Ambient Seismic Noise Imaging of the Lowermost Mantle Beneath the North Atlantic Ocean

• Published in: Geophysical Journal International
• Main Authors: Retailleau, Lise, Boué, Pierre, Li, Lei, Campillo, Michel
• Other Authors: Observatoire Volcanologique du Piton de la Fournaise (OVPF), Institut de Physique du Globe de Paris (IPG Paris), Institut des Sciences de la Terre (ISTerre), Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Gustave Eiffel-Université Grenoble Alpes (UGA)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2020
• Subjects: Ambient noise correlations; body waves; Core-Mantle-Boundary; [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]; North Atlantic
• Online Access: https://hal.univ-grenoble-alpes.fr/hal-02928287; https://hal.univ-grenoble-alpes.fr/hal-02928287/document; https://hal.univ-grenoble-alpes.fr/hal-02928287/file/25.%20Geophysical%20Journal%20International%20%7C%20AM%20manuscrit%20Retailleau_et_al%202020.pdf; https://doi.org/10.1093/gji/ggaa210

International audience Body waves can be extracted from correlation functions computed from seismic records even at teleseismic distances. Here we use P and PcP waves from the secondary microseism frequency band that are propagating between Europe and the Eastern United States to image the core–mantle boundary (CMB) and D” structure beneath the North Atlantic. This study presents the first 3-D image of the lower mantle obtained from ocean-generated microseism data. Robustness of our results is evaluated by comparing images produced by propagation in both directions. Our observations reveal complex patterns of lateral and vertical variations of P-wave reflectivity with a particularly strong anomaly extending upward in the lower mantle up to 2600 km deep. We compare these results with synthetic data and associate this anomaly to a Vp velocity increase above the CMB. Our image aims at promoting the study of the lower mantle with microseism noise excitations.