| 000 | 02957nam a22004815i 4500 | ||
|---|---|---|---|
| 001 | 978-94-007-5545-1 | ||
| 003 | DE-He213 | ||
| 005 | 20140220082938.0 | ||
| 007 | cr nn 008mamaa | ||
| 008 | 121205s2013 ne | s |||| 0|eng d | ||
| 020 |
_a9789400755451 _9978-94-007-5545-1 |
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| 024 | 7 |
_a10.1007/978-94-007-5545-1 _2doi |
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| 050 | 4 | _aQE351-399.2 | |
| 072 | 7 |
_aPNV _2bicssc |
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| 072 | 7 |
_aSCI048000 _2bisacsh |
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| 082 | 0 | 4 |
_a549 _223 |
| 100 | 1 |
_aPaterson, Mervyn S. _eauthor. |
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| 245 | 1 | 0 |
_aMaterials Science for Structural Geology _h[electronic resource] / _cby Mervyn S. Paterson. |
| 264 | 1 |
_aDordrecht : _bSpringer Netherlands : _bImprint: Springer, _c2013. |
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| 300 |
_aXIV, 247 p. 36 illus. _bonline resource. |
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| 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 |
_atext file _bPDF _2rda |
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| 490 | 1 |
_aSpringer Geochemistry/Mineralogy, _x2194-3176 |
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| 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. | ||
| 650 | 0 | _aGeography. | |
| 650 | 0 | _aGeology. | |
| 650 | 0 | _aMineralogy. | |
| 650 | 0 | _aThermodynamics. | |
| 650 | 1 | 4 | _aEarth Sciences. |
| 650 | 2 | 4 | _aMineralogy. |
| 650 | 2 | 4 | _aGeology. |
| 650 | 2 | 4 | _aThermodynamics. |
| 710 | 2 | _aSpringerLink (Online service) | |
| 773 | 0 | _tSpringer eBooks | |
| 776 | 0 | 8 |
_iPrinted edition: _z9789400755444 |
| 830 | 0 |
_aSpringer Geochemistry/Mineralogy, _x2194-3176 |
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| 856 | 4 | 0 | _uhttp://dx.doi.org/10.1007/978-94-007-5545-1 |
| 912 | _aZDB-2-EES | ||
| 999 |
_c99651 _d99651 |
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