The 3rd INQUA-IGCP 567 Int’l workshop on Earthquake Geology, Paleoseismology and Archaeoseismology has started here in Morelia, Mexico. We are going to cover the sessions whenever we have time to drop a few lines, however, we can not comment all talks and posters.
[Note: this post was updated on 2012-11-29, see Maria’s comment]
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Quite near my personal working area or, in other words, some hundreds of kilometers away (which I didn’t experience as much of a distance in a huge country like China), the terrific and over 1500 km long Altyn Tagh Fault separates the northern Tibetan Plateau from the Tarim Basin and the Alashan and Alxa blocks. more
Natural Hazards and Earth System Sciences (NHESS) has just published a new issue with lots of papers on marine and lake paleoseismology. So enough stuff for a good read on a cold and rainy autumn evening. The Special issue was edited by Daniela Pantosti, Eulàlia Gràcia, Geoffroy Lamarche, and Hans Nelson, and is an outcome of the European Science Foundation Research Conference: Submarine Paleoseismology – The Offshore Search of Large Holocene Earthquakes; Obergurgl, Austria, 11-16 September 2010. All articles are availabe for free download! Open access rules! more
The preliminary program of the 3rd INQUA-IGCP 567 Workshop to be held at Morelia (Mexico) from 19 – 23 November 2012 is out now. This program is subject to very minor modifications regarding social events, etc.. The scientific program will be the definitive one, but might be subject to late unforeseen inconveniences.
Please note that some dates like the field trip have changed! more
The Sparta Fault in Greece is marked by one of the most impressive mountain fronts I’ve ever seen. A huge (yes, huge!) fault scarp has developed, traceable for kilometers; the fault itself is more than 60 km long. Ancient Sparta has been devastated by the last known major (M>7) earthquake that happened at this fault in 464 BC. Now, Papanikolaou et al. have published new data on this fault. They examined how paramaters like throw, segmentation, and catchments vary along strike and created a new seismic hazard map, showing a site-specific long-term recurrence interval of ~1.8 ka (+/- 450 a). more
This morning at 03:00 UTC an earthquake with magnitude MW7.7 occurred in the Sea of Okhotsk. Due to its great depth of more than 600 km no tsunami was triggered and surface shaking was pretty low, however, the event was felt in a wide area. Moment tensor solutions indicate a thrust event. Historical seismicity tells us that significant earthquakes are likely to happen in the region and mostly occur in great depths, but at this certain location only few events have been registered during the last decades. more
Although I already recommended some papers earlier this week, I have two more to mention: Supawit Yawsangratt and colleagues published new data on “Evidence of probable paleotsunami deposits on Kho Khao Island, Phang Nga Province, Thailand”. Nat Hazards, 63,151-163, DOI 10.1007/s11069-011-9729-4 in a special issue dedicated to tsunami research. Ran et al. presented work on the Wenchuan EQ epicentral area: “Paleoseismic events and recurrence interval along the Beichuan -Yingxiu fault of Longmenshan fault zone, Yingxiu, Sichuan, China.” Tectonophysics (2012), doi: 10.1016/j.tecto.2012.07.013. more
Currently I spend my time working on some papers that deal with tsunamis in the Eastern Mediterranean and earthquakes in Spain. Searching for literature and looking for data on the Minoan catastrophe I came across this new open access publication by Simon Jusseret and Manuel Sintubin:
Our colleagues from IGCP567 – Earthquake Archaeology put a lot of effort into getting rid of catastrophism and into making archeoseismology a more reliable, quantitative science. By the way, don’t miss the next workshop on archeoseismology and active tectonics in Mexico 2012! more
On 11 April 2012, a Mw8.6 strike-slip earthquake occurred off Sumatra in a kind of intra-plate setting and came as a surprise to the earthquake community. Such a strong strike-slip event was not expected, we always thought that the huge thrust quakes at subduction zones were the only ones to release that much energy. Now a press release by CalTech reports on the latest studies that came to the result that many previously unknown perpendicular faults ruptured at this event. Immediately some journalists suggested that this might also happen at the San Andreas Fault. I do not know of any paleoseismological evidence that this has happened there before. However, how likely is this scenario?
Link to the paper: An earthquake in a maze: compressional rupture branching during the April 11 2012 M8.6 Sumatra earthquake. more
The deadline for the 3rd INQUA-IGCP567 workshop on Active Tectonics, Paleoseismology and Archeoseismology has been extended to 15 August 2012. The meeting will be held from 19-24 November in Morelia, Mexico, in remembrance of the devastating Acambay earthquake form 1912. Registration is between $60 and $250, an additional fieldtrip can be booked for $60. more