Month: September 2018
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Identifying the recurrence patterns of non-volcanic tremors using a 2-D hidden Markov model
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Tectonic movements create stress within the Earth’s crust, which gets released in sudden earthquakes, but also in less dramatic slow slip events. Such events are sometimes accompanied by so-called non-volcanic tremors – weak seismic signals of extended duration along major faults.
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Final presentations from the 2018 LML Summer School now online
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The LML Summer School for 2018 ran from mid-July to mid-August and was a great success, with eight students collaborating on projects supervised by LML Fellows. The students made their final presentations on 17 August, and these are now available online, links […]