Announcement of Union Session, Fall AGU Meeting 2000


PLATE-MANTLE INTERACTION AND FORCES THAT MOVE PLATES

In its original form, plate tectonics describes the motion of rigid plates over the deeper mantle. Plates were assumed to be essentially decoupled from the deeper mantle by the asthenosphere, driven mainly by slab pull and ridge push (i.e., forces acting on the sides of the plates) and resisted slightly by basal drag. This assumption recently has attained increased attention with the suggestion that basal drag may be an important plate driving mechanism. This session focuses on the kinematic and dynamic nature of the coupling between lithospheric plates and underlying mantle, and on which forces drive the plates.

Conveners: Götz Bokelmann, Department of Geophysics, Stanford University, Stanford, CA 943025-2215, tel. (650) 725-9181, fax (650) 725-7344, goetz@alumni.princeton.edu; Eugene Humphreys, Department of Geology, University of Oregon, Eugene, OR 97403, tel. (503) 346-5575, fax (503) 346-4692, gene@newberry.uoregon.edu.

The sessions will be held on Sunday, December 17, 2000, with an oral session in the morning (U71a), and a poster session in the afternoon (U72a).


Program Session Union U71A (Sunday Morning)

"Plate-Mantle Interaction and Forces That Move Plates", I Oral Part, Room MC 135, Conveners: G. Bokelmann, E. Humphreys


Session Program U72A (Sunday Afternoon)

"Plate-Mantle Interaction and Forces That Move Plates II Posters",Location MC Hall D, Conveners: G. Bokelmann, E. Humphreys


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