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Postdoctoral researcher (M/F). Modeling damage during earthquakes. Comparison with geophysical data.
generated during earthquakes. The work will be based on the joint study of micromechanical damage models and their comparison with seismological and geodetic data published as part of this same ANR project
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-seismic deformation models for the various earthquakes. Responsibilities include analyzing GNSS time series, evaluating the Least Squares Collocation time-series technique for separating GNSS data white and
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Earthquake Engineering Research Center. Some travel to stakeholder meetings will be required. Additional travel to partners or for conferences is possible. Required Qualifications: · Ph.D. in engineering
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fault mechanics, as well as earthquake hazards; (b) Volcanology: geochemistry, physical volcanology, igneous petrology, and volcanic systems modeling; (c) Climate science: glaciology, paleoclimate and
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to the ERC-PoC project NOSHAKE (a New paradigm fOr forecaSting injection-induced eartHquAKEs), funded by the European Research Council (ERC, https://erc.europa.eu/ ). The candidate will perform her/his
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Engineering Earthquake Research (CCEER), which houses advanced earthquake simulation equipment like shake tables and a large-scale structures lab and the Cybersecurity Center, focusing on protecting information
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open science, peer and student mentoring, reproducible workflows, and collaborative tools. The project’s scope includes event detection and classification (earthquakes, landslides, lahars, glacier motion
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of investigation include: Earthquake seismology: detection, characterization, and location of regional/local earthquakes and tectonic tremor, with implications for the Cascadia megathrust and Axial Seamount
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perturbations of the geyser system. External drivers to be assessed are earthquakes and the tides, while internal drivers will be assessed based on pressure and temperature loggers inside the conduit and
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earthquakes using Music information retrieval separation. Based on this data, a tremor location approach using seismic amplitudes and phases will be developed. Finally, tremor source locations will be