Dear Colleagues,
Session Description:
The rheology of Earth's upper mantle determines its deformation in response to evolving stress at time-scales ranging from seconds (seismic waves) to millions of years (mantle convection). A holistic, multiscale understanding of mantle rheology is therefore
necessary to describe geophysical observations probing plate tectonic processes at various length and time-scales. Laboratory experiments on mantle materials have quantified microphysical mechanisms that impact anelastic and viscous deformation. This has enabled
insights into the thermo-mechanical state of the mantle from geophysical observations, and geodynamic models that employ more realistic mantle rheologies.
We invite contributions that integrate geophysical observations (e.g., seismic velocity, anisotropy, attenuation), laboratory experiments on mantle materials, and/or geodynamic modeling to better constrain upper-mantle rheology. This includes studies that address
discrepancies between observations and experimental predictions, explore the role of partial melt, volatiles, and compositional heterogeneity on rheology, or develop new frameworks for translating geophysical/petrological observations into mechanical properties.
Invited Presenters:
Thomas Breithaupt (University of Cambridge)
TBD
Conveners:
Josh Russell (Syracuse University)
Diede Hein (RWTH Aachen University)
Fred Richards (Imperial College London)
Zhuoran Zhang (Michigan State University)
Sincerely,
Josh, Diede, Fred, Zhuoran
Joshua Russell (he/him)
Assistant Professor
Department of Earth and Environmental Sciences
Syracuse University