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Earth Science

D-Index
38
Citations
8305
World Ranking
6347
National Ranking
664

Overview

Shamita Das is affiliated with the University of Oxford in the United Kingdom. Their research focuses primarily on Earth and Planetary Sciences, with a significant emphasis on the subfield of Geophysics.

Their work covers several main topics within geophysics, including:

  • Earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Earthquake Detection and Analysis
  • Seismic Imaging and Inversion Techniques

Each of these topics reflects a distinct aspect of geophysical research, highlighting investigations into the mechanisms and properties associated with earthquakes and tectonic movements, as well as the behavior of materials under high pressure conditions.

Although detailed information about recent papers, co-authors, or frequent publication venues is not listed, the focus areas suggest that their contributions likely involve analytical and imaging methodologies in seismology and tectonics. This includes exploring seismic data and inversion techniques, which are critical for understanding Earth's internal processes and dynamics.

Best Publications

  • Rupture Process of the 2004 Sumatra-Andaman Earthquake

    Charles J. Ammon;Chen Ji;Hong-Kie Thio;David Robinson

  • Fault plane with barriers: A versatile earthquake model

    Shamita Das;Keiiti Aki

  • A numerical study of two-dimensional spontaneous rupture propagation

    Shamita Das;Keiiti Aki

  • Theory of time-dependent rupture in the Earth

    S. Das;C. H. Scholz

  • Source mechanism of volcanic tremor: fluid-driven crack models and their application to the 1963 kilauea eruption

    Keiiti Aki;Mike Fehler;Shamita Das

  • Earthquake source mechanics

    Shamita Das;John Boatwright;C. H. Scholz

  • Off-fault aftershock clusters caused by shear stress increase?

    Shamita Das;Christopher H. Scholz

  • Principles of Earthquake Source Mechanics

    B. V. Kostrov;Shamita Das

  • Spatial relation between main earthquake slip and its aftershock distribution

    S. Das;C. Henry

  • Why large earthquakes do not nucleate at shallow depths

    Shamita Das;C. H. Scholz

  • An enhanced image of the Pamir–Hindu Kush seismic zone from relocated earthquake hypocentres

    G. Pegler;S. Das

  • Aftershock zones of large shallow earthquakes: fault dimensions, aftershock area expansion and scaling relations

    C. Henry;S. Das

  • Inversion for seismic slip rate history and distribution with stabilizing constraints: Application to the 1986 Andreanof Islands Earthquake

    Shamita Das;B. V. Kostrov

  • Aseismic zone and earthquake segmentation associated with a deep subducted seamount in Sumatra

    Satish C. Singh;Nugroho Hananto;Maruf Mukti;David P. Robinson

  • Earthquake Rupture Stalled by a Subducting Fracture Zone

    D. P. Robinson;S. Das;A. B. Watts

  • Faulting characteristics of supershear earthquakes

    Michel Bouchon;Hayrullah Karabulut;Marie-Paule Bouin;Jean Schmittbuhl

  • Three‐dimensional spontaneous rupture propagation and implications for the earthquake source mechanism

    Shamita Das

  • A numerical method for determination of source time functions for general three‐dimensional rupture propagation

    Shamita Das

  • Simultaneous Rupture Along Two Conjugate Planes of the Wharton Basin Earthquake

    D. P. Robinson;C. Henry;S. Das;J. H. Woodhouse

  • The great March 25, 1998, Antarctic Plate earthquake: Moment tensor and rupture history

    C. Henry;S. Das;J. H. Woodhouse

  • Earthquake Source Mechanics: Das/Earthquake Source Mechanics

    Shamita Das;John Boatwright;Christopher H. Scholz

Frequent Co-Authors

Christopher H. Scholz
Christopher H. Scholz Lamont-Doherty Earth Observatory
Keiiti Aki
Keiiti Aki University of Southern California
Peter Suhadolc
Peter Suhadolc University of Trieste
Raul Madariaga
Raul Madariaga École Normale Supérieure
Michel Bouchon
Michel Bouchon Centre national de la recherche scientifique, CNRS
Anthony Watts
Anthony Watts University of Oxford
John Boatwright
John Boatwright United States Geological Survey
Sidao Ni
Sidao Ni Chinese Academy of Sciences
Martin Vallée
Martin Vallée Institut de Physique du Globe de Paris

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