000			03752cam a2200433 i 4500
005			20250918235549.0
008			140626s2013 enkab bi 001 0 eng
020			_a9781107030060 _cRM283.31
020			_a1107030064
039		9	_a201410301518 _blan _y06-26-2014 _zhamudah
040			_aDLC _beng _erda _cDLC _dBTCTA _dUKMGB _dYDXCP _dCDX _dGZM _dIUL _dSTF _dOCLCF _dSHH _dINU _dYBM _dUKM
090			_aQE534.3O533 3
090			_aQE534.3 _bO533 3
100	1		_aOnaka, Michiyasu, _d1940-
245	1	4	_aThe physics of rock failure and earthquakes / _cMitiyasu Ohnaka, The University of Tokyo, Professor Emeritus.
264		1	_aCambridge : _bCambridge University Press, _c2013.
300			_ax, 270 pages : _billustrations, maps ; _c26 cm.
336			_atext _2rdacontent
337			_aunmediated _2rdamedia
338			_avolume _2rdacarrier
504			_aIncludes bibliographical references and index.
505	0		_aIntroduction -- Fundamentals of rock failure physics -- Laboratory-derived constitutive relations for shear failure -- Constitutive laws for earthquake ruptures -- Earthquake generation processes -- Physical scale-dependence -- Large earthquake generation cycles and accompanying seismic activity.
520			_a'Physical modelling of earthquake generation processes is essential to further our understanding of seismic hazard. However, the scale-dependent nature of earthquake rupture processes is further complicated by the heterogeneous nature of the crust. Despite significant advances in the understanding of earthquake generation processes, and the derivation of underlying physical laws, controversy remains regarding what the constitutive law for earthquake ruptures ought to be, and how it should be formulated. It is extremely difficult to obtain field data to define physical properties along a fault during a rupture event, at sufficiently high spatial and temporal resolution to resolve the controversy. Instead, laboratory experiments offer a means of obtaining high-resolution measurements that allow the physical nature of shear rupture processes to be deduced. This important new book is written using consistent notation, providing a deeper understanding of earthquake processes from nucleation to their dynamic propagation. Its key focus is a deductive approach based on laboratory-derived physical laws and formulae, such as a unifying constitutive law, a constitutive scaling law, and a physical model of shear rupture nucleation. Topics covered include: the fundamentals of rock failure physics, earthquake generation processes, physical scale dependence, and large-earthquake generation cycles and their seismic activity'-- _cProvided by publisher.
650		0	_aSeismology.
650		0	_aRock mechanics.
650		0	_aEarthquakes.
856	4	2	_3Contributor biographical information _uhttp://catdir.loc.gov/catdir/enhancements/fy1215/2012035059-b.html.
856	4	2	_3Publisher description _uhttp://catdir.loc.gov/catdir/enhancements/fy1215/2012035059-d.html.
856	4	1	_3Table of contents only _uhttp://catdir.loc.gov/catdir/enhancements/fy1215/2012035059-t.html.
856	4	1	_zAvailable to Stanford-affiliated users. _uhttp://dx.doi.org/10.1017/CBO9781139342865 _yCambridge Books Online
907			_a.b1593651x _b2019-11-12 _c2019-11-12
942			_c01 _n0 _kQE534.3O533 3
914			_avtls003563408
990			_arab
991			_aFakulti Kejuruteraan dan Alam Bina
998			_al _b2014-01-06 _cm _da _feng _genk _y0 _z.b1593651x
999			_c573078 _d573078