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Rohtas Formation

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Journal Article
Published: 01 June 1988
Jour. Geol. Soc. India (1988) 31 (6): 584–590.
... of Longfengsahnia chopanensis sp. nov. are reported from the Rohtas Limestone Formation, Semri Group. Beside these, Longfengsahnia stiplala and epirelief of trace fossils belonging to possibly annelids are reported from the Ghurma Shale Formation of Kaimur Group. The macrobiota record indicates that during...
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(a) Steepening of strata and change in the strike of the beds in limestone of the Rohtas Formation, east of Baradih. (b) Ferruginous shale in limestone showing ferruginous material rich in hematite forming botryoidal structure along the bedding parallel fault, southwest of Nauhata. (c) Inclined fault plane in the Ghaghar sandstone, southeast of Ramgarh, corroborates with the regional Sone-Narmada lineament having trend NE-SW. (d) Slickenside with enrichment of ferruginous material mainly in hematite forming botryoidal structure in the Ghaghar sandstone towards east of Bhoreyan. (e) Vertical fault in sandstone with thinly bedded siltstone of the Scarp Formation, southeast of Salempur. (f) Slickenside with iron enrichment mainly hematite with botryoidal form in the Dhandraul Sandstone, northwest of Dahar.
Published: 01 June 2021
Fig. 4: (a) Steepening of strata and change in the strike of the beds in limestone of the Rohtas Formation, east of Baradih. (b) Ferruginous shale in limestone showing ferruginous material rich in hematite forming botryoidal structure along the bedding parallel fault, southwest of Nauhata
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Figure 1. Paleogeographic reconstructions of distribution of limestone-marl and limestone-shale alternations (green dots), and nodular limestones (red dots). Each dot represents occurrence reported in published literature (database is available from GSA Data Repository; see text footnote 1). Based on maps from Scotese (2001). Sedimentary units plotted include following: A: Cambrian—Conasauga Group, Sneakover Limestone; Ute, Dismal Gap, Lancara, Cabitza, Kaili, Zhangxia, Rohtas Formations, and others. B: Ordovician—Trenton Group, Upton Group, Cincinnatian Series, Lexington Limestone, Chongson Limestone, Balclatchie Shales; Ponon Trehue, Edinburg, Clays Ferry, Martinsburg, Bull Fork, Drakes, Pamelia, Catoche, Table Point, Whitby, ?Ibbett Bay, Killerod, Yanwashan, Dawan Formations, and others. C: Permian—Rattendorf Group, Lower Magnesia, Khuff Formations, and others. D: Jurassic—Lias, Dogger, Malm, Ammonitico rosso, Bourgogne Marble, Calcaire Grossier, Calcaires a Cancellophycus, Gruenanger, Gintsi, Turmiel, Sarialan, Duodigou, Jomosom, Vaca Muerta Formations, and others. E: Cretaceous—Greenhorn Limestone, Chalk, Maiolica, Scaglia, “Barre du Gattar” Eq., Bagh-Beds, Beckum Beds, Santa Fe Limestone; Muleros, Walnut, Kiamichi, Kelvin, Niobrara, Annona, Demopolis, Cuchillo, Lagrima, Tamaulipas Inferior, Cotinguiba, Zumaya-Algorta, Balgarene, Bahloul, Samhan Formations, and others; Deep Sea Drilling Project Sites in Atlantic Ocean
Published: 01 March 2003
on maps from Scotese (2001) . Sedimentary units plotted include following: A: Cambrian—Conasauga Group, Sneakover Limestone; Ute, Dismal Gap, Lancara, Cabitza, Kaili, Zhangxia, Rohtas Formations, and others. B: Ordovician—Trenton Group, Upton Group, Cincinnatian Series, Lexington Limestone, Chongson
Journal Article
Published: 01 June 2021
Jour. Geol. Soc. India (2021) 97 (6): 603–614.
...Fig. 4: (a) Steepening of strata and change in the strike of the beds in limestone of the Rohtas Formation, east of Baradih. (b) Ferruginous shale in limestone showing ferruginous material rich in hematite forming botryoidal structure along the bedding parallel fault, southwest of Nauhata...
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First thumbnail for: Geology, Structure and Geochemical Features of the...
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Journal Article
Published: 01 May 2022
Jour. Geol. Soc. India (2022) 98 (5): 641–646.
