Crystallographic preferred orientation, seismic velocity and anisotropy in roofing slates-Reference-Cited by-同舟云学术

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Crystallographic preferred orientation, seismic velocity and anisotropy in roofing slates

Published:2021-06 Issue: Volume:808 Page:228815
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Cardenes Víctor,Lopez-Sanchez Marco A.,Barou Fabrice,Olona Javier,Llana-Fúnez Sergio

Funder

Government of Principality of Asturias

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference66 articles.

1. Upper-crustal seismic anisotropy in the Cantabrian mountains (North Spain) from shear-wave splitting and ambient noise interferometry analysis;Acevedo;Seismol. Res. Lett.,2020

2. Multiscale porosity changes along the pro- and retrograde deformation path: an example from Alpine slates;Akker;Solid Earth,2018

3. Seismic properties and anisotropy of the continental crust: predictions based on mineral texture and rock microstructure;Almqvist;Rev. Geophys.,2017

4. Strength evolution and the development of crystallographic preferred orientation during deformation of two-phase marbles;Austin;Tectonophysics,2014

5. Folding in orogens: a case study in the northern Iberian Variscan Belt;Bastida;Geol. J.,2010

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1. Gondwana platform paleoenvironment reconstruction: Insights from Ordovician black-grey shales in NW Iberia;2024-05-15

2. Los discos de Pizarra de Teotihuacán: caracterización y procedencia de la materia prima;Ancient Mesoamerica;2023-09-14

3. Crystallographic and shape preferred orientation producing anisotropy in slates from Northern Spain;Journal of Structural Geology;2022-11

4. Experimental modelling of primary migration in a layered, brittle analogue system;Tectonophysics;2022-10

5. Radial anisotropy and S-wave velocity depict the internal to external zone transition within the Variscan orogen (NW Iberia);Solid Earth;2022-03-21

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