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• W2000148468 abstract "Research Article| January 01, 2000 North Aegean crustal deformation: An active fault imaged to 10 km depth by reflection seismic data Mireille Laigle; Mireille Laigle 1Laboratoire de Sismologie Expérimentale, UMR 7580 CNRS, Institut de Physique du Globe, 4, place Jussieu, 75252 Paris, France Search for other works by this author on: GSW Google Scholar Alfred Hirn; Alfred Hirn 1Laboratoire de Sismologie Expérimentale, UMR 7580 CNRS, Institut de Physique du Globe, 4, place Jussieu, 75252 Paris, France Search for other works by this author on: GSW Google Scholar Maria Sachpazi; Maria Sachpazi 2National Observatory of Athens, Lofos Nymfon, Athens, Greece Search for other works by this author on: GSW Google Scholar Nikos Roussos Nikos Roussos 3Hellenic Petroleum, Maroussi, Athens, Greece Search for other works by this author on: GSW Google Scholar Author and Article Information Mireille Laigle 1Laboratoire de Sismologie Expérimentale, UMR 7580 CNRS, Institut de Physique du Globe, 4, place Jussieu, 75252 Paris, France Alfred Hirn 1Laboratoire de Sismologie Expérimentale, UMR 7580 CNRS, Institut de Physique du Globe, 4, place Jussieu, 75252 Paris, France Maria Sachpazi 2National Observatory of Athens, Lofos Nymfon, Athens, Greece Nikos Roussos 3Hellenic Petroleum, Maroussi, Athens, Greece Publisher: Geological Society of America Received: 01 Jun 1999 Revision Received: 05 Oct 1999 Accepted: 13 Oct 1999 First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2000) 28 (1): 71–74. https://doi.org/10.1130/0091-7613(2000)28<71:NACDAA>2.0.CO;2 Article history Received: 01 Jun 1999 Revision Received: 05 Oct 1999 Accepted: 13 Oct 1999 First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Mireille Laigle, Alfred Hirn, Maria Sachpazi, Nikos Roussos; North Aegean crustal deformation: An active fault imaged to 10 km depth by reflection seismic data. Geology 2000;; 28 (1): 71–74. doi: https://doi.org/10.1130/0091-7613(2000)28<71:NACDAA>2.0.CO;2 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 SocietyGeology Search Advanced Search Abstract Three multichannel seismic profiles imaged a normal fault to at least 10 km depth in the North Aegean Trough and Thermaïkos basin. The fault is active and recent, forming a scarp at sea bottom and crossing the Quaternary deltaic front on the northern slope of the trough controlled to the south by the North Anatolian fault. Prestack depth migration imaged the fault as a seismic reflector cutting steeply across the sedimentary rocks and flattening in the basement. From the seismic image, the N100°E strike of the fault scarp, and the orientations of the three profiles, the true fault dip is constrained to an average 20° in the basement, a low-angle dip. The throw and age estimated from the geometry in the sedimentary rocks document recent onset of the motion that must have occurred at a high rate. Both the direction and the rate of slip are consistent with the instantaneous motion as measured by space-based geodesy, which shows the fault to be forming by pure normal slip. Large earthquakes that have occurred in the basin may relate to such normal faults, whereas the North Anatolian fault with its current strike-slip earthquakes appears to slip here under low resolved shear stress. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2000148468 title "North Aegean crustal deformation: An active fault imaged to 10 km depth by reflection seismic data" @default.
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