By Su-Ying Chien

Our realizing of the rheological and seismic houses of the Earth’s inside will depend on studying geophysical observations utilizing mineral physics info. The complexity of common fabrics complicates those interpretations, yet the following the foremost positive factors of such fabrics in controlling the attenuation of seismic waves are made up our minds through a suite of cautious experiments. This thesis sincerely explains how dynamic mechanical spectroscopy has been used to figure out the visco-elastic houses of igneous and sedimentary rocks containing geological fluids. those experiments spotlight, for the 1st time, the significance of mineral and rock microstructures as controls on geophysical homes of solids, fairly close to the melting aspect. the consequences have affects in parts starting from volcanic procedures, throughout the constitution of the deep Earth, to fluid-saturated porous media.

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Rheological and Seismic Properties of Solid-Melt Systems: A Mechanical Spectroscopy Study (Springer Theses) by Su-Ying Chien

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