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Pawan Dewangan

Researcher at National Institute of Oceanography, India

Publications -  87
Citations -  1839

Pawan Dewangan is an academic researcher from National Institute of Oceanography, India. The author has contributed to research in topics: Clathrate hydrate & Gas hydrate stability zone. The author has an hindex of 21, co-authored 85 publications receiving 1489 citations. Previous affiliations of Pawan Dewangan include Indian Institute of Technology Kharagpur & Colorado School of Mines.

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A Cenozoic record of the equatorial Pacific carbonate compensation depth

Heiko Pälike, +70 more
- 30 Aug 2012 - 
TL;DR: A carbonate accumulation record that covers the past 53 million years from a depth transect in the equatorial Pacific Ocean is presented and large superimposed fluctuations in carbonate compensation depth are found during the middle and late Eocene.
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Inversion of multicomponent, multiazimuth, walkaway VSP data for the stiffness tensor

TL;DR: In this paper, Horne and Leaney proved the feasibility of joint inversion of the slowness and polarization vectors for parameters of transversely isotropic media with a vertical symmetry axis (VTI symmetry).
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Physical modeling and analysis of P-wave attenuation anisotropy in transversely isotropic media

TL;DR: In this article, the spectral-ratio method was used to estimate the group effective attenuation coefficient of P-waves transmitted through the sample for a wide range of propagation angles from 0° to 90° with the symmetry axis.
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Evidence of paleo–cold seep activity from the Bay of Bengal, offshore India

TL;DR: In this article, the authors reported evidence of paleo-cold seep associated activities, preserved in methane-derived carbonates in association with chemosynthetic clams (Calyptogena sp) from a sediment core in the Krishna-Godavari basin, Bay of Bengal.
MonographDOI

Expedition 320/321 summary.

TL;DR: The Pacific Equatorial Age Transect (PEAT) as discussed by the authors was designed to recover a continuous Cenozoic record of the equatorial Pacific by coring above the paleoposition of the Equator at successive crustal ages on the Pacific plate.