V014:
Geological Reactive Systems from the Mantle to the Abyssal Sub-seafloor

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Session ID#: 24113

Session Description:
Understanding the processes controlling the transport of magmas and hydrothermal fluids through the oceanic lithosphere, and their feedbacks on its physical, rheological, magnetic and chemical properties, and habitability is crucial to comprehend the Earth system over time. This session focusses on the physical, hydrodynamic and geochemical mechanisms controlling mass and energy transfers during the formation and cooling of the lithosphere, from mid-oceanic spreading ridges to subduction zones with linkages and feedbacks between processes and the implications for Earth’s geodynamics, global geochemical cycle (including carbon and other volatile elements), life and marine mineral resources in the deep-sea. We encourage contributions on geological, geochemical and biological processes active at mid-oceanic ridge spreading centers and, more generally, in the oceanic lithosphere, from the observation of natural systems (e.g., ophiolitic complexes, dredged and drilled material from the oceanic mantle and crust), geophysics, flow and thermodynamic modeling and experimental works.
Primary Convener:  Marguerite Godard, University of Montpellier II, Montpellier Cedex 05, France
Conveners:  Wolfgang Bach, University of Bremen, Bremen, Germany and Suzanne A McEnroe, Norwegian University of Science and Technology, Trondheim, Norway
Co-Organized with:
Volcanology, Geochemistry and Petrology, Biogeosciences, Geomagnetism, Paleomagnetism and Electromagnetism, and Tectonophysics

Cross-Listed:
  • B - Biogeosciences
  • GP - Geomagnetism, Paleomagnetism and Electromagnetism
  • T - Tectonophysics

Abstracts Submitted to this Session:

Julie Noël1, Marguerite Godard1, Isabelle Martinez2, Emilien Oliot1, Morgan Williams3, Olivier Rodriguez4, Carine Chaduteau2 and Philippe Gouze5, (1)Géosciences Montpellier, Montpellier Cedex 05, France, (2)Institut de Physique du Globe de Paris, Paris, France, (3)Australian National University, Canberra, ACT, Australia, (4)Voxaya SAS, Montpellier, France, (5)CNRS, Montpellier CEDEX 5, France
Kristina Dunkel1, Håkon Austrheim1, Oliver Plümper2, Benoit Ildefonse3, Markus Ohl2 and Bjørn Jamtveit1, (1)University of Oslo, Oslo, Norway, (2)Utrecht University, Utrecht, Netherlands, (3)CNRS, Montpellier, France
Elisabetta Rampone1, Giulio Borghini2, Cornelia Class3, Steven L Goldstein4, Yue Cai3, Anna Cipriani3,5, Alberto Zanetti6 and Albrecht W Hofmann3,7, (1)University of Genoa, Genoa, Italy, (2)University of Milano, Milano, Italy, (3)Lamont -Doherty Earth Observatory, Palisades, NY, United States, (4)Columbia University, Sparkill, NY, United States, (5)University of Modena and Reggio Emilia, Modena, Italy, (6)CNR, Pavia, Italy, (7)Max Planck Institute for Chemistry, Mainz, Germany
Valentin Basch1, Elisabetta Rampone1, Laura Crispini1, Carlotta Ferrando2, Benoit Ildefonse3 and Marguerite Godard2, (1)University of Genoa, Genoa, Italy, (2)Géosciences Montpellier, Montpellier Cedex 05, France, (3)CNRS, Montpellier, France
Patrizia Fumagalli1, Giulio Borghini1, Elisabetta Rampone2 and Stefano Poli3, (1)University of Milano, Milano, Italy, (2)University of Genoa, Genoa, Italy, (3)Universita'' di Milano, Milano, Italy
Giulio Borghini, University of Milano, Milano, Italy, Patrizia Fumagalli, ARRAY(0xf3ffd9c), Milano, Italy and Elisabetta Rampone, University of Genoa, Genoa, Italy