| 000 | 03033nam a22005295i 4500 | ||
|---|---|---|---|
| 001 | 978-3-319-03098-2 | ||
| 003 | DE-He213 | ||
| 005 | 20140220082512.0 | ||
| 007 | cr nn 008mamaa | ||
| 008 | 131125s2014 gw | s |||| 0|eng d | ||
| 020 |
_a9783319030982 _9978-3-319-03098-2 |
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| 024 | 7 |
_a10.1007/978-3-319-03098-2 _2doi |
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| 050 | 4 | _aQE601-613.5 | |
| 050 | 4 | _aQE500-639.5 | |
| 072 | 7 |
_aRBGD _2bicssc |
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| 072 | 7 |
_aSCI031000 _2bisacsh |
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| 082 | 0 | 4 |
_a551.8 _223 |
| 100 | 1 |
_aChien, Su-Ying. _eauthor. |
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| 245 | 1 | 0 |
_aRheological and Seismic Properties of Solid-Melt Systems _h[electronic resource] : _bA Mechanical Spectroscopy Study / _cby Su-Ying Chien. |
| 264 | 1 |
_aCham : _bSpringer International Publishing : _bImprint: Springer, _c2014. |
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| 300 |
_aXVIII, 159 p. 94 illus., 17 illus. in color. _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 Theses, Recognizing Outstanding Ph.D. Research, _x2190-5053 |
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| 505 | 0 | _aIntroduction -- Experimental methods -- Sample characteristics -- Thermal relaxations in gabbro and basalt -- Glass transition and brittle failure of crystal-glass silicates -- Crackling noise in basalt and gabbro -- Fluid pressure and failure modes of sandstones -- Conclusion. | |
| 520 | _aOur understanding of the rheological and seismic properties of the Earth’s interior relies on interpreting geophysical observations using mineral physics data. The complexity of natural materials complicates these interpretations, but here the key features of such materials in controlling the attenuation of seismic waves are determined by a set of careful experiments. This thesis clearly explains how dynamic mechanical spectroscopy has been used to determine the visco-elastic properties of igneous and sedimentary rocks containing geological fluids. These experiments highlight, for the first time, the importance of mineral and rock microstructures as controls on geophysical properties of solids, particularly near the melting point. The results have impacts in areas ranging from volcanic processes, through the structure of the deep Earth, to fluid-saturated porous media. | ||
| 650 | 0 | _aGeography. | |
| 650 | 0 | _aGeologyxMathematics. | |
| 650 | 0 | _aGeology, Structural. | |
| 650 | 0 | _aPhysical geography. | |
| 650 | 0 | _aMaterials. | |
| 650 | 1 | 4 | _aEarth Sciences. |
| 650 | 2 | 4 | _aStructural Geology. |
| 650 | 2 | 4 | _aQuantitative Geology. |
| 650 | 2 | 4 | _aSpectroscopy and Microscopy. |
| 650 | 2 | 4 | _aContinuum Mechanics and Mechanics of Materials. |
| 650 | 2 | 4 | _aGeophysics/Geodesy. |
| 710 | 2 | _aSpringerLink (Online service) | |
| 773 | 0 | _tSpringer eBooks | |
| 776 | 0 | 8 |
_iPrinted edition: _z9783319030975 |
| 830 | 0 |
_aSpringer Theses, Recognizing Outstanding Ph.D. Research, _x2190-5053 |
|
| 856 | 4 | 0 | _uhttp://dx.doi.org/10.1007/978-3-319-03098-2 |
| 912 | _aZDB-2-EES | ||
| 999 |
_c92957 _d92957 |
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