Physics
Scientist
Department of Geological Sciences, Brown University, Providence, Rhode Island, USA
Department of Geological Sciences, Brown University, Providence, RI, USA
Department of Geology and Mineralogy, University of Oxford, Oxford OXI 3PR Great Britain
Department of Geological Sciences, Brown University, Providence, RI 02912, USA
Brown University, Providence, RI, US
Brown Univ., Providence, RI, US
Brown University
Department of Geological Sciences, Brown University, 02912, Providence, RI, USA
Brown University, Providence, RI
Department of Geology and Mineralogy, University of Oxford, Oxford Great Britain
Brown Univ., Providence, RI.
Department of Geological Sciences, Brown University, Providence, RI 02912, USA Sciences, Brown University, 324 Brook St., Providence, RI 02192, USA OF GEOLOGICAL SCIENCES, BROWN UNIV., PROVIDENCE, RI 02919
Lamont-Doherty Earth Observatory, Palisades, NY, US
Department of Geological Sciences, Brown University, Providence, RI 02912 USA
Brown University, Providence, R.I.
Paris Univ., France
Brown University, Providence RI
Department of Geological Sciences, Brown University, Box 1846, Providence, RI 02910, USA
Brown University, Box 1846, Providence, RI 02912
Geological Dept., Brown University, Box 1846, Providence, RI 02912
Department of Geological Sciences, Brown University, Box 1846, Providence, RI 02912
Scripps Inst. of Oceanography, La Jolla, CA, US
Brown University, Providence, Rhode-Island, USA
Department of Geological Science, Brown University, 02912, Providence, RI, USA
Geological Sciences, Brown University, 324 Brook Street, Providence, RI 02912, USA
Department of Geological Sciences, Brown University, Providence, Rh
A community benchmark for subduction zone modeling
A dynamic origin for the global asymmetry of lunar mare basalts
A Finite Amplitude Necking Model for the Formation and Evolution of Rift Zones: Application to the Beta Regio Rift
A geometric analysis of surface deformation - Implications for the tectonic evolution of Ganymede
A high-order numerical study of reactive dissolution in an upwelling heterogeneous mantle—I. Channelization, channel lithology and channel geometry
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