In my DFG-financed project “Earth surface response to Quaternary faulting and shallow crustal structure in the eastern Adria-Alpine collision zone and the Friulian plain” I investigate the active faults of NE Italy and western Slovenia. This project is part of the Priority Programme SPP2017 “Mountain Building Processes in 4D“. We’ve now published a paper on the activity of the Udine-Buttrio thrust fault. The paper is open access and available here.
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New paper: Tectonic activity of the Udine-Buttrio Thrust in NE Italy
2020-02-24 | in Paper -
Papers on harbours & archaeoseismology in the Med
2017-09-05 | in PaperWhile compiling the monthly paper round-up, I will of course miss some publications. This may be because I was in the field when the papers were published, because I don’t have an alert for the journals, or because my alerts didn’t include the right key words. For example, I missed a couple of 2017 papers by our colleagues from Mainz: more
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A Holocene surface rupture in Germany
2016-02-13 | in Earthquake, Paper | 4 responsesI am quite happy that our new paper has finally been published in GJI. We worked on a fault between Aachen and Cologne in Germany and found that there has been a surface rupturing earthquake less than 9000 years ago, and possibly not much older than 2500 years BP. The area is of interest also because in 1755/56 a series of damaging earthquakes hit Düren and its surroundings – these are the strongest historical events in Germany that we know of. The quakes were felt as far away as Berlin, Strasbourg, and London, yet there were no primary ruptures. “Our” quake must have been much stronger… more
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Crete and mainland Greece Fieldwork, March 2014
2014-04-14 | in Centerfault, Events | 2 responsesDuring the month of March 2014, Sascha and I along with Tobi and Lauretta (BSc students from RWTH University) were in Greece for fieldwork. The fieldwork campaign started on the island of Crete; our institute at RWTH Aachen has a joint project with Mainz University to carry out paleotsunami investigations on the island. The western part of Crete was uplifted by approximately 9 m during the 21st July AD 365 earthquake and also hit by the associated tsunami. Due to the strong seismic and highly tsunamigenic activity of the nearby Hellenic Trench, it is suggested that numerous earlier tsunamis have also struck the island. more