Routine Regional Moment Tensor Inversion for Earthquakes in the Greek Region: The National Observatory of Athens (NOA) Database (2001-2006)

Research Article| September 01, 2010 Routine Regional Moment Tensor Inversion for Earthquakes in the Greek Region: The National Observatory of Athens (NOA) Database (2001–2006) K. I. Konstantinou; K. I. Konstantinou Institute of Geophysics National Central University Jhongli, 320 Taiwan kkonst@ncu.edu.tw (K. I. K.) 1Institute of Geophysics, National Central University, Jhongli, Taiwan Search for other works by this author on: GSW Google Scholar N. S. Melis; N. S. Melis Institute of Geophysics National Central University Jhongli, 320 Taiwan kkonst@ncu.edu.tw (K. I. K.) 2Institute of Geodynamics, National Observatory of Athens, Greece Search for other works by this author on: GSW Google Scholar K. Boukouras K. Boukouras Institute of Geophysics National Central University Jhongli, 320 Taiwan kkonst@ncu.edu.tw (K. I. K.) 2Institute of Geodynamics, National Observatory of Athens, Greece Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2010) 81 (5): 750–760. https://doi.org/10.1785/gssrl.81.5.750 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation K. I. Konstantinou, N. S. Melis, K. Boukouras; Routine Regional Moment Tensor Inversion for Earthquakes in the Greek Region: The National Observatory of Athens (NOA) Database (2001–2006). Seismological Research Letters 2010;; 81 (5): 750–760. doi: https://doi.org/10.1785/gssrl.81.5.750 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search The routine use of regional broadband data for the determination of moment tensors of even very small events (Mw ∼ 3.5) has considerably enhanced our understanding of tectonic processes in many active regions worldwide (e.g., Kao and Jian 2001; Braunmiller et al. 2002; Kubo et al. 2002; Pondrelli et al. 2002; Clinton et al. 2006; Risteau 2008). This development can be attributed to a number of reasons, such as the ability to generate accurate synthetic seismograms for a given velocity model and an increase in the amount and quality of data... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.