V019
Magmatic and Hydrothermal Processes at Mid-Ocean Ridges
Magmatic and Hydrothermal Processes at Mid-Ocean Ridges
Session ID#: 249158
Session Description:
Mid-ocean ridges are dynamic systems where magmatic, hydrothermal, and biological processes interact. They are key sites of oceanic lithosphere formation and heat and mass transfer between the Earth’s interior and the oceans. Submarine volcanoes and hydrothermal vents with associated ecosystems play a critical role in global chemical evolution and biogeochemical cycles. This session seeks to foster discussion across disciplines to advance our understanding of mid-ocean ridge processes from a variety of approaches. We invite contributions that explore the interplay between seafloor magmatism, hydrothermal activity, and biological systems across temporal and spatial scales. Interdisciplinary studies that integrate field measurements, laboratory experiments, numerical modeling, and geochemical analyses are welcome. Contributions highlighting new data from ocean drilling expeditions, ocean observatories, and geophysical instrumentation networks, especially those focused on active ridge volcanism, hydrothermalism, serpentinization and hydrogen gas generation, and carbonate mineral formation in ultramafic rocks and carbon sequestration are particularly encouraged.
Co-Sponsor(s):
- B - Biogeosciences
- OS - Ocean Sciences
- S - Seismology
- T - Tectonophysics
Index Terms:
3017 Hydrothermal systems [MARINE GEOLOGY AND GEOPHYSICS]
3035 Midocean ridge processes [MARINE GEOLOGY AND GEOPHYSICS]
3075 Submarine tectonics and volcanism [MARINE GEOLOGY AND GEOPHYSICS]
Primary Convener: Qi Fu, University of Houston, Department of Earth and Atmospheric Sciences, Houston, TX, United States
Convener: Karen G Bemis, Rutgers, The State University of New Jersey - New Brunswick, Marine and Coastal Sciences, New Brunswick, United States
See more of: Volcanology, Geochemistry and Petrology