3 Tectonosedimentary Process Interaction at Global Ocean Margins: Holistic Strategies for Earth System Modelling–I
Monday, 25 June 2001
10:00 AM - 12:30 PM
GEOLOGICAL RESEARCH ON OCEAN MARGINS: TRENDS AND POSSIBILITIES
Paper number: 3-2
Program: THEME SESSIONS
Time: 10:05 AM – 10:35 AM
Authors
Abstract
The deliberations also focused on the important questions that need to be resolved by the marine geological community on the convergent and passive margins given the realization that ocean margins evolve through a complex interaction of mechanical, chemical, biological and fluid processes. These processes over time accumulate most of the Earth’s valuable resources. Also, most of the world’s principal geological hazards converge at the margins, the site of the greatest population density. To understand the evolution of the continental margins several broad processes need first to be understood: the deformation of the lithosphere and strain partitioning within the crust and upper mantle; heat and mass transfer associated with subduction that lead to production of magma and the role of fluid flow on this system; the relationships between small-scale physical events and the formation of longer-term sedimentary record; and the role of fluid circulation through sediments and igneous rocks at active and passive margins.
The results of these deliberations, steps undertaken in the US to realize these research goals in collaboration with the international scientific community and the important role that the next phase of Ocean Drilling (the IODP) will play in the ocean margins research will be highlighted during this presentation.