Katalog Plus
Bibliothek der Frankfurt UAS
Bald neuer Katalog: sichern Sie sich schon vorab Ihre persönlichen Merklisten im Nutzerkonto: Anleitung.
Dieses Ergebnis aus BASE kann Gästen nicht angezeigt werden.  Login für vollen Zugriff.

Mapping the geometry of volcanic systems with magnetotelluric soundings: results from a land and marine magnetotelluric survey performed during the 2018-2019 Mayotte seismovolcanic crisis

Title: Mapping the geometry of volcanic systems with magnetotelluric soundings: results from a land and marine magnetotelluric survey performed during the 2018-2019 Mayotte seismovolcanic crisis
Authors: Darnet, Mathieu; Wawrzyniak, Pierre; Tarits, Pascal; Hautot, Sophie; d'Eu, Jean-François
Contributors: Bureau de Recherches Géologiques et Minières (BRGM); Laboratoire Géosciences Océan (LGO); Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO EPE)-Centre National de la Recherche Scientifique (CNRS); IMAGIR Sarl; MAPPEM Geophysics SAS
Source: 25th EM Induction Workshop; https://brgm.hal.science/hal-03693765; 25th EM Induction Workshop, Sep 2022, Çeşme, Turkey; https://emiw2022.emiw.org/
Publisher Information: CCSD
Publication Year: 2022
Collection: Université de Bretagne Occidentale: HAL
Subject Terms: magnetotelluric; electrical resistivity; seismovolcanic; geothermal; [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
Subject Geographic: Çeşme; Turkey
Description: International audience ; A major seismovolcanic crisis has afflicted the islands of Mayotte, Comoros Archipelago, since May 2018, although the origin is debated. Magnetotellurics (MT), which is sensitive to hydrothermal and/or magmatic fluids and can map the subsurface electrical resistivity structure, can provide insight by revealing the internal structure of the volcanic system. In this paper, we report the results of a preliminary land and shallow marine MT survey performed on and offshore the island nearest the crisis. The 3D inversion-derived electrical resistivity model suggests that the island is underlain by a shallow ~500-m-thick conductive layer atop a deeper, more resistive layer, possibly associated with a high-temperature geothermal system. At depths of ~15 km, the resistivity drops by almost two orders of magnitude, possibly due to partial melting. Further petrophysical and geophysical studies are underway for confirmation and to map the geometry and evolution of the volcanic system.
Document Type: conference object
Language: English
Availability: https://brgm.hal.science/hal-03693765; https://brgm.hal.science/hal-03693765v1/document; https://brgm.hal.science/hal-03693765v1/file/Mayotte_MT.pdf
Rights: https://about.hal.science/hal-authorisation-v1/ ; info:eu-repo/semantics/OpenAccess
Accession Number: edsbas.D317CF5A
Database: BASE