Regional gravity anomaly map with contour interval of 0.1 mGal.

Geological Examples of the Flexure Model of Isostasy (Chapter 4) - Isostasy and Flexure of the Lithosphere

William MOHANTY, Ph.D., Indian Institute of Technology Kharagpur, Kharagpur, IIT KGP, Department of Geology & Geophysics

PDF) Integrated geological and geophysical studies for delineation of chromite deposits: A case study from Tangarparha, Orissa, India

Residual gravity anomaly map of the study area. Contour interval is 0.1

0.academia-photos.com/attachment_thumbnails/830356

Surajit MISRA, Assistant Professor, Ph.D., Gauhati University, Guwahati, G.U., Department of Geological Sciences

Shashi SHARMA, Professor, Ph.D., Indian Institute of Technology Kharagpur, Kharagpur, IIT KGP, Department of Geology & Geophysics

Surajit MISRA, Assistant Professor, Ph.D., Gauhati University, Guwahati, G.U., Department of Geological Sciences

a) Bouguer gravity anomaly map of the study area. (b) Residual gravity

Bouguer anomaly - Wikipedia

Saibal GUPTA, Ph.D. (University of Cambridge, U.K.), Indian Institute of Technology Kharagpur, Kharagpur, IIT KGP, Department of Geology & Geophysics

Dynamics and Impacts of the North Pacific Eddy-Driven Jet Response to Sudden Stratospheric Warmings in: Journal of Climate Volume 36 Issue 3 (2023)

Saibal GUPTA, Ph.D. (University of Cambridge, U.K.), Indian Institute of Technology Kharagpur, Kharagpur, IIT KGP, Department of Geology & Geophysics

Exploring the Application of Potential Field Gravity Method in Characterizing Regional-trends of the Earth's Sequence System over the Sokoto Basin, NW, Nigeria

Gravity study of the Douala sub-basin (Cameroon) using Euler 3D deconvolution, source edge detection (SED) and special function analysis