3-3-3-3-3-3-3-3-3-3-3-3-3 From: AURELIEN MORDRET <aurelien.mordret@xxxxxxxxxxxxxxxxxxxxxx> Dear Colleagues, We would like to remind you to submit your abstract to session GMPV10.3: " *Interdisciplinary studies of the European intraplate volcanism: origin(s), links with Variscan structures and Cenozoic rift systems, and present activity* ", to be held during EGU 2023 that will take place in Vienna, Austria, 23â??28 April 2023. (https://urldefense.com/v3/__https://meetingorganizer.copernicus.org/EGU23/session/45189__;!!IKRxdwAv5BmarQ!bo5Fs11H08VHtjrfpWEjL24lUqLu5JMQ9M23-WEMVyboqbqa999FTUM3kVyB89CJfMiUvQpR229Ijp85$ <https://urldefense.com/v3/__https://meetingorganizer.copernicus.org/egu23/sessionprogramme*__;Iw!!IKRxdwAv5BmarQ!fpXDOTtaXaiH2fR7RW4zm4zMjlFZugogIPg6sO4cJBqhRGp2PNPTa8SOA6EXle0_J3BtVGGP6hgG9uo_LUtaLdWSb9ITyWWwrRA2jFE$> ). Abstract submission closes on *January 10 at 1 PM CET*. The session accepts abstracts on a wide range of topics to be found within the appended description below. Looking forward to meeting you in Vienna! Kind regards, Aurélien Mordret Torsten Dahm Olivier Vanderhaeghe Magdalena Matusiak-MaÅ?ek ---- Session scope: GMPV10.3 *Interdisciplinary studies of the European intraplate volcanism: origin(s), links with Variscan structures and Cenozoic rift systems, and present activity* The Cenozoïc European intraplate volcanism is temporally and spatially linked with the Alpine-Pyrenean orogeny and spreads from Spain to Romania and Bulgaria. It is associated with widespread extensional rifts systems and local Variscan basement uplifts. Magmatic activity within the European foreland of the Alpine orogen is typically mafic. It occurs in various styles, from monogenetic fields to large stratovolcanoes and fissural basaltic plateaus. Despite the extensive studies in each region, intraplate volcanism and magmatism in Europe are only broadly understood. The current signs of unrest in the Eifel volcanic region (Germany) remind us of the severe natural hazards (e.g., potential VEI 6 eruption of the Laacher See volcano in a populated area) that remain difficult to assess in these dormant regions. In this interdisciplinary session, we welcome geochemical, geological, petrological, geodynamical, and geophysical contributions related to all aspects of the Cenozoïc European intraplate volcanism. We are interested in studies documenting: - The deep processes at the origin of the magmatism - The magmatic plumbing systems from the mantle to volcanoes - The relationship between inherited Variscan structures and emplacement of the different volcanic edifices and their morphology - Approaches and studies to assess the hazard of intraplate volcanic fields We are also welcoming studies focusing on the current crustal and surface expressions of the volcanism, such as CO2 degassing (in lakes, wet springs, and mofettes), regional deformation and uplift, and seismicity. We encourage abstracts on ongoing data acquisition initiatives to further foster discussions on ongoing and future projects. 3-3-3-3-3-3-3-3-3-3-3-3-3 ------------------------------
