The Seismological Society of America has currently three interesting calls for papers.
The Department of Earth Sciences at the University of Oxford is currently recruiting a PDRA in Active Tectonics Research:
We seek to appoint a Postdoctoral Research Assistant to work closely with Professor Richard Walker as part of a broader consortium in the NERC-funded ‘Looking Into the Continents from Space’ project, whose principal aim is to provide insights into earthquake hazard and crustal deformation through the application of a range of remote-sensing, field-based, seismological, and modelling approaches. The post is co-funded by COMET, which is a world-leading centre for understanding tectonic and volcanic processes and hazards (comet.nerc.ac.uk). The PDRA will join a thriving group involved in remote-sensing and field-based research in the study of active faulting and natural hazards.
The post is based in the Department of Earth Sciences and will be overseen by Richard Walker, Barry Parsons and Philip England. The post will also involve close collaboration with scientists at the other partner institutions involved in COMET and LICS. The successful applicant will be responsible for the mapping and analysis of fault-based geomorphology using high-resolution satellite imagery and digital topography, supplemented with fieldwork in selected regions. The production of high-resolution digital topographic datasets through field-based, aerial, or satellite methods, forms an important component of the duties. They will also be expected to possess or to develop skills in measuring surface displacements through the matching of optical satellite imagery, and to support both tectonic and volcanic applications of high-resolution imagery and elevation data throughout COMET
Find more information here: https://my.corehr.com/pls/uoxrecruit/erq_jobspec_version_4.display_form?p_company=10&p_internal_external=E&p_display_in_irish=N&p_process_type=&p_applicant_no=&p_form_profile_detail=&p_display_apply_ind=Y&p_refresh_search=Y&p_recruitment_id=142106
or at the department website: https://www.earth.ox.ac.uk/vacancies/.
Application deadline is 9 September 2019.
On July 4th and 5th, 2019 two earthquakes (Mw 6.4 and Mw 7.1, respectively) occurred in eastern California and produced distinct surface ruptures. Field surveys started immediately after the first event and, less than two weeks later, a provisional map of surface rupture was compiled and made available to everyone (Contributors from USGS, CGS, UNR, USC, CSUF). I downloaded the map and kmz files of the ruptures from the SCEC response site, which contains tons of fruitful information.
The two strike-slip earthquakes ruptured two perpendicular faults, the first running NE-SW with left-lateral slip and the second running NW-SE with right-lateral slip (Figure 1). The location of the earthquake falls within the Eastern California shear zone, a region of distributed faulting associated with motion across the Pacific-North America plate boundary, and an area of high seismic hazard.
Ruptures come with a variable degree of complexity: some sectors show a “simple” single strand, others show multiple sub-parallel or diverging splays. Distributed faulting represents displacements occurred off the principal fault and is generally made up by less continuous ruptures, which can be located tens of meters to a few kilometers from the principal fault trace. A method to evaluate the fault displacement hazard has been proposed by Youngs et al. (2003) and later refined by Petersen et al. (2011); the former study analyzed normal faults, while the latter analyzed strike-slip faults.
Basically, the method defines the conditional probability of faulting occurrence as a function of distance from the principal fault and derives scaling relations between rupture probability and distance. I applied the same method on the 2019 sequence and compared the output with the results by Petersen; results are grid-dependent – since available data are still provisional, I used a quite coarse grid size of 200 m, more detailed studies will come.
Results are in good agreement (Figure 2): the 2019 ruptures show a higher than average rupture probability at 0-2 km from the main fault, but also taper out faster than the previous events.
References:
Petersen, M. D., et al. (2011). Fault displacement hazard for strike-slip faults. BSSA, 101(2), 805-825.
Youngs, R. R., et al. (2003). A methodology for probabilistic fault displacement hazard analysis (PFDHA). Earthquake Spectra, 19(1), 191-219.
The next INQUA meeting on Paleoseismology, Archaeoseismology, and Active Tectonics (PATA Days) will be held in Hornitos, Chile, from 8-12 November, 2020. Download the 1st circular here (PDF, 400 kb).
See you all in Chile 2020!
Dr. Gülsen Ucarkus send us the first circular for the following interesting meeting:
moreWe would like to invite you to the international meeting organized by Active Tectonics Research Group (ATAG) of Turkey in commemoration of 20th Anniversary of 1999 Marmara Earthquakes. Following these two devastating earthquakes (1999 Mw 7.4 İzmit and 1999 Mw 7.2 Düzce Earthquakes), a vast number of international/national projects carried out in the Marmara Sea region of Turkey and the outcomes of research done contributed significantly to multi-disciplinary studies in active tectonics. The meeting aims to revisit the results of these important number of observations together with new research going on to highlight the current state of seismic hazard in Marmara Sea where the next big earthquakes is expected to occur.
The second circular for the Summer School on Active tetonics in Prague, 24-27 September, 2019, is out now. Download here. We are sorry that the summer school is already fully booked. See you in Prague in September!
The event organised by the Institute of Rock Structure and Mechanics (Czech Academy of Sciences), Charles University in Prague (Faculty of Science), Masaryk University in Brno, and INQUA’s IFG EGSHaz. We are supported by, and work in the framework of, INQUA – the International Union for Quaternary Research, and the Czech Association of Geomorphologists (CAG) as a contributor and member of IAG.
This is a pretty cool job opportunity in one of the world’s most interesting places. Topics include: (1) developing techniques for processing historical aerial photographs into digital elevation data; (2) analysis of pre- and post-earthquake data for the purpose of assessing fault geometries, connectivity and kinematics; (3) modelling multi-fault ruptures using geologic and remotely sensed validation datasets, and exploring the implications of this research for seismic hazard analysis.
https://findajob.agu.org/job/8009710/phd-scholarship-at-the-university-of-canterbury-new-zealand/
Pa·le·o·seis·mic·i·ty [ pālē·ə·sīz·mĭs′ĭ·tē ] noun, plural -ties. Ancient earthquake activity.
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