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Geodynamics

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(Top Panel) Thin section from experiment on deformation of partially molten rocks representative of the Earth's upper mantle.  Experiment shows that melt (dark regions) may organize into melt-rich networks, substantially changing the nature of the deformation.  (Bottom) Numerical model of porosity development during shear deformation, in an approximate simulation of the deformation experiment from the top panel.  Red depicts regions of high porosity (melt), while blue colors depict melt-free regions.  For full details of this experiment, see Katz et al., Nature, 676-679, 2006.

 

 

 

 

 

 

Geodynamics research in SG&T is focused on understanding the forces that drive deformation and tectonism in the solid Earth, and the role that rock rheology, physical state (solid or partially molten), and composition play in controlling such deformation.  The techniques include computational and laboratory studies of deformation and melt migration, and the application of observational geodetic and seismic techniques to probe these processes at the field scale.  SG&T's geodynamicists collaborate closely with colleagues in Deep Earth Structure and Earthquake Faulting, as well as geodynamics researchers in Lamont's MG&G and Geochemistry divisions.

Faculty and Scientists
James Gaherty, Doherty Research Scientist
Ben Holtzman, Doherty Associate Research Scientist
Mikhail Kogan, Doherty Research Scientist
William Menke, Professor, Earth and Environmental Sciences
Meredith Nettles, Assistant Professor, Earth and Environmental Sciences
Leonardo Seeber, Doherty Senior Research Scientist
Marc Spiegelman, Associate Professor, Earth and Environmental Sciences
Grigory Steblov, Adjunct Research Scientist
Spahr Webb, Palisades Geophysical Institute Senior Research Scientist
 
Graduate Students
Martin Collier
Ethan Coon

 

 

 
Highlights
Center for Hazards and Risk Research
Lamont-Doherty Cooperative Seismographic Network
The Global Centroid-Moment-Tensor (CMT) Project

 

 
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