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001			313824
003			MX-SnUAN
005			20160429160719.0
007			cr nn 008mamaa
008			150903s2013 ne | o |||| 0|eng d
020			_a9789400755451 _99789400755451
024	7		_a10.1007/9789400755451 _2doi
035			_avtls000367597
039		9	_a201509030716 _bVLOAD _c201405070444 _dVLOAD _y201402251628 _zstaff
040			_aMX-SnUAN _bspa _cMX-SnUAN _erda
050		4	_aQE351-399.2
100	1		_aPaterson, Mervyn S. _eautor _9326954
245	1	0	_aMaterials Science for Structural Geology / _cby Mervyn S. Paterson.
264		1	_aDordrecht : _bSpringer Netherlands : _bImprint: Springer, _c2013.
300			_axiv, 247 páginas 36 ilustraciones _brecurso en línea.
336			_atexto _btxt _2rdacontent
337			_acomputadora _bc _2rdamedia
338			_arecurso en línea _bcr _2rdacarrier
347			_aarchivo de texto _bPDF _2rda
490	0		_aSpringer Geochemistry/Mineralogy, _x2194-3176
500			_aSpringer eBooks
505	0		_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.
520			_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.
590			_aPara consulta fuera de la UANL se requiere clave de acceso remoto.
710	2		_aSpringerLink (Servicio en línea) _9299170
776	0	8	_iEdición impresa: _z9789400755444
856	4	0	_uhttp://remoto.dgb.uanl.mx/login?url=http://dx.doi.org/10.1007/978-94-007-5545-1 _zConectar a Springer E-Books (Para consulta externa se requiere previa autentificación en Biblioteca Digital UANL)
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999			_c313824 _d313824