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 attenu...

Πλήρης περιγραφή

Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριος συγγραφέας: Chien, Su-Ying (Συγγραφέας)
Συγγραφή απο Οργανισμό/Αρχή: SpringerLink (Online service)
Μορφή: Ηλεκτρονική πηγή Ηλ. βιβλίο
Γλώσσα:English
Έκδοση: Cham : Springer International Publishing : Imprint: Springer, 2014.
Σειρά:Springer Theses, Recognizing Outstanding Ph.D. Research,
Θέματα:
Διαθέσιμο Online:Full Text via HEAL-Link
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100 1 |a Chien, Su-Ying.  |e author. 
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. 
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 
347 |a text file  |b PDF  |2 rda 
490 1 |a Springer Theses, Recognizing Outstanding Ph.D. Research,  |x 2190-5053 
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 Earth sciences. 
650 0 |a Geology  |x Statistical methods. 
650 0 |a Structural geology. 
650 0 |a Geophysics. 
650 0 |a Spectroscopy. 
650 0 |a Microscopy. 
650 0 |a Continuum mechanics. 
650 1 4 |a Earth Sciences. 
650 2 4 |a Structural Geology. 
650 2 4 |a Quantitative Geology. 
650 2 4 |a Spectroscopy and Microscopy. 
650 2 4 |a Continuum Mechanics and Mechanics of Materials. 
650 2 4 |a Geophysics/Geodesy. 
710 2 |a SpringerLink (Online service) 
773 0 |t Springer eBooks 
776 0 8 |i Printed edition:  |z 9783319030975 
830 0 |a Springer Theses, Recognizing Outstanding Ph.D. Research,  |x 2190-5053 
856 4 0 |u http://dx.doi.org/10.1007/978-3-319-03098-2  |z Full Text via HEAL-Link 
912 |a ZDB-2-EES 
950 |a Earth and Environmental Science (Springer-11646)