Articles | Volume 10, issue 1
Solid Earth, 10, 343–356, 2019
https://doi.org/10.5194/se-10-343-2019
Solid Earth, 10, 343–356, 2019
https://doi.org/10.5194/se-10-343-2019
Research article
18 Feb 2019
Research article | 18 Feb 2019

The role of mechanical stratigraphy on the refraction of strike-slip faults

Mirko Carlini et al.

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Cited articles

Agosta, F., Wilson, C., and Aydin, A.: The role of mechanical stratigraphy on normal fault growth across a Cretaceous carbonate multi-layer, central Texas (USA), Ital. J. Geosci., 134, 423–441, https://doi.org/10.3301/IJG.2014.20, 2015. 
Benini, A., Martelli, L., Poccianti, C., Rosselli, S., Benvenuti, M., Catanzariti, R., Giulio, A. Di, Gargini, A., and Fornaciari, E.: Note Illustrative della Carta Geologica d'Italia – foglio 253 Marradi, Regione Emilia Romagna – Servizio Geologico, Sismico e dei Suoli, 2014. 
Bennett, R. A., Serpelloni, E., Hreinsdóttir, S., Brandon, M. T., Buble, G., Basic, T., Casale, G., Cavaliere, A., Anzidei, M., Marjonovic, M., Minelli, G., Molli, G., and Montanari, A.: Syn-convergent extension observed using the RETREAT GPS network, northern Apennines, Italy, J. Geophys. Res., 117, 1–23, https://doi.org/10.1029/2011JB008744, 2012. 
Bettelli, G., Panini, F., Fioroni, C., Nirta, G., Remitti, F., Vannucchi, P., and Carlini, M.: Revisiting the geology of the “Sillaro line”, Northern Apennines, Italy, Rend. Online Soc. Geol. Ital., 22, 14–17, 2012. 
Carlini, M., Artoni, A., Aldega, L., Balestrieri, M. L., Corrado, S., Vescovi, P., Bernini, M., and Torelli, L.: Exhumation and reshaping of far-travelled/allochthonous tectonic units in mountain belts, New insights for the relationships between shortening and coeval extension in the western Northern Apennines (Italy), Tectonophysics, 608, 267–287, https://doi.org/10.1016/j.tecto.2013.09.029, 2013. 
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Short summary
Physical properties of layered sedimentary rocks affect nucleation and propagation of discontinuities therein. Fractures developing through sedimentary sequences characterized by the alternation of strong and weak layers are strongly deviated along their track at layers’ boundaries, and depending on the layer they cross-cut, they show very thick (strong layers) or very thin (weak layers) infills of precipitated minerals, potentially representing pathways for ore deposits and oil/water resources.