Lithofacies, provenance and diagenesis of Surajkund Formation, Central Narmada Basin, Narmadapuram District, Madhya Pradesh, India
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| Publicado en: | Journal of Earth System Science vol. 133, no. 3 (Sep 2024), p. 134 |
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Springer Nature B.V.
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| Acceso en línea: | Citation/Abstract Full Text Full Text - PDF |
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MARC
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| 024 | 7 | |a 10.1007/s12040-024-02335-x |2 doi | |
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| 045 | 2 | |b d20240901 |b d20240930 | |
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| 100 | 1 | |a Kale, M G |u Savitribai Phule Pune University, Department of Geology, Pune, India (GRID:grid.32056.32) (ISNI:0000 0001 2190 9326) | |
| 245 | 1 | |a Lithofacies, provenance and diagenesis of Surajkund Formation, Central Narmada Basin, Narmadapuram District, Madhya Pradesh, India | |
| 260 | |b Springer Nature B.V. |c Sep 2024 | ||
| 513 | |a Journal Article | ||
| 520 | 3 | |a Surajkund Formation of Central Narmada Basin exhibits fining upward sequences of pebbly conglomerate, coarse-fine grained sandstone, siltstone and association of seven lithofacies, namely massive pebbly conglomerate, coarse-medium grained sandstone with large scale tabular cross bedding, massive coarse grained sandstone, coarse to medium grained sandstone with horizontal parallel bedding, fine grained sandstone with parallel lamination, fine grained sandstone with ripple lamination and siltstone, indicates their deposition in mixed load meandering river. Granulometric studies of Surajkund sediments also support the fluvial depositional environment. Soft sediment deformation structures documented in the siltstones suggest sediment liquification due to earthquake shocks. Abundant development of nodular, bedded calcretes and rhizoliths within these sediments are indicative of semi-arid climate and related subaerial exposure. These sediments are prominently lithic arenites, and clay mineralogy as well as geochemistry indicate deposition in the proximity of source, short distance of transport and mixed provenance of a variety of pre-Quaternary rocks such as Precambrian metamorphic rocks and granites, Vindhyan and Gondwana Supergroups, Deccan Trap basalt and laterite. Evidences of fresh water phreatic as well as vadose zone diagenesis linked to the semi-arid climatic conditions, together with subaerial exposure of these sediments, are seen in thin sections, which are supported by δ13C (av. −5.67%) and δ18O (av. −3.88%) values of calcretes. These values also suggest calcretes formed due to pedogenic and shallow groundwater processes in warm climate with C4-dominated vegetation. OSL date of one sample from Surajkund Formation gave an Ionian Age of Pleistocene Epoch. | |
| 651 | 4 | |a Narmada River | |
| 651 | 4 | |a India | |
| 651 | 4 | |a Madhya Pradesh India | |
| 653 | |a Earthquakes | ||
| 653 | |a Basalt | ||
| 653 | |a Bedding | ||
| 653 | |a Carbon 13 | ||
| 653 | |a Diagenesis | ||
| 653 | |a Inland water environment | ||
| 653 | |a Sediments | ||
| 653 | |a Quaternary | ||
| 653 | |a Lithofacies | ||
| 653 | |a Semiarid climates | ||
| 653 | |a Metamorphic rocks | ||
| 653 | |a Sandstone | ||
| 653 | |a Siltstone | ||
| 653 | |a Geochemistry | ||
| 653 | |a Groundwater | ||
| 653 | |a Climatic conditions | ||
| 653 | |a Sediment load | ||
| 653 | |a Clay minerals | ||
| 653 | |a Laterites | ||
| 653 | |a Mineralogy | ||
| 653 | |a Precambrian | ||
| 653 | |a Vadose water | ||
| 653 | |a Pleistocene | ||
| 653 | |a Meandering | ||
| 653 | |a Conglomerates | ||
| 653 | |a Sediment | ||
| 653 | |a Climate and vegetation | ||
| 653 | |a Arid climates | ||
| 653 | |a Deposition | ||
| 653 | |a Deformation | ||
| 653 | |a Lamination | ||
| 653 | |a Seismic activity | ||
| 653 | |a Fossils | ||
| 653 | |a River meanders | ||
| 653 | |a Gondwana | ||
| 653 | |a Sedimentary rocks | ||
| 653 | |a Arenites | ||
| 653 | |a Paleontology | ||
| 653 | |a Fresh water | ||
| 653 | |a Freshwater | ||
| 653 | |a Warm climates | ||
| 653 | |a Archaeology | ||
| 653 | |a Climate | ||
| 653 | |a Sedimentation & deposition | ||
| 653 | |a Aridity | ||
| 653 | |a Environmental | ||
| 700 | 1 | |a Pundalik, Ashwin S |u St. Xavier’s College, Department of Geology, Mumbai, India (GRID:grid.454329.d) | |
| 700 | 1 | |a Kumar, Devender |u CSIR-National Geophysical Research Institute, Hyderabad, India (GRID:grid.419382.5) (ISNI:0000 0004 0496 9708) | |
| 773 | 0 | |t Journal of Earth System Science |g vol. 133, no. 3 (Sep 2024), p. 134 | |
| 786 | 0 | |d ProQuest |t Science Database | |
| 856 | 4 | 1 | |3 Citation/Abstract |u https://www.proquest.com/docview/3078829607/abstract/embedded/2AXJIZYYTBW5RQEH?source=fedsrch |
| 856 | 4 | 0 | |3 Full Text |u https://www.proquest.com/docview/3078829607/fulltext/embedded/2AXJIZYYTBW5RQEH?source=fedsrch |
| 856 | 4 | 0 | |3 Full Text - PDF |u https://www.proquest.com/docview/3078829607/fulltextPDF/embedded/2AXJIZYYTBW5RQEH?source=fedsrch |