3D Elastic Full Waveform Inversion of Teleseismic Data for High-resolution Ospheric Imaging
- Others:
- Géoazur (GEOAZUR 6526) ; Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (1965 - 2019) (UNS) ; COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur ; COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)
- Institut des Sciences de la Terre (ISTerre) ; Université Joseph Fourier - Grenoble 1 (UJF)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement [IRD] : UR219-PRES Université de Grenoble-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)
- Géoazur (GEOAZUR 7329) ; Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur ; COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])
- Equations aux Dérivées Partielles (EDP) ; Laboratoire Jean Kuntzmann (LJK) ; Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)
- Department of Earth Sciences [Oxford] ; University of Oxford [Oxford]
- Unité de recherche Géochimie des Sols et des Eaux (URGSE) ; Institut National de la Recherche Agronomique (INRA)
- State Key Laboratory of Lithospheric Evolution (SKL) ; Institute of Geology and Geophysics [Beijing] (IGG) ; Chinese Academy of Sciences [Beijing] (CAS)-Chinese Academy of Sciences [Beijing] (CAS)
Description
We present a 3D time-domain target-oriented elastic full-waveform inversion method well-adapted to the reconstruction of lithospheric images from passive teleseismic data. In teleseismic configurations, sources no longer correspond to point sources embedded in the lithospheric target but rather correspond to a nearly plane wavefronts generated by distant Earthquake incoming from the outside of the targeted medium. To save computation time and apply FWI in the lithospheric target, we follow a two steps strategy based on grid-injection technics. First, wavefields generated by earthquake are propagated in axisymmetric global Earth model with AxiSEM to be stored on the target boundaries. Then, these wawefields are injected within the lithospheric medium and propagated with a spectral element method. We efficiently compute the gradient of the misfit function with the adjoint-state method in time domain. We assess the feasibility of the method on two synthetic models: a cubic inclusion and a realistic lithospheric model representative of the Western Alps. Preliminary results suggest that, despite a weak number of sources and a a coarse aperture illumination, our FWI implementation succeed in reconstructing the initial model thanks to the contribution of both forward and backward scattering regimes.
Abstract
International audience
Additional details
- URL
- https://hal.archives-ouvertes.fr/hal-02009483
- URN
- urn:oai:HAL:hal-02009483v1
- Origin repository
- UNICA