Here is the latest list of papers that deal with paleoseismology, past large earthquakes, active faults, archaeoseismology, and earthquake proxies such as tsunamis. Enjoy reading and let us know if we’ve missed something.
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The Seismology and Gravimetry Section of the Royal Observatory of Belgium and the Unit of Physical Geography and Quaternary of the University of Liège recruit a postdoctoral researcher in earthquake geology and tectonic geomorphology. The position is for 2 yrs, and 50% funding is already secured for an additional 5 years. Deadline is 28 March, 2024. Download the ad with all details here:
The PATA Days are the meeting on Paleoseismology, Active Tectonics, and Archaeoseismology, organised within the framework of INQUA‘s TERPRO commission. The official website has been launched, containing all infos on the programme, field trips, grant applications, the venue, the abstract template, and the deadlines. Check it out: https://www.patadayschile.cl.
Abstract submission will open 4 March and the deadline for the 4-page abstracts is 29 March. No short abstracts this time.
See you all in Chile in October!
Our colleague Tejpal Singh and his co-guest editors Riccardo Caputo and Chittenipattu P. Rajendran invite contributions to their special issue “Earthquake Geology of Plate Margins and Plate Interiors: Integrating Classical Methods with New Approaches” to be published in Geosciences. Please find more info here:
– Focus: Mexican Pacific coast – Subduction Zone
– Responsibilities: Field and lab research on coastal geomorphology and tectonic deformation, or/and earthquake, and tsunami geology
– Qualifications: Recent Ph.D. in earth sciences, desirable background in either coastal geomorphology, earthquake geology, sedimentology, Quaternary dating, microfossils analytical techniques
In a new study, Rosell et al. look into the earthquake history of the Tambomachay Fault near Cusco in Peru. Cusco has been hit by damaging earthquakes in 1650, 1950, and 1986, and there is also some evidence for another earthquake during Inca times between AD 1418–1471. Very little is known about the causative faults. There is also very limited information on older events. The closest fault to the city is a 20 km-long normal fault at the northern margin of the Cusco Basin, the Tambomachay Fault. Here we constrained the fault’s Holocene slip rate by dating offset lateral moraines, and we identified three Holocene surface ruptures in a paleoseismological trench. The study was recently published open access in τeκτoniκa.
moreThis has become a long list again, and I partly blame the New Zealanders who are currently publishing a lot of studies related to their new hazard model. Really cool work! But of course the inclined readers will also find other gems for their taste. As always – please send me paleoseismology studies that I have missed. Enjoy reading!
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