Rheological and Seismic Properties of Solid-Melt Systems A Mechanical Spectroscopy Study /

Our 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 a...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Chien, Su-Ying (Autor)
Autor Corporativo: SpringerLink (Online service)
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Cham : Springer International Publishing : Imprint: Springer, 2014.
Edición:1st ed. 2014.
Colección:Springer Theses, Recognizing Outstanding Ph.D. Research,
Temas:
Geology.
Spectrum analysis.
Mechanics, Applied.
Solids.
Geophysics.
Spectroscopy.
Solid Mechanics.
Acceso en línea:Texto Completo

MARC

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100 1 |a Chien, Su-Ying.  |e author.  |4 aut  |4 http://id.loc.gov/vocabulary/relators/aut 
245 1 0 |a Rheological and Seismic Properties of Solid-Melt Systems  |h [electronic resource] :  |b A Mechanical Spectroscopy Study /  |c by Su-Ying Chien. 
250 |a 1st ed. 2014. 
264 1 |a Cham :  |b Springer International Publishing :  |b Imprint: Springer,  |c 2014. 
300 |a XVIII, 159 p. 94 illus., 17 illus. in color.  |b online resource. 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
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490 1 |a Springer Theses, Recognizing Outstanding Ph.D. Research,  |x 2190-5061 
505 0 |a Introduction -- 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 |a Our 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 |a Geology. 
650 0 |a Spectrum analysis. 
650 0 |a Mechanics, Applied. 
650 0 |a Solids. 
650 0 |a Geophysics. 
650 1 4 |a Geology. 
650 2 4 |a Spectroscopy. 
650 2 4 |a Solid Mechanics. 
650 2 4 |a Geophysics. 
710 2 |a SpringerLink (Online service) 
773 0 |t Springer Nature eBook 
776 0 8 |i Printed edition:  |z 9783319030999 
776 0 8 |i Printed edition:  |z 9783319030975 
776 0 8 |i Printed edition:  |z 9783319380636 
830 0 |a Springer Theses, Recognizing Outstanding Ph.D. Research,  |x 2190-5061 
856 4 0 |u https://doi.uam.elogim.com/10.1007/978-3-319-03098-2  |z Texto Completo 
912 |a ZDB-2-EES 
912 |a ZDB-2-SXEE 
950 |a Earth and Environmental Science (SpringerNature-11646) 
950 |a Earth and Environmental Science (R0) (SpringerNature-43711) 

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