Detection and Identification of Low-magnitude Seismic Events near Bala, Central Turkey, Using Array-based Waveform Correlation

Abstract

Research Article| January 01, 2011 Detection and Identification of Low-magnitude Seismic Events near Bala, Central Turkey, Using Array-based Waveform Correlation Korhan U. Semin; Korhan U. Semin Search for other works by this author on: GSW Google Scholar Nurcan M. Ozel; Nurcan M. Ozel Search for other works by this author on: GSW Google Scholar Ocal Necmioglu Ocal Necmioglu Search for other works by this author on: GSW Google Scholar Author and Article Information Korhan U. Semin Nurcan M. Ozel Ocal Necmioglu Publisher: Seismological Society of America First Online: 09 Mar 2017 Online ISSN: 1938-2057 Print ISSN: 0895-0695 © 2011 by the Seismological Society of America Seismological Research Letters (2011) 82 (1): 97–103. https://doi.org/10.1785/gssrl.82.1.97 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 Korhan U. Semin, Nurcan M. Ozel, Ocal Necmioglu; Detection and Identification of Low-magnitude Seismic Events near Bala, Central Turkey, Using Array-based Waveform Correlation. Seismological Research Letters 2011;; 82 (1): 97–103. doi: https://doi.org/10.1785/gssrl.82.1.97 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 Belbasi Seismic Station is composed of two seismic sub-arrays. One is a medium-period seismic array with a radius of about 45 km located in Ankara, and the second is a short-period seismic array with a radius of about 3 km located in Keskin. The distance between the two arrays is approximately 80 km. Both arrays consist of seven elements. Each array has a broadband seismometer located at the middle element of the circular array. Short-period vertical seismometers (Geotech 23900) are installed at depth 30 m from the surface while medium and broadband instruments (Geotech KS54000) are installed at depth 60... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.