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• W2049755719 startingPage "277" @default.
• W2049755719 abstract "Seismic reflection profiling across the Central Alps (NFP20) shows strong reflectors, some of which correspond to a Mesozoic marble zone which underlies the contact between the Tambo and Suretta nappes. By means of experimental velocity measurements at confining pressures up to 300 MPa on rock samples collected in the marble zone, we determined the seismic properties of these marbles and calculated their reflection coefficients, in order better to constrain the seismic interpretation. The main findings are as follows: a) Marbles exhibit Vp anisotropy up to 9%, with orthorhombic or transverse isotropic (tetragonal) symmetry due to the crystallographic preferred orientation of calcite. b) Compressional waves, shear waves, and shear wave splitting are very sensitive to the type of fabric (presence or absence of an r-axes concentration). c) Interfaces between marbles and amphibolites or orthogneisses could be good reflectors in normal incidence reflection." @default.
• W2049755719 created "2016-06-24" @default.
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• W2049755719 date "1998-02-01" @default.
• W2049755719 modified "2023-09-26" @default.
• W2049755719 title "Seismic properties of highly strained marbles from the Splügenpass, central Alps" @default.
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• W2049755719 doi "https://doi.org/10.1016/s0191-8141(97)00084-9" @default.
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