TY - JOUR A1 - Kinscher, Jannes A1 - Krüger, Frank A1 - Woith, H. A1 - Lühr, B. G. A1 - Hintersberger, E. A1 - Irmak, T. Serkan A1 - Baris, S. T1 - Seismotectonics of the Armutlu peninsula (Marmara Sea, NW Turkey) from geological field observation and regional moment tensor inversion JF - Tectonophysics : international journal of geotectonics and the geology and physics of the interior of the earth N2 - The Armutlu peninsula, located in the eastern Marmara Sea, coincides with the western end of the rupture of the 17 August 1999, Izmit M-W 7.6 earthquake which is the penultimate event of an apparently westward migrating series of strong and disastrous earthquakes along the NAFZ during the past century. We present new seismotectonic data of this key region in order to evaluate previous seismotectonic models and their implications for seismic hazard assessment in the eastern Marmara Sea. Long term kinematics were investigated by performing paleo strain reconstruction from geological field investigations by morphotectonic and kinematic analysis of exposed brittle faults. Short term kinematics were investigated by inverting for the moment tensor of 13 small to moderate recent earthquakes using surface wave amplitude spectra. Our results confirm previous models interpreting the eastern Marmara Sea Region as an active transtensional pull-apart environment associated with significant NNE-SSW extension and vertical displacement. At the northern peninsula, long term deformation pattern did not change significantly since Pliocene times contradicting regional tectonic models which postulate a newly formed single dextral strike slip fault in the Marmara Sea Region. This area is interpreted as a horsetail splay fault structure associated with a major normal fault segment that we call the Waterfall Fault. Apart from the Waterfall Fault, the stress strain relation appears complex associated with a complicated internal fault geometry, strain partitioning, and reactivation of pre-existing plane structures. At the southern peninsula, recent deformation indicates active pull-apart tectonics constituted by NE-SW trending dextral strike slip faults. Earthquakes generated by stress release along large rupture zones seem to be less probable at the northern, but more probable at the southern peninsula. Additionally, regional seismicity appears predominantly driven by plate boundary stresses as transtensional faulting is consistent with the southwest directed far field deformation of the Anatolian plate. (C) 2013 Elsevier B.V. All rights reserved. KW - Seismotectonics KW - Moment tensor inversion KW - Brittle fault analysis KW - Morphotectonics KW - North Anatolian Fault Zone (NAFZ) KW - Marmara Sea Y1 - 2013 U6 - https://doi.org/10.1016/j.tecto.2013.07.016 SN - 0040-1951 SN - 1879-3266 VL - 608 IS - 46 SP - 980 EP - 995 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Sirocko, Frank A1 - Dietrich, Stephan A1 - Veres, Daniel A1 - Grootes, Pieter M. A1 - Schaber-Mohr, Katja A1 - Seelos, Klemens A1 - Nadeau, Marie-Josee A1 - Kromer, Bernd A1 - Rothacker, Leo A1 - Roehner, Marieke A1 - Krbetschek, Matthias A1 - Appleby, Peter G. A1 - Hambach, Ulrich A1 - Rolf, Christian A1 - Sudo, Masafumi A1 - Grim, Stephanie T1 - Multi-proxy dating of Holocene maar lakes and Pleistocene dry maar sediments in the Eifel, Germany JF - Quaternary science reviews : the international multidisciplinary research and review journal N2 - During the last twelve years the ELSA Project (Eifel Laminated Sediment Archive) at Mainz University has drilled a total of about 52 cores from 27 maar lakes and filled-in maar basins in the Eifel/Germany. Dating has been completed for the Holocene cores using 6 different methods (Pb-210 and Cs-137 activities, palynostratigraphy, event markers, varve counting, C-14) In general, the different methods consistently complement one another within error margins. Event correlation was used for relating typical lithological changes with historically known events such as the two major Holocene flood events at 1342 AD and ca 800 BC. Dating of MIS2-MIS3 core sections is based on greyscale tuning, radiocarbon and OSL dating, magnetostratigraphy and tephrochronology. The lithological changes in the sediment cores demonstrate a sequence of events similar to the North Atlantic rapid climate variability of the Last Glacial Cycle. The warmest of the MIS3 interstadials was GI14, when a forest with abundant spruce covered the Eifel area from 55 to 48 ka BP, i.e. during a time when also other climate archives in Europe suggested very warm conditions. The forest of this "Early Stage 3 warm phase" developed subsequently into a steppe with scattered birch and pine, and finally into a glacial desert at around 25 ka BP. Evidence for Mono Lake and Laschamp geomagnetic excursions is found in two long cores. Several large eruptions during Middle and Late Pleistocene (Ulmener Maar - 11,000 varve years BP, Laacher See - 12,900 varve years BP, Mosenberg volcanoes/Meerfelder Maar 41-45 cal ka BP, Dumpel Maar 116 ka BP, Glees Maar - 151 ka BP) produced distinct ash-layers crucial for inter-core and inter-site correlations. The oldest investigated maar of the Eifel is Ar-40/Ar-39 dated to the time older than 520 ka BP. KW - Eifel maar KW - Laminated lake sediments KW - Tuning KW - Historical events KW - C-14-derived chronology KW - Varve counting KW - Luminescence dating KW - Palynostratigraphy KW - (CS)-C-137 and Pb-210 dating KW - Palaeomagnetism KW - Tephrostratigraphy KW - Argon-Argon dating KW - GIS Y1 - 2013 U6 - https://doi.org/10.1016/j.quascirev.2012.09.011 SN - 0277-3791 VL - 62 SP - 56 EP - 76 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Hinzen, Klaus-G A1 - Reamer, Sharon K. A1 - Scherbaum, Frank T1 - Slow fourier transform JF - Seismological research letters Y1 - 2013 U6 - https://doi.org/10.1785/0220120139 SN - 0895-0695 VL - 84 IS - 2 SP - 251 EP - 257 PB - Seismological Society of America CY - Albany ER -