Stratigraphy and correlations in Deccan Volcanic Province, India: quo vadis?
VS Kale, G Dole, P Shandilya, K Pande - GSA Bulletin, 2020 - pubs.geoscienceworld.org
Abstract The Deccan Volcanic Province (DVP) is significant for its eruption close to
Cretaceous–Paleogene (K-Pg) boundary. Chemostratigraphy established in its western …
Cretaceous–Paleogene (K-Pg) boundary. Chemostratigraphy established in its western …
The Deccan Volcanic Province (DVP), India: a review: Part 1: Areal extent and distribution, compositional diversity, flow types and sequences, stratigraphic …
P Krishnamurthy - Journal of the Geological Society of India, 2020 - Springer
Abstract The Deccan Volcanic Province (DVP), covering presently an area of 0.5 million km
2, and estimated to be 2–3 times larger during the Upper Cretaceous-Paleocene, is one of …
2, and estimated to be 2–3 times larger during the Upper Cretaceous-Paleocene, is one of …
[图书][B] The making of India: geodynamic evolution
KS Valdiya - 2015 - books.google.com
This book presents in a concise format a simplified and coherent geological-dynamical
history of the Indian subcontinent (including Sri Lanka, Bangladesh, Myanmar, Southern …
history of the Indian subcontinent (including Sri Lanka, Bangladesh, Myanmar, Southern …
Determination of rapid Deccan eruptions across the Cretaceous‐Tertiary boundary using paleomagnetic secular variation: Results from a 1200‐m‐thick section in the …
AL Chenet, F Fluteau, V Courtillot… - Journal of …, 2008 - Wiley Online Library
Flow‐by‐flow reanalysis of paleomagnetic directions in two sections of the Mahabaleshwar
escarpment, coupled with analysis of intertrappean alteration levels shows that volcanism …
escarpment, coupled with analysis of intertrappean alteration levels shows that volcanism …
U-Pb zircon age constraints on the earliest eruptions of the Deccan Large Igneous Province, Malwa Plateau, India
Climate instability driven by emission of volatiles during emplacement of large igneous
provinces (LIPs) is frequently invoked as a potential cause of mass extinctions. However …
provinces (LIPs) is frequently invoked as a potential cause of mass extinctions. However …
[HTML][HTML] Developments in the stratigraphy of the Deccan Volcanic Province, peninsular India
Abstract The Deccan Volcanic Province has been considered as one of the largest
magmatic regions, involving an aerial coverage of ca. 500,000 km 2. It is subdivided into four …
magmatic regions, involving an aerial coverage of ca. 500,000 km 2. It is subdivided into four …
Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian)
The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-
Pg) transition are a matter of ongoing debate. While there is a general consensus regarding …
Pg) transition are a matter of ongoing debate. While there is a general consensus regarding …
Trace elemental and Nd-Sr-Pb isotopic compositional variation in 37 lava flows of the Mandla lobe and their chemical relation to the western Deccan stratigraphic …
JP Shrivastava, JJ Mahoney, MR Kashyap - Mineralogy and Petrology, 2014 - Springer
The Mandla lobe is a 900 m thick lava pile that forms a 29,400 km 2 northeastern extension
of the Deccan Traps. Earlier, combined field, petrographic, and major element studies have …
of the Deccan Traps. Earlier, combined field, petrographic, and major element studies have …
Cretaceous volcanism in Peninsular India: Rajmahal–Sylhet and Deccan Traps
VS Kale - Geodynamics of the Indian Plate: Evolutionary …, 2020 - Springer
Abstract The Indian Peninsula hosts Cretaceous continental flood basalts (CFB) that
manifest its passage over the Kerguelen and Reunion hotspots in succession. The former …
manifest its passage over the Kerguelen and Reunion hotspots in succession. The former …
Chemical evolution, petrogenesis, and regional chemical correlations of the flood basalt sequence in the central Deccan Traps, India
L Melluso, M Barbieri, L Beccaluva - Journal of Earth System Science, 2004 - Springer
The lava sequence of the central-western Deccan Traps (from Jalgaon towards Mumbai) is
formed by basalts and basaltic andesites having a significant variation in TiO 2 (from 1.2 to …
formed by basalts and basaltic andesites having a significant variation in TiO 2 (from 1.2 to …