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Petroleum source-rock characterization and the depositional environment of Kimmeridgian–Tithonian sequences, Jaisalmer Basin, western Rajasthan, India
The Star-shaped Resting Traces Asteriacites lumbricalis from Thaiat Member (Early Jurassic -Bajocian) of Lathi Formation of the Jaisalmer Basin, Western India
Petrography of the Bajocian Sandstone of Joyan Member, Jaisalmer Basin, Western Rajasthan: Implications for Provenance and Basin Evolution
Thermal Modification of the Northwest Indian Shield: As Evidenced by Integrated Geopotential Modelling
Late Paleocene-Early Eocene Foraminiferal Assemblage and Carbon Isotope Excursion Indicating Hyperthermal Events in Paleotropical Succession of Northwestern India
Abstract The Indus River drains the Western Himalayas and is supplying sediment to the second largest submarine fan in the world in the Arabian Sea. Sediment flux represents erosion in the mountains, driven by tectonic and climatic processes, yet these are buffered over several time scales, spanning millions of years in the foreland basin and shorter time scales due to storage in terraces and on floodplains. Further recycling and buffering of the erosional signal is possible because of interactions with the dunes of the Thar Desert, whose volume exceeds the size of the Holocene Delta along the eastern edge of the drainage basin. Volume calculations suggest significant storage and recycling of sediment on time scales of around 10–20 ka both in the valleys of the Karakoram and on the flood plains adjacent to the mountain front. Although much of the sediment is generated by glacial processes, the transport of that material appears to be controlled by the strength of the monsoon precipitation. Sediments that are delivered to the ocean are transported relatively quickly into the submarine canyon but with only limited buffering at least in the landward portions. Rising and high stand sea level conditions do not cut off sediment supply to the canyon. The composition of material in the thalweg and terraces indicate lag times of no more than around 8000 years and probably much less between the river mouth and the canyon, especially in the early Holocene. Sediment supply modulated by the monsoon appears to dominate over sea level in controlling delivery to the deep ocean. On longer time scales (~2 Ma) sediments recovered on the submarine fan by IODP have most similarity with the interglacial composition of the Indus River rather than the glacial, as defined by zircon U-Pb ages. This again implies that monsoon precipitation dominates in controlling sediment flux to the deep sea.
Diagenetic Features of Jurassic Fort Member Sandstone, Jaisalmer Formation, Western Rajasthan
Radioactive Occurrence in Sediments of Cenozoic Age near Bandha Village, Jaisalmer District, Rajasthan
Depositional Environment In Great Indian Desert Using Grain Size Parameters And Its Chemical Characterization: by Chander Kumar Singh, Pankaj Kumar, Alok Kumar and Saumitra Mukherjee. Jour. Geol. Soc. India, v.86, October 2015, pp.412-420
Distribution, Forms and Spatial Variability of Desert Pavements in Arid Western Rajasthan
New Report of Isocrinid Crinoid Chariocrinus from the Jurassic of Jaisalmer, Rajasthan, India
Depositional Environment in Great Indian Desert using Grain Size Parameters and its Chemical Characterization
Fluvial–Eolian Interactions In Sediment Routing and Sedimentary Signal Buffering: An Example From the Indus Basin and Thar Desert
Provenance of the Late Paleocene Sandstones of the Jaisalmer Basin, Western India
Jurassic Foraminifera from Jajiya Member, Jaisalmer Formation, Western Rajasthan
Abstract: Early Paleocene planktic foraminifera (Zones P1c to P4) from well sections (Sanu, Sam, Tanot, Ram-1, GTF-1) are reported from the Jaisalmer Basin. The Subzone P1c is characterized by the hemipelagic early Danian species Globoconusa daubjergensis, Eoglobigerina edita, Praemurica pseudoinconstans, P. inconstans, Parasubbotina pseudobulloides, Subbotina triloculinoides and Globanomalina compressa. Zone P2 is identified by the total range of Praemurica uncinata and Eoglobigerina spiralis and Zone P3 by the occurrence of Igorina pusilla in association of Morozovella angulata and M. conicotruncata. Larger benthic foraminiferal species, such as Assilina dandotica , are abundant in the interval identified as Zone P4 characterized by Globanomalina pseudomenardii , Morozovella velascoensis, Igorina albeari, I. tadjikistanensis, Subbotina velascoensis, S. triangularis, Acarinina soldadoensis , and Parasubbotina varianta . This indicates a lower P4 stratigraphic range for Assilina dandotica , which was assumed to appear in Zone P5 (= Standard benthic foraminiferal Zone 5). The Paleocene-Eocene boundary was identified based on Acarinina africana and A. sibaiyaensis marking the Zones P5 to E1 interval.