Abstract. We make a thorough review of geological and seismological data on the long-lived Schio-Vicenza Fault System (SVFS) in northern Italy present for it geodynamic seismotectonic interpretation. The SVFS is major high-angle structure transverse to mean trend eastern Southern Alps fold-and-thrust belt, knowledge this deeply rooted literature spans more than century half. main fault (SVF), w...

We present our analysis of the characteristics waveforms earthquakes and quarry blasts that occurred within extreme local-distance (< 25 km) Csókakő (CSKK) station in Vértes Hills, Hungary. Our motivation was to determine linear discrimination line between earthquake explosion populations. CSKK is located Mór Graben, a seismically relatively active region, also characterized by significant mini...

How can the sluggish, long-wavelength mantle convection be expressed by so many time and space scales of morphotectonic activity? To investigate these relationships, we explore Java-Banda subduction zone, where geodynamic records cluster. In far-East Tethys, exceptionally arcuate Banda zone circumscribes deepest oceanic basin on Earth, seismotectonic activity slices upper plate more efficiently...