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ben holtzmanlamont doherty earth observatory columbia university 61 rt. 9W palisades, new york, 10964 email: benh (at) ldeo.columbia.edu
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My research combines rock physics, seismology and geodynamics.
Through field work, experiments and theory, I have studied the interactions of melt migration and deformation and the influences of melt on the mechanical properties of rocks in the deep Earth.
Currently, my work is focused on the interpretation of seismic velocities measured at plate
boundaries in terms of both rock fabrics and melt distribution, towards building more detailed
images of the structure of plate boundaries and the upper mantle.
Such images provide an observational basis for an explanation of why the Earth has discrete
tectonic plates.
NEW:
Sounds of Seismology (shown at LDEO Open House 2008)
Some illustrations
[1] B.K. Holtzman and D. L. Kohlstedt. Stress-driven Melt Segregation and Strain Partitioning in Partially Molten
Rocks: Effects of Stress and Strain
pdf from J.Pet.
[2] Katz, R. F., M. Spiegelman, and B. Holtzman, (2006) The
dynamics of melt and shear localization in partially molten aggregates, Nature, 442, 676--679,
doi:10.1038/nature05039.
[3] B.K. Holtzman, D.L. Kohlstedt, J.Phipps Morgan. Viscous Energy Dissipation and Strain Partitioning in
Partially Molten Rocks.
pdf from J.Petrology
[4] J.Phipps Morgan and B.K. Holtzman. Melt transport and deformation of partially molten viscoelastic
rocks: the Vug Wave.
pdf
[5] B.K. Holtzman, D.L. Kohlstedt, M.E. Zimmerman, F. Heidelbach, T. Hiraga, and J. Hustoft. Melt
segregation and strain partitioning: Implications for seismic anisotropy and mantle flow,
pdf
[6] B. K. Holtzman, M. E. Zimmerman, N. J. Groebner, S. B. Ginsberg, and D. L. Kohlstedt.
Stress-driven melt segregation in partially molten rocks.
pdf