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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Indian Peninsula
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India
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Deccan Plateau (1)
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Gujarat India (1)
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Rajasthan India
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Barmer India (1)
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Bikaner India (7)
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Jaisalmer India (1)
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Jhunjhunu India (1)
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Jodhpur India (1)
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Indian Ocean Islands
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elements, isotopes
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geologic age
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Cenozoic
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Paleogene
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lower Eocene
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K-T boundary (1)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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K-T boundary (1)
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igneous rocks
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igneous rocks
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volcanic rocks
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basalts
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flood basalts (1)
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Primary terms
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Asia
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Indian Peninsula
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India
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Deccan Plateau (1)
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Gujarat India (1)
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Rajasthan India
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Barmer India (1)
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Bikaner India (7)
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Jaisalmer India (1)
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Jhunjhunu India (1)
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Jodhpur India (1)
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biogeography (2)
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Cenozoic
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Tertiary
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Paleogene
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Eocene
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lower Eocene
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Ypresian (1)
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middle Eocene
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Lutetian (1)
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Paleocene
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lower Paleocene
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K-T boundary (1)
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geochemistry (1)
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ground water (1)
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igneous rocks
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volcanic rocks
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basalts
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flood basalts (1)
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Indian Ocean Islands
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Mascarene Islands
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Reunion (1)
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Invertebrata
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Arthropoda
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Chelicerata
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Arachnida (1)
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-
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Protista
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Foraminifera (1)
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isotopes
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U-238 (1)
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mantle (1)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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K-T boundary (1)
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metals
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actinides
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uranium
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alkali metals
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sodium (1)
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paleoecology (1)
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paleontology (1)
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Plantae
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algae
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Botryococcus (1)
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Spermatophyta
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plate tectonics (1)
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tectonics (1)
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water resources (1)
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rock formations
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Bikaner India
Assessment of Groundwater Quality for Drinking and Irrigation Purpose using Geospatial and Statistical techniques in a Semi-arid Region of Rajasthan, India
An orb-weaver spider (Araneae, Araneidae) from the early Eocene of India
Botryococcus from the early Eocene lignite mines of western India: inferences on morphology, taphonomy and palaeoenvironment
Assessment of Uranium in Correlation with Physico-chemical Properties of Drinking Water of Northern Rajasthan
A New Fossil Leaf of Kleinhovia L. from the Early Eocene of India and its Palaeoclimatic and Phytogeographical Significance
K-T magmatism and basin tectonism in western Rajasthan, India, results from extensional tectonics and not from Réunion plume activity
Evolution of sedimentary basins took place in the Barmer, Jaisalmer, and Bikaner regions during K-T (Cretaceous–Tertiary) time in western Rajasthan, India. These intracratonic rift basins developed under an extensional tectonic regime from Early Jurassic to Tertiary time. Rift evolution resulted in alkaline magmatism at the rift margins. This magmatism is dated at 68.5 Ma and has been considered an early phase of Deccan volcanism. Deccan volcanism, sedimentary basin development, and the alkaline magmatism of western Rajasthan have thus been considered the products of Réunion plume activity. However, sedimentary basin evolution began in western Ra-jasthan prior to Deccan volcanism and K-T alkaline magmatism. Gondwanaland fragmentation during the Mesozoic caused the development of the rift basins of Gujarat and western Rajasthan. This resulted in the opening of the Jurassic rift system and mildly alkaline magmatism at ca. 120 Ma in western India. This event was pre-K-T, and plume activity has not hypothesized for it. Continental fragmentation under an extensional tectonic regime during K-T time resulted in the magmatism and basin tectonism in western Rajasthan. Crustal development during the K-T period in western Rajasthan resulted from an extensional tectonic regime and is not the manifestation of Réunion plume activity.