledge of tectonic faults as an integral part of our dynamic planet. 410 0$aDahlem workshop reports ;$v95 606 $aFaults (Geology)$vCongresses 606 $aGeodynamics$vCongresses 608 $aElectronic books. 615 0$aFaults (Geology) 615 0$aGeodynamics 676 $a551.8/72 701 $aHandy$b Mark R$0857495 701 $aHovius$b Niels$0857496 701 $aHirth$b Greg$0857497 712 12$aDahlem Workshop on the Dynamics of Fault Zones 801 0$bCaBNVSL 801 1$bCaBNVSL 801 2$bCaBNVSL 906 $aBOOK 912 $a9910452356203321 996 $aTectonic faults$91914740 997 $aUNINA