1 / 6

Croatian FAULT-plane solutions (fps) database

M. Herak, S. Markušić, D. Herak Department of Geophysics, Faculty of Science University of Zagreb, Zagreb. Croatian FAULT-plane solutions (fps) database. Source detail is needed for NGA. Application of modern GMPE requires DETAILED knowledge of source properties.

shiloh
Download Presentation

Croatian FAULT-plane solutions (fps) database

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. M. Herak, S. Markušić, D. Herak Department of Geophysics, Faculty of Science University of Zagreb, Zagreb Croatian FAULT-plane solutions (fps) database

  2. Source detail is needed for NGA... Application of modern GMPE requires DETAILED knowledge of source properties. For instance: Abrahamson & Silva (2008), M = 7, Rrup = 5 km, RJB = 5 km, FHW = 1, W = 15 km: dip = 45° PGA = 0.48 gdip = 80°  PGA = 0.39 g

  3. Croatian FPS database • 216 solutions • 1909–2012 • Excel-database • 161 FPS computed by us (first motion polarity) • 6 by CMT Harvard, MEDNET, ZUR_RMT • 31 by Pondrelli et al. • 18 by ARSO, Slovenia

  4. Croatian FPS database • P-axis (horizontal projection) – only quality 2 and better • Tectonic stresses are directed SW–NE (in the southern and eastern regions) to S–N (in the northern and western parts). • This reflects counter-clockwise motions of Adria and its compression against the Dinarides. • Most of solutions indicate reverse or strike-slip faulting.

  5. Croatian FPS database Zagreb and Pokupsko areas (M > 3.45) Banja Luka region (M> 3.95) In general, solutions agree with tectonics and mapped faults quite well.

  6. Croatian FPS database – conclusions • The database is regularly updated at least twice a year. • The database is now good enough to roughly define geometry of faulting in many (but not all!) Croatian and neighbouring regions. • Rapid and easy access to data of neighbouring networks would greatly improve solutions (past and future!). • An effort to adopt routine moment-tensor computation for local and regional earthquakes is needed! • All software is written by us and is free to anyone.

More Related