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Characteristics of deep crustal seismic anisotropy from a compilation of rock elasticity tensors and their expression in receiver functions
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2017
Source: Tectonics, 36(9), 1835-1857
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Journal Title:Tectonics
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Description:Rocks in the continental crust are long lived and have the potential to record a wide span of tectonic history in rock fabric. Mapping rock fabric in situ at depth requires the application of seismic methods. Below depths of microcrack closure seismic anisotropy presumably re flects the shape and crystallographic preferred orientations in fluenced by deformation processes. Interpretation of seismic observables relevant for anisotropy requires assumptions on the symmetry and orientation of the bulk elastic tensor. We compare commonly made assumptions against a compilation of 95 bulk elastic tensors from laboratory measurements, including electron backscatter diffraction and ultrasound, on crustal rocks. Themajority of samples developed fabric at pressures corresponding to middle to lower crustal condition. Tensor
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Source:Tectonics, 36(9), 1835-1857
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ISSN:0278-7407;1944-9194;
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Rights Information:CC BY-NC-ND
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Compliance:Library
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