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Gérôme Calvès

Researcher at University of Toulouse

Publications -  35
Citations -  1178

Gérôme Calvès is an academic researcher from University of Toulouse. The author has contributed to research in topics: Continental margin & Cretaceous. The author has an hindex of 13, co-authored 35 publications receiving 934 citations. Previous affiliations of Gérôme Calvès include University of Aberdeen & Centre national de la recherche scientifique.

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Correlation of Himalayan exhumation rates and Asian monsoon intensity

TL;DR: In this article, weathering records from the South China Sea, Bay of Bengal and Arabian Sea were used to reconstruct the earliest Neogene climate of the Himalayan orogen and showed a correlation between the rate of Himalayan exhumation and monsoon intensity.
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Seismic volcanostratigraphy of the western Indian rifted margin: The pre‐Deccan igneous province

TL;DR: In this article, an analysis of the offshore segment of the western Indian volcanic large igneous province, between the shoreline and the first magnetic anomaly (An 28 ∼63 Ma), using seismic reflection and potential field data is presented.
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Tectonics of the Deccan Large Igneous Province: an introduction

TL;DR: SoumyaJit MUKHERJEE as discussed by the authors, ACHYUTA AYAN MISRA, GÉRÔME CALVÈS3 & MICHAL NEMOK4,5 Department of Earth Sciences, Indian Institute of Technology Bombay, Mumbai 400 076, Maharashtra, India Exploration, Reliance Industries Ltd., Mumbai 400 701, India Université Toulouse 3, Paul Sabatier, Géosciences Environnement Touloustouse, 14 avenue Edouard Belin, 31400, Toul
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Anomalous subsidence on the rifted volcanic margin of Pakistan: No influence from Deccan plume

TL;DR: The role of hotter than ambient plume mantle in the formation of a rifted volcanic margin in the northern Arabian Sea is investigated using subsidence analysis of a drill site located on the seismically defined Somnath volcanic ridge as mentioned in this paper.
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Giant fossil mass wasting off the coast of West India: The Nataraja submarine slide

TL;DR: The Nataraja Submarine Slide as mentioned in this paper is the second largest passive margin landslide/mass-transport deposit in the world, with a volume of over 330 km long, a maximum of 190 km wide and its run-out basal gradient is 1.2°.