Abstract
Brittle deformation of mineral grains may slip (=fault), separate along either a parallel opening (parallel-pull-apart) or along a v-opening.
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References
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Mukherjee, S. (2013). Pull-Aparts, Boudins and Brittle Faults. In: Deformation Microstructures in Rocks. Springer Geochemistry/Mineralogy. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-25608-0_7
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DOI: https://doi.org/10.1007/978-3-642-25608-0_7
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