Dr. Chandra Prakash Dubey

Scientist C, Crustal Processes (CrP)

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Phone(Off) : 0471- 2511635

Fax : 0471-2442280


  1. Dubey, C. P., and Tiwari, V. M., Moho variation and upper crustal structure along passive continental margin of Western Ghats, India: constraints from gravity, gravity gradients and topography data. Journal of Geological Society of India, Vol. 92, Nov 2018, pp. 517-522.
  2. Dubey, C. P., Tiwari, V. M., and Rama Rao, P., Insights into the lurking structures and intraplate earthquake in the region of Bay of Bengal using gravity and full gravity gradient tensor. Pure and Applied Geophysics, https://doi.org/10.1007/s00024-017-1661-4
  3. Dubey, C. P., Tiwari, V. M., and Rama Rao, P., Imaging of concealed structures beneath thick sedimentary fan in the region of Bay of Bengal. SEG Technical Program Expanded Abstracts 2017: pp. 5305-5307.
  4. Gupta, H. et al., (Dubey, C. P.: 22nd author out of 29), Investigations of continued reservoir triggered seismicity at Koyna, India. Geological Society, London, Special Publications, 445, http://doi.org/10.1144/SP445.11
  5. Dubey, C. P., and Tiwari, V. M., Computation of gravity field and its gradient: some applications; Computer and Geosciences, doi:10.1016/j.cageo.2015.12.007.
  6. Dubey, C. P., Gotze, H. J., Schmidt, S., Tiwari, V. M., 2014, A 3D model of the Wathlingen salt dome in the Northwest German Basin from joint modeling of gravity, gravity gradient, and curvature. Interpretation, Vol. 2, No. 4, p. 1-13, doi: 10.1190/INT-2014-0012.1.
  7. Gupta, H. et al. (Dubey, C. P.: 17th author out of 27), Investigations related to scientific deep drilling to study reservoir-triggered earthquakes at Koyna, India, International Journal of Earth Sciences, DOI 10.1007/s00531-014-1128-0.

Technical Reports:

  1. Tiwari, V. M., Singh, B., Sain, K., Dubey, C. P., Yadav, R., 3D Lithospheric structure of Andaman Subduction zone. Final report submitted to Ministry of Earth Science (MoES).
  2. Singh, B. Tiwari, V.M. Dubey, C. P. Yadav, R., 2012, Crustal density structure across the Central Indian Shear Zone, G-M studies in the western India and parts of Ganga basin, G-M studies over Dharwar Craton. Annual Report, CSIR-NGRI, Hyderabad, India.