Stephen A. Miller

TL;DR: It is proposed that aftershocks of large earthquakes in such geologic environments may be driven by the coseismic release of trapped, high-pressure fluids propagating through damaged zones created by the mainshock, which may provide a link between earthquakes, aftershock, crust/mantle degassing and earthquake-triggered large-scale fluid flow.

TL;DR: In this paper, the authors show that the wide scatter observed for very large mass wasting events in all environments collapses to a single relationship between event volume or inundation area and mobility, and demonstrate that fluidization is associated with long run-out distances, and that the degree of fluidization can be predicted by the volume and physical and topographic parameters of the flow.

TL;DR: In this article, a porosity reduction mechanism is used to drive pore pressure within a fault zone in excess of hydrostatic, which induces slip that may propagate to surrounding cells depending on the local state of stress.

TL;DR: In this article, the authors apply a new analysis technique using earthquake focal mechanisms to infer the 3D fluid pressure field at depth in the source region of the A.D. 2009 L9Aquila earthquake/aftershock sequence.

TL;DR: Time-resolved spectroscopy of three DPP derivatives with phenyl (3,6-diphenylpyrrolo[3,4-c]pyrrole-1,4(2H,5H)-dione, PhDPP) aromatic substituents reveals that efficient SF occurs only in TDPP and PhTDPP, and demonstrates that SF in DPP is highly sensitive to the electronic coupling between adjacent chromophores.