000			01100cam a2200277 a 4500
999			_c2931
001			16714803
003			EC-UrYT
005			20180309151431.0
006			s||||gr|||| 00| 00
008			110331s2012 enka b 001 0 eng
010			_a 2011012030
020			_a9781444338867 (cloth)
020			_a9781444338874 (pbk.)
040			_aDLC _cDLC _dDLC
041			_aeng
050	0	0	_aGB401.5 _b.B86 2012
082	0	4	_a551.41 _223
100	1		_aBurbank, Douglas W. _96746 _q(Douglas West).
245	1	0	_aTectonic geomorphology / _cDouglas W. Burbank and Robert S. Anderson.
250			_aSecond Edition
264	3	4	_aChichester, West Sussex ; _aHoboken, N.J. : _bJ. Wiley & Sons, _c2012.
300			_axiv, 454 pages : _billustrations ; _c25 cm.
504			_aIncludes bibliographical references and index.
505	2		_a1. Introduction to tectonic geomorphology -- 2. Geomorphic markers -- 3. Establishing timing in the landscape: dating methods -- 4. Stress, faults, and folds -- 5. Short-term deformation: geodesy -- 6. Paleoseismology: ruptures and slip rates -- 7. Rates of erosion and uplift -- 8. Holocene deformation and landscape responses -- 9. Deformation and geomorphology at intermediate time scales -- 10. Tectonic geomorphology at late Cenozoic time scales -- 11. Numerical modeling of landscape evolution.
520	3		_a"Tectonic geomorphology is the study of the interplay between tectonic and surface processes that shape the landscape in regions of active deformation and at time scales ranging from days to millions of years. Over the past decade, recent advances in the quantification of both rates and the physical basis of tectonic and surface processes have underpinned an explosion of new research in the field of tectonic geomorphology. Modern tectonic geomorphology is an exceptionally integrative field that utilizes techniques and data derived from studies of geomorphology, seismology, geochronology, structure, geodesy, stratigraphy, meteorology and Quaternary science. While integrating new insights and highlighting controversies from the ten years of research since the 1st edition, this 2nd edition of Tectonic Geomorphology reviews the fundamentals of the subject, including the nature of faulting and folding, the creation and use of geomorphic markers for tracing deformation, chronological techniques that are used to date events and quantify rates, geodetic techniques for defining recent deformation, and paleoseismologic approaches to calibrate past deformation"--Provided by publisher.
650	2	4	_aGeomorphology _96745
650	2	4	_aGeology, Structural. _96032
650	2	4	_aMorphotectonics _96747
650	2	4	_aGeomorfología _96744
650	2	4	_aGeología estructural _96033
650	2	4	_aMorfotectónica _96748
700	1		_aAnderson, Robert S. _q(Robert Stewart), _d1952- _96749 _eautor
906			_a7 _bcbc _corignew _d1 _eecip _f20 _gy-gencatlg
942			_2ddc _cLIBRO
955			_bre04 2011-03-31 _ire04 2011-03-31 _axn02 2012-03-21 1 copy rec'd., to CIP ver.