000 | 02760nam a2200361Ki 4500 | ||
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001 | ocn842932586 | ||
003 | OCoLC | ||
005 | 20240726105341.0 | ||
008 | 130514s2013 enk ob 001 0 eng d | ||
040 |
_aNT _beng _erda _cNT |
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020 |
_a9781107341968 _q((electronic)l(electronic)ctronic)l((electronic)l(electronic)ctronic)ctronic bk. |
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050 | 0 | 4 |
_aQE534 _b.P497 2013 |
049 | _aNTA | ||
100 | 1 |
_aŌnaka, Michiyasu, _d1940- _e1 |
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245 | 1 | 0 | _aThe physics of rock failure and earthquakesMitiyasu Ohnaka. |
260 |
_aCambridge : _bCambridge University Press, _c(c)2013. |
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300 | _a1 online resource (pages cm.) | ||
336 |
_atext _btxt _2rdacontent |
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337 |
_acomputer _bc _2rdamedia |
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338 |
_aonline resource _bcr _2rdacarrier |
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347 |
_adata file _2rda |
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520 | 0 |
_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. |
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504 | _a2 | ||
530 |
_a2 _ub |
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650 | 0 | _aSeismology. | |
650 | 0 | _aRock mechanics. | |
650 | 0 | _aEarthquakes. | |
655 | 1 | _aElectronic Books. | |
856 | 4 | 0 |
_uhttps://search.ebscohost.com/login.aspx?direct=true&scope=site&db=nlebk&db=nlabk&AN=545024&site=eds-live&custid=s3260518 _zClick to access digital title | log in using your CIU ID number and my.ciu.edu password |
942 |
_cOB _D _eEB _hQE. _m2013 _QOL _R _x _8NFIC _2LOC |
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994 |
_a02 _bNT |
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999 |
_c97490 _d97490 |
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902 |
_a1 _bCynthia Snell _c1 _dCynthia Snell |