... the Rohtasgarh Limestone belonging to the Rohtas Formation of the Semri Group of Sone valley and reported the age to be 1601±130 Ma. K-Ar dating yielded 940 Ma age of Scarp sandstone which was determined by Vinogradov et al. (1964) and the age of Majhgawan kimberlite has been dated at 1140±12 Ma ( Crawford...
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First thumbnail for: Incidence of Sulphide Mineralization in Porcellani...
Second thumbnail for: Incidence of Sulphide Mineralization in Porcellani...
Third thumbnail for: Incidence of Sulphide Mineralization in Porcellani...
Journal Article
Published: 01 June 1999
Jour. Geol. Soc. India (1999) 53 (6): 727–730.
... Banerjee of Delhi University and Wolfgang Frank of Vienna Universityhave now obtainedpreliminary ArIAr results from fine-grained volcanic material in the Porcellanite Formation below the Rohtas Formation, from which the supposed SSFs of Azmi (1998a) have come. This yields an isochron of 619k3.2 Ma...
Journal Article
Published: 01 April 1999
Jour. Geol. Soc. India (1999) 53 (4): 476–500.
... to MiddIe Riphean age) from Maihar and Rohtas areas in the Son valley. I wish to offer the following comments on the paper: 1. The reported microfoss;ls have been compared with the Lower Cambrian assemblage of Chert-Phosphorite Member of the Lower Tal Formation. However, the typical Lower Cambrian taxa...
Series: Geological Society, London, Special Publications
Published: 01 January 2012
DOI: 10.1144/SP365.13
EISBN: 9781862396135
... based on megafossils is given in Table 1 . Records of 1.1 Ga old triploblastic animal traces ( Seilacher et al. 1998 ) from the Churhat Sandstone; small shelly fauna, calcareous algae, metazoan embryo ( Azmi 1998 ; Azmi et al. 2007 ) from the Rohtas and Chitrakut formations, respectively...
Journal Article
Published: 01 April 2022
Jour. Geol. Soc. India (2022) 98 (4): 567–575.
... from the Rohtas Formation, the Vindhyan Supergroup, India . Precambrian Res. , v. 173 ( 1-4 ), pp. 105 – 122 . Summons , R.E. , Powell , T.G. and Boreham , C.J. ( 1988 ) Petroleum geology and geochemistry of the Middle Proterozoic McArthur Basin, Northern Australia: III...
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First thumbnail for: Mineralogy, Organic Richness and Macerated Microbi...
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Journal Article
Published: 01 January 1999
Jour. Geol. Soc. India (1999) 53 (1): 120–133.
... to the problem. M.N. Joshi, Department of Geology, DBS college, Dehra Dun comments: The discovery of Cambrian fossils from the Rohtas Formation of Vindhyan Supergroup has undoubtedly given ajolt to the established concept. Although the presence of Phanerozoic biogenic elements were reported earlier from...
Journal Article
Journal: GSA Bulletin
Published: 01 November 2007
GSA Bulletin (2007) 119 (11-12): 1486–1505.
..., the Old World appearance of the perissodactyl Hipparion, indicates that the base of the Rohtas section postdates Chron 5 or 10.9 Ma because specimens of Hipparion occur near the base of this section. Determinations of the age of the Hipparion datum in the Miocene Sinap Formation of Turkey...
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First thumbnail for: The structure and rate of late Miocene expansion o...
Second thumbnail for: The structure and rate of late Miocene expansion o...
Third thumbnail for: The structure and rate of late Miocene expansion o...
Journal Article
Published: 01 September 2008
The Journal of Geology (2008) 116 (5): 540–542.
... megascopic, eukaryotic alga bearing Rohtas Formation, Vindhyan Supergroup, India: implications for Precambrian atmospheric oxygen evolution . Precambrian Res. 132 : 107 – 121 . SubbaRao D. V. ; Khan M. W. Y. ; Sridharan D. N. ; and Nagaraju . 2007 . A new find of younger dolerite...
Journal Article
Published: 01 October 1998
Jour. Geol. Soc. India (1998) 52 (4): 381–389.
