Frictional instabilities in clay illuminate the origin of slow earthquakes.

The shallowest regions of subduction megathrusts mainly deform aseismically, but they can sporadically host slow-slip events (SSEs) and tsunami earthquakes, thus representing a severe hazard. However, the mechanisms behind these remain enigmatic because the frictional properties of shallow subduction zones, usually rich in clay, do not allow earthquake slip according to standard friction theory. We present experimental data showing that clay-rich faults with bulk rate-strengthening behavior and null healing rate, typically associated with aseismic creep, can contemporaneously creep and nucleate SSE.

The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults.

Many rock deformation experiments used to characterize the frictional properties of tectonic faults are performed on powdered fault rocks or on bare rock surfaces. These experiments have been fundamental to document the frictional properties of granular mineral phases and provide evidence for crustal faults characterized by high friction. However, they cannot entirely capture the frictional properties of faults rich in phyllosilicates.

Efficacy of repeated cycles of combination therapy for the eradication of infecting organisms in chronic bacterial prostatitis.

A total of 137 patients with a diagnosis of chronic bacterial prostatitis (CBP) were subjected to combination pharmacological therapy with antibacterial agents (ciprofloxacin/azithromycin), alpha-blockers (alfuzosin) and Serenoa repens extracts. Of those, 88 patients (64.2%) showed microbiological eradication at the completion of a 6-week cycle of therapy.