The April 2017 Mw 6.5 Botswana Earthquake: An Intraplate Event Triggered by Deep Fluids

@article{Gardonio2018TheA2,
  title={The April 2017 Mw
6.5 Botswana Earthquake: An Intraplate Event Triggered by Deep Fluids},
  author={B. Gardonio and Romain Jolivet and {\'E}ric Calais and Henri Lecl{\`e}re},
  journal={Geophysical Research Letters},
  year={2018}
}
Large earthquakes in stable continental regions remain puzzling as; unlike at plate boundaries, they do not result from the local buildup of strain driven by plate tectonics. The 2017 Mw6.5, Bostwana normal faulting earthquake occurred in a region devoid from recent tectonic activity and where present-day deformation is negligible. The depth of the event (29 ± 4 km), in a felsic lower crust where ductile deformation is expected, likely requires a transient pulse of fluids from a deep source to… 

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