...R. J. Azmi Abstract R. J. Azmi of the Wadia Institute of Himalayan Geology here reports the discovery of small shelly fossils and brachiopods of lower Cambrian affinity from the topmost Rohtasgarh Limestone at Maihar and Rohtas in the Son Valley. This discovery is of importance as it necessitates...
Journal Article
Published: 01 November 2021
Jour. Geol. Soc. India (2021) 97 (11): 1465.
... of the geological signatures for appropriate interpretations. The sedimentary facies description and interpretation constituting Deoland and Porcellinite formations around Chopan area, Kajrahat limestone in Kuteswar-Dhanwahi area, Koldaha shale, Chorahat sandstone around Chorhat area, Rampur shale around Kudari...
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Figure 8. Three alternative models for vegetation patterns through successive time intervals (T1–T3) that could explain observed lateral variation in δ13C (Peedee belemnite [PDB]) values in the pedogenic carbonates from Rohtas. On a spatial scale of hundreds of meters, vegetation may consist of (A) patches of C3 and C4 plants that remained stable during soil formation, resulting in distinct areas of lower and higher δ13C values; (B) patches of C3 and C4 plants that shifted on the landscape during the time of soil formation, resulting in an intermediate δ13C (PDB) value (possibly with high variability among different samples from the same paleosol); or (C) a persistent, evenly distributed, fine-scale (tens of meters) mix of C3 and C4 vegetation, also resulting in an intermediate δ13C (PDB) value.
Published: 01 November 2007
Figure 8. Three alternative models for vegetation patterns through successive time intervals (T1–T3) that could explain observed lateral variation in δ 13 C (Peedee belemnite [PDB]) values in the pedogenic carbonates from Rohtas. On a spatial scale of hundreds of meters, vegetation may consist
Journal Article
Published: 01 November 2013
Jour. Geol. Soc. India (2013) 82 (5): 499–508.
... - - - - - - - - - - - - - - - - - - - - - - - - - - - - Lower Vindhyan Rohtas Formation Grypania – Chuaria Assemblage Kumar (1995) Semri Group Kheinjua Formation Coniform stromatolites Mistassinia Misra and Kumar (2005)   Kumar and Misra (2007) Porcellanite Formation - - Basal Formation Coniform stromatolites Misra...
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First thumbnail for: Organic Walled Microbiota from the Silicified Alga...
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Journal Article
Journal: Geology
Published: 01 February 2002
Geology (2002) 30 (2): 103–106.
... volcanic rocks, so samples were collected from two tuff bands (1.0–1.5 m thick) at the top of the immediately overlying Rampur Shale (RP/5/AUG and RP/4/AUG) and from a single tuff layer at the top of the underlying Porcellanite Formation (9/CH/PR/2000; Fig. 1 ). The sample RP/5/ AUG is from a tuff...
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First thumbnail for: 1.6 Ga U-Pb zircon age for the Chorhat Sandstone, ...
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Journal Article
Published: 09 September 2009
Geological Magazine (2010) 147 (2): 206–218.
... from the Kajrahat and Rohtas formations are 1721 ± 90 Ma ( Fig. 1 b; Sarangi, Gopalan & Kumar, 2004 ; Ray, 2006 ) and 1601 ± 130 Ma (Ray, Veizer & Davis, 2003 ) and 1599 ± 48 Ma (Sarangi, Gopalan & Kumar, 2004 ), respectively. Although the Pb–Pb ages are inherently not very reliable...
Journal Article
Published: 01 August 2022
Jour. Geol. Soc. India (2022) 98 (8): 1131–1136.
... . Sarangi , S. , Gopala , K. and Kumar , S. ( 2004 ) Pb-Pb age of earliest megascopic eukaryotic alga bearing Rohtas Formation, Vindhyan Supergroup, India: implications for Precambrian atmospheric oxygen evolution; Precambrian Res. v. 132 , pp. 107 – 121 . Sengupta , C.K...
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First thumbnail for: Organic Matter (OM) Associated Uranium Mineralisat...
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Journal Article
Published: 01 March 1996
Jour. Geol. Soc. India (1996) 47 (3): 313–324.
... comprises six dominantly siliciclastic formations (Table I) overlying the Semri Group. Most earlier workers considered the KaimurlSemri boundary to be conformable, criteria being that the Rohtas Limestone (the topmost unit of the Sernri Group) passes to overlying Sasaram Sandstone (lowermost unit...