000			02012nam a22004575i 4500
001			u373212
003			SIRSI
005			20160812084135.0
007			cr nn 008mamaa
008			101109s2011 gw | s |||| 0|eng d
020			_a9783540765042 _9978-3-540-76504-2
040			_cMX-MeUAM
050		4	_aQE1-996.5
082	0	4	_a551 _223
100	1		_aFrisch, Wolfgang. _eauthor.
245	1	0	_aPlate Tectonics _h[recurso electrónico] : _bContinental Drift and Mountain Building / _cby Wolfgang Frisch, Martin Meschede, Ronald C. Blakey.
264		1	_aBerlin, Heidelberg : _bSpringer Berlin Heidelberg, _c2011.
300			_aVIII, 212 p. _bonline resource.
336			_atext _btxt _2rdacontent
337			_acomputer _bc _2rdamedia
338			_aonline resource _bcr _2rdacarrier
347			_atext file _bPDF _2rda
520			_aHow are mountains formed? Why are there old and young mountains? Why do the shapes of South America and Africa fit so well together? Why is the Pacific surrounded by a ring of volcanoes and earthquake-prone areas while the edges of the Atlantic are relatively peaceful? Frisch and Meschede and Blakey answer all these questions and more through the presentation and explanation of the geodynamic processes upon which the theory of continental drift is based and which have led to the concept of plate tectonics.
650		0	_aGeography.
650		0	_aGeology.
650		0	_aGeology, Structural.
650		0	_aPlanetology.
650	1	4	_aEarth Sciences.
650	2	4	_aGeology.
650	2	4	_aStructural Geology.
650	2	4	_aPlanetology.
700	1		_aMeschede, Martin. _eauthor.
700	1		_aBlakey, Ronald C. _eauthor.
710	2		_aSpringerLink (Online service)
773	0		_tSpringer eBooks
776	0	8	_iPrinted edition: _z9783540765035
856	4	0	_zLibro electrónico _uhttp://148.231.10.114:2048/login?url=http://link.springer.com/book/10.1007/978-3-540-76504-2
596			_a19
942			_cLIBRO_ELEC
999			_c201092 _d201092