Posts in the category »   «  ( 39 Posts )

  • This was the INQUA Summer School on Active Tectonics and Tectonic Geomorphology in Prague

    The INQUA Summer School on Active Tectonics and Tectonic Geomorphology was held in Prague from 24-27 September, 2019. This summer school was run by INQUA‘s IFG EGSHaz as part of the TERPRO commission. The event was hosted by the Institute of Rock Structure and Mechanics, Academy of Sciences of the Czech Republic, Dpt. Neotectonics and Thermochronology. Main organizer was IFG co-leader Petra Štěpančíková. We would also like to thank MSc. Jakub Stemberk, Monika Hladká, Jana Šreinová, the deputy director Dr. Filip Hartvich, and all the staff involved for their professionalism and warm hospitality. Overall, 50 participants and 14 lecturers from 25 countries participated in the summer school.

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  • Registration now open for the INQUA Int’l Summer School on Tectonics & Tectonic Geomorphology, 24-27 Sep, 2019, Prague

    Register here for the INQUA International Summer School on Tectonics and Tectonic Geomorphology, 24-27 Sep 2019, Prague:

    ECR & DCR travel grants are also available! Note that no accommodation will be organised in Prague, but one night is included during the field trip.

  • New papers on paleoseismology, earthquakes, and active tectonics (Aug 2018)

    This time we have an impressive variety of earthquake study sites: Turkey, China, USA, Tadjik Basin, Italy, Japan, Sumatra, Himalayas, Spain, Mexico, Balkans, Mars, laboratory. Who could possibly ask for more? Plus some interesting work on fault physics. Check out the latest papers on earthquakes, active tectonics, and paleoseismicity:

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  • New papers on paleoseismology, tsunami, and active tectonics (Jan 2018)

    I hope you’ve had a great start into the new year. A lot of new and exciting papers have been published at the end of the old one, including work on New Zealand and Europe. Enjoy reading and have fantastic new year 2018!

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  • Almaty sits on a huge active fault, and here is why we know

    Almaty, the former capital of Kazakhstan and home to ~2 million people, is a rapidly growing, vibrant city, beautifully situated at the foothills of the mighty Zailisky Alatau, the northernmost mountain range of the Tien Shan at this longitude. The city sits on a huge alluvial fan with the snow-capped mountains in the background, reaching 5,000 m elevation. Almaty has suffered from earthquakes in its young history: in 1887, the Verny earthquake with a magnitude of about 7.3 had its epicentre a few kilometres west of the city but did not produce surface ruptures (Verny is the old name of Almaty). Only two years later, the M8 Chilik earthquake ruptured the surface 100 km to the southeast of Almaty. Finally, Almaty was heavily damaged by the 1911 Chon Kemin earthquake with a magnitude of ~8, which occurred on the southern flank of the Zailisky Alatau. In our new paper we now report on a fault that did not rupture in historical times, but surely did so in the Holocene – and this fault is right beneath the city. more

  • Postdoctoral Research Assistant Position/ Upper plate deformation – Mexican subduction, available March 2017

    The following open position might be of interest to the paleoseismology community:

    “We are seeking a Postdoctoral Research Assistant for a 12 month fixed term appointment working on the exciting new UNAM-CONACYT-funded project on “Spatial and Temporal Variations of Upper Plate Deformation across the Guerrero portion of the Mexican Subduction Zone” at the Institute of Geography and the Environmental Geophysics University Laboratory (LUGA), National Autonomous University of Mexico (UNAM), Campus Mexico City. The candidate will pursue fundamental and applied research into the assessment of both temporal and spatial vertical crustal deformation associated with both slow (interseismic) and rapid (coseismic) crustal deformation across the inner forearc region of the central Mexican subduction zone on the Guerrero sector, where the Cocos plate underthrusts the North American plate. The candidate will be responsible for the development and execution of laboratory and field research, conduct studies to develop a model of long-term deformation, writing reports and papers. more

  • This was my field work on active faults in Kazakhstan 2015 (pt. II)

    The first part of my report on the field work that I did in Kazakhstan this year focussed on the stuff we had done in the South. Here is part II which is all about the Dzhungarian Fault. You’ve never heard about this fault? That’s easily possible. There are only very few papers that deal with this fault. In the 1960s Soviet geologist V.S. Voytovich published results from extensive field work on this fault (Voytovich, 1965; 1969). 40-50 years later a few studies on geodesy and geodynamics covered the broader study area and Shen et al. (2003) did some work in the Chinese part of the fault, but it took until 2013 before Campbell et al. revisited the Kazakh side and came up with new field data. They focussed on the tectonic geomorphology of this structure and determined a slip rate. Given this little amount of research done one would assume that the fault is not very large and of minor importance, but the opposite is true. The fault is around 300 km long in its Kazakh section and probably twice as long in total! more

  • What’s up? The Friday links (82)

    Today is Friday and here are your links on human-caused earthquakes, induced aseismic slip, typesetting costs, flash flood video footage, and more!

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  • This was the Fucino15 meeting – part II

    I blogged about the scientific sessions at the Fucino15 meeting last week, here’s my report about the pre- and post-meeting field trips. The pre-meeting field trip was held in Rome, where we explored the archaeological and historical evidence for earthquake damage in the Eternal City. After the conference we followed the traces of the 1915 Fucino earthquake and then finally visited L’Aquila. This blog covers Rome and the geological field trips, a special on L’Aquila will follow later. more

  • Tectonics from above – RAS discussion meeting

    Last Friday the RAS held a discussion meeting on Tectonics from Above: Recent Advances in the Use of High-resolution Topography and Imagery in London. Almost the entire Cambridge Tectonics Group went there and I absolutely enjoyed the meeting and the discussion with friends and colleagues mainly from the UK and from France. The speakers reported on open-source software for producing high-res DEMs, advances in aerial and satellite imagery, new techniques in remote sensing, and latest developments in fault/offset mapping. The meeting was supported by NERC, COMET+ and LICS. more

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