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Jaisalmer Basin
Hydrocarbon Uncertainty Based on Facies Analysis: Middle Jurassic Sequence (Jaisalmer Formation), Jaisalmer Basin, Rajasthan
Petrography of the Bajocian Sandstone of Joyan Member, Jaisalmer Basin, Western Rajasthan: Implications for Provenance and Basin Evolution
Petroleum source-rock characterization and the depositional environment of Kimmeridgian–Tithonian sequences, Jaisalmer Basin, western Rajasthan, India
Evaluation of Maturity (Late Diagenesis) in Source Rocks of Jaisalmer Basin in Rajasthan, India using 57 Fe Mössbauer Spectroscopy
The Star-shaped Resting Traces Asteriacites lumbricalis from Thaiat Member (Early Jurassic -Bajocian) of Lathi Formation of the Jaisalmer Basin, Western India
Hillichnus agrioensis and Associated Trace Fossils from Hettangian to Bajocian Thaiat Member of Lathi Formation, Jaisalmer Basin, Western Rajasthan
Provenance of the Late Paleocene Sandstones of the Jaisalmer Basin, Western India
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.