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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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Mirko Carlini on behalf of the Authors (22 Jan 2019)  Author's response    Manuscript
ED: Publish as is (25 Jan 2019) by Mark Allen
ED: Publish as is (25 Jan 2019) by Federico Rossetti(Executive Editor)
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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.