Your OP addressed the unusual nature of the Reno area fault (deep hypocenter). Now the LA Times is reporting on a swarm of shallow quakes.
As you know, the Basin & Range is an extensional province, caused, I believe, from the effects of the shallow subduction of the Farallon plate. Extensional block faulting tends to run from shallow to moderately deep, does it not?
What's your take on this?
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