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Lise Retailleau

Researcher at Institut de Physique du Globe de Paris

Publications -  26
Citations -  469

Lise Retailleau is an academic researcher from Institut de Physique du Globe de Paris. The author has contributed to research in topics: Volcano & Geology. The author has an hindex of 7, co-authored 17 publications receiving 247 citations. Previous affiliations of Lise Retailleau include Sorbonne & Stanford University.

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Global quieting of high-frequency seismic noise due to COVID-19 pandemic lockdown measures.

Thomas Lecocq, +84 more
- 11 Sep 2020 - 
TL;DR: The 2020 seismic noise quiet period is the longest and most prominent global anthropogenic seismic noise reduction on record and suggests that seismology provides an absolute, real-time estimate of human activities.
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In situ observations of velocity changes in response to tidal deformation from analysis of the high-frequency ambient wavefield

TL;DR: In this paper, the authors reported systematic seismic velocity variations in response to tidal deformation, and the velocity dependence on strain implies nonlinear behavior, but conclusions regarding elasticity are more ambiguous.
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Locating Microseism Sources Using Spurious Arrivals in Intercontinental Noise Correlations

TL;DR: In this article, the authors proposed to use Rayleigh wave spurious arrivals detected on correlation functions computed between European and United States seismic stations to locate microseism sources in the Atlantic Ocean.
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Mayotte seismic crisis: building knowledge in near real-time by combining land and ocean-bottom seismometers, first results

TL;DR: In this paper, the authors build a new local 1D velocity model and established specific data processing procedures to estimate a low VP/VS ratio that is compatible with a volcanic island context, and manually pick about 125,000 P and S phases on land and sea bottom stations to locate more than 5,000 events between February 2019 and May 2020.
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Ambient seismic noise imaging of the lowermost mantle beneath the North Atlantic Ocean

TL;DR: In this article, the authors used P and PcP waves from the secondary microseism frequency band propagating between Europe and the Eastern United States to image the core-mantle boundary (CMB) and D” structure beneath the North Atlantic.