00875nam0 22002411i 450 UON0000701120231205101915.56520020107d1963 |0itac50 baurdPK|||| 1||||Sa'er-e InsaniyatMir'Abdu'l-Samad XanPesawarManzur-e'am Kutubxana1963391 p.23 cmLETTERATURA PASHTOCRITICAUONC001992FIAFG VIAFGHANISTAN - LETTERATURAAXANMir Abdu'l SamadUONV0057550ITSOL20240220RICASIBA - SISTEMA BIBLIOTECARIO DI ATENEOUONSIUON00007011SIBA - SISTEMA BIBLIOTECARIO DI ATENEOSI AFG VI 031 N SI SA 73403 5 031 N Sa'er-e Insaniyat1176303UNIOR03251nam 2200625Ia 450 991043779370332120200520144314.01-283-91086-194-007-5545-710.1007/978-94-007-5545-1(CKB)2670000000309538(EBL)1083586(OCoLC)822029243(SSID)ssj0000811364(PQKBManifestationID)11442091(PQKBTitleCode)TC0000811364(PQKBWorkID)10847203(PQKB)10508593(DE-He213)978-94-007-5545-1(MiAaPQ)EBC1083586(PPN)168341212(EXLCZ)99267000000030953820121219d2013 uy 0engur|n|---|||||txtccrMaterials science for structural geology /Mervyn S. Paterson1st ed. 2013.Dordrecht ;New York Springerc20131 online resource (254 p.)Springer geochemistry/mineralogyDescription based upon print version of record.94-017-8300-4 94-007-5544-9 Includes bibliographical references and index.From 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.This 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.Springer geochemistry/mineralogy.Geology, StructuralMaterials scienceCrystalsPlastic propertiesGeology, Structural.Materials science.CrystalsPlastic properties.550.24624Paterson M. S1755457MiAaPQMiAaPQMiAaPQBOOK9910437793703321Materials science for structural geology4192237UNINA01138nam0 22002891i 450 UON0028790620231205103908.92806-911227-5-X20070208d2006 |0itac50 baengGB|||| |||||Making war and building peaceUnited Nations peace operationsMichael W.Doyle and Nicholas SambanisPrincetonOxfordPrinceton University Press2006XVI, 400 p.23 cm.OnuControlloConflittiUONC034410FIGBOxfordUONL000029USPrincetonUONL000074DoyleMichael W.UONV12569166351SAMBANISNicholasUONV168248693714Princeton University PressUONV245813650ITSOL20250718RICASIBA - SISTEMA BIBLIOTECARIO DI ATENEOUONSIUON00287906SIBA - SISTEMA BIBLIOTECARIO DI ATENEOSI PUB 2.0 0116 SI SC 42367 5 0116 BuonoMaking war and building peace1250044UNIOR