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Feb 18, 2021

Jun 14, 2019 Measureable permanent ground displacements are produced by shallow earthquakes of magnitude 5 and greater. These displacements are used by seismologists to understand the earthquake source in detail.Past earthquakes have shown that the amplification of motions due to surface-to-bedrock geology, 3D crustal structure, and topography have a major influence on seismic damage and loss in

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    rock - rock - Thermal properties: Heat flow (or flux), q, in the Earth’s crust or in rock as a building material, is the product of the temperature gradient (change in temperature per unit distance) and the material’s thermal conductivity (k, the heat flow across a surface per unit area per unit time when a temperature difference exists in unit length perpendicular to the surface)

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