Übersicht			Auf mobile öffnen

Lieferstatus:	i.d.R. innert 5-10 Tagen versandfertig
Veröffentlichung:	September 2016
Genre:	Naturwissensch., Medizin, Technik
	B / Earth and Environmental Science / Earth Sciences / Geology, geomorphology & the lithosphere / Geology—Statistical methods / Geophysics / Geophysics/Geodesy / Mechanics / Mechanics of solids / Mechanics, Applied / Microscopy / Quantitative Geology / Scientific equipment, experiments & techniques / Solid Earth Sciences / Solid Mechanics / spectroscopy / Spectroscopy and Microscopy / Spectrum analysis, spectrochemistry, mass spectrometry / Structural Geology
ISBN:	9783319380636
EAN-Code:	9783319380636
Verlag:	Springer International Publishing
Einband:	Kartoniert
Sprache:	English
Serie:	Springer Theses
Dimensionen:	H 235 mm / B 155 mm / D 11 mm
Gewicht:	283 gr
Seiten:	180
Zus. Info:	Paperback
Bewertung:	Titel bewerten / Meinung schreiben

Inhalt:

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.