Today we went for field work again – mapping active faults in Northern Attica, trying to find out about offsets and slip rates, and scouting sites for applying Ground Penetrating Radar (GPR) later. We found some very beautiful fault scarps and measured a good number of strike and dip values. At two locations we also recorded topographic profiles across the scarps in order to get an idea about the vertical offset. Combined with the assumption that these scarps are post-glacial, we can estimate slip rates. more
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Field work on active faults – wildlife edition
2013-05-09 | in Centerfault, Teaching -
Field work on active faults in Greece
| in Centerfault, Teaching | 2 responsesI am currently in Greece for field work on faults in the vicinity of Athens. Sascha from RWTH Aachen University is doing his MSc. thesis on remote sensing, geophysical analyses, and mapping of some structures that we think could be active, and me and Ioannis are with him in the field for the first few days. Right on the first day we found some promising outcrops which we will map and check in detail during the next days. more
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New Papers: BSSA Special Issue on the Tohoku Earthquake and Tsunami, Japan, March 2011
2013-05-04 | in PaperThe latest issue (May 2013) of the Bulletin of the Seismological Society of America (BSSA) is dedicated to the Tohoku Earthquake and Tsunami of March 2011. The studies published therein deal with the source models of the megaquake and rupture dynamics, the ground motions, the tsunami propagation, earthquake triggered landslides and induced seismicity, earthquake environmental effects, and one paper presents a new proposal for an extended Tsunami Intensity scale. more
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Kind of surprising M4.5 earthquake in NE Hungary
2013-04-23 | in Earthquake | one responseLast night (22:29 UTC on 22 April) a M4.5 earthquake rattled NE Hungary. The event was shallow (~10 km) and the epicentre was only about 25 km south of the city of Eger, famous for its red wine (Egri bikavér). The area is south to the Inner Western Carpathian Mountains. Light damage has been reported from the epicentral area, the EMSC questionnaires document intensities of VI. more
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Shallow M3.0 earthquake in W Germany, near ex-NPP Mülheim-Kärlich
2013-04-18 | in EarthquakeA shallow (12 km) earthquake of magnitude ML3.0 occurred this morning in W Germany near Koblenz in Ochtendung. According to the Geological Survey of Baden Württemberg, the magnitude was ML2.6 only, but the quake was preceded by few minor events (M<2.0) on 9 April and 14 April. Local news (The Rhein Zeitung) report that some people felt the event and that birds were afraid. This earthquake didn’t cause any damage, but it’s interesting in another way: Its epicentre is only 8 km away from the former nuclear power plant (NPP) Mülheim-Kärlich. more
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Shallow (update: medium depth) M7.8 earthquake hits E Iran, widely felt across Middle East
2013-04-16 | in EarthquakeA very strong earthquake occurred in Eastern Iran close to the Iran-Pakistan border. USGS reports a magnitude of 7.8 and a shallow depth of 15 km, EMSC data suggest M7.7 and 50 km depth. Preliminary shake maps estimate intensities around MSK VIII, which would be enough to make traditional adobe buildings to collapse. Reports confirm the event was felt as far away as Muscat, Oman (600 km distance!). Update: USGS now also reports a depth of 80 km.
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M6.3 earthquake rocks southwestern Iran, felt in Dubai, Abu Dhabi, Qatar, Bahrain
2013-04-09 | in EarthquakeUpdate: Read the article of The Times of Oman here!
Today at 11:52:50 UTC a magnitude 6.3 earthquake occurred in SW Iran close to the shore in a depth of 10 km. The event was widely felt in Iran and across the NE Arabian Peninsula. Moment tensor solution reveal a thrust mechanism, which is in perfect concordance with the historic seismicity pattern. The event was caused by the convergence of the Arabian and Eurasian plates, that not only built up the impressive Zagros Mountains, but also lead to the formation of the Makran Subduction Zone. Relative plate motions there are as fast as 20 mm/yr in the central part. more
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Georadar on active (?) faults in Oman
2013-04-08 | in Centerfault, Earthquake | 2 responsesI am currently at GUtech in Oman, a sister university of RWTH Aachen University, for teaching Geophysics and I spend most of the free time in the field with my colleague Gösta Hoffmann. On Friday we went to the Batinah area NW of Mascat to look for active faults. The Batinah is a plain of most likely Quaternary age, made up from the sediments delivered from the huge mountains in the south. Folded Tertiary limestones are cropping out close to the mountain range. Some of them are covered by Quaternary gravels, others aren’t. more
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Aachen 2013 – 4th International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology, 9-14 October, Aachen, Germany
2013-03-24 | in Aachen 2013, Meeting, PATA daysDear friends and colleagues,
in 2013 we will organize the 4th International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology in Western Germany. The online registration will open soon at paleoseismicity.org and additional information will follow during the next days.
Date: 9-14 October 2013
Location: Aachen, Germany
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Paleoseismological papers in the BSSA April 2013 issue
2013-03-22 | in PaperBSSA’s most recent issue is full of paleoseismological work. The April 2013 issue contains a number of papers dealing with old earthquakes in Turkey, California, Argentina, and Jamaica. Also, there’s info on earthquake catalogues in South America and China. A study on seismic sources in the Lower Rhine Embayment, (W Germany, Belgium, The Netherlands) is especially interesting for me, because it’s right in my backyard. Plus, there are some basic studies on the reliability of paleoseismological investigation and problems in earthquake geology. more