Magali Collin

ORCID: 0000-0003-3683-7980
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About
Contact & Profiles
Research Areas
  • earthquake and tectonic studies
  • Seismic Waves and Analysis
  • Geological and Geophysical Studies Worldwide
  • Seismic Imaging and Inversion Techniques
  • Seismology and Earthquake Studies
  • Geological Modeling and Analysis
  • Geological formations and processes
  • Underwater Acoustics Research
  • Geological and Geophysical Studies
  • Aerodynamics and Acoustics in Jet Flows
  • Voice and Speech Disorders
  • Flood Risk Assessment and Management
  • Landslides and related hazards
  • Geophysics and Sensor Technology
  • Geology and Paleoclimatology Research
  • Ear Surgery and Otitis Media
  • Geological and Tectonic Studies in Latin America
  • Nasal Surgery and Airway Studies
  • High-pressure geophysics and materials
  • Geological and Geochemical Analysis
  • Earthquake Detection and Analysis

Total (France)
2018-2022

Passive Seismic is a broad term, incorporating various techniques and methodologies, which all exploit some part of the seismic signal that naturally exists or occurs in Earth’s subsurface. This may differ significantly form and/or provenance (e.g. earthquakes, ambient noise, etc.), as well frequency content and, subsequently, subspace on it carry useful information.

10.3997/1365-2397.n0085 article EN First Break 2018-04-01

ABSTRACT During the large-N MAUPASACQ passive seismic experiment in foreland of western Pyrenees (southwest France), an unusual swarm-type sequence was serendipitously recorded a normally quiet area. Thanks to density deployment and proximity all events, it possible relocate hypocenters with very good relative accuracy through template matching, cross-correlation phase picks, double-difference algorithm. The four-month activity consists more than 600 events local magnitudes ranging between...

10.1785/0120220263 article EN Bulletin of the Seismological Society of America 2023-06-14

<p>Horizontal-to-Vertical Spectral Ratios (HVSR) and Rayleigh group velocity dispersion curves (DC) can be used to estimate the shallow S-wave (Vs) structure. Knowing Vs structure is important for geophysical data interpretation either in order better constrain inversions P-wave (Vp) structures such as travel time tomography or full waveform inversions, directly study geo-engineering purposes (e.g. ground motion prediction). The purpose of this appraise particular how much...

10.5194/egusphere-egu2020-13681 article EN 2020-03-10
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