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Singhora India

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Journal Article
Published: 01 April 2013
Journal of Sedimentary Research (2013) 83 (4): 368–376.
... is erosional, and (c) that the unconformity PU-2 is erosional. However, this work does not resolve any question on the stratigraphic status of either the Singhora Group or the Kharsyia Group. This research has been supported by Indiana University and grants from DST Government of India, and Indian...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M43.13
EISBN: 9781862397194
... , 1995 , 1999 ; Murti 1987 , 1996 ; Chatterjee (Jha) et al. 1990 ). Babu & Singh (2011) reported carbonaceous metaphytes related to eukaryotic algae and acritarchs also from the shales of Saraipali Formation, Singhora Group. Recently, Chakraborty et al. (2012 a , b ) described an array...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M43.14
EISBN: 9781862397194
... basins. The obtained data have already proved valuable in constraining India’s changing position in global Proterozoic reconstructions. However, tuffaceous units present within relatively small-scale basins (cropping out in hundreds of square kilometres of areal scale), despite their strategic geodynamic...
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Journal Article
Published: 09 September 2009
Geological Magazine (2010) 147 (2): 206–218.
... 111 , 379 –90. Chakraborty P. P. , Sarkar A. , Das K. & Das P. 2009 . Fan-delta and storm-dominated shelf sedimentation in the Proterozoic Singhora Group, Chattisgarh Supergroup, central India . Precambrian Research 170 , 88 – 106 . Chalapathi Rao N. V...
Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M43.3
EISBN: 9781862397194
... cratonic elements contains Precambrian–Early Palaeozoic sedimentary (or metasedimentary) sequences that form the basinal infrastructure of Peninsular India. Among the best-preserved sedimentary sequences are the so-called ‘Purana’ or ancient basins. These include the areally extensive Cuddapah...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2011
GSA Bulletin (2011) 123 (1-2): 158–167.
... ( Murti, 1987 ; Moitra, 1995 ). Das et al. (1992) described an unconformity-bounded sequence, the Singhora Group, from the basal part of the Chattisgarh succession ( Figs. 1 and 2 ). In recent years, Patranabis-Deb et al. (2007) identified an unconformity-bounded sequence, the Kharsiya Group, above...
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Journal Article
Published: 02 October 2018
Canadian Journal of Earth Sciences (2019) 56 (3): 335–346.
.... , Chakraborty , P.P. , Horie , K. , Tsutsumi , Y. , Saha , S. , and Balakrishnan , S. 2017 . Detrital zircon U–Pb geochronology, Nd isotope mapping, and sediment geochemistry from the Singhora Group, central India: implications toward provenance, its shift, and regional stratigraphic...
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Image
Simplified map of peninsular <b>India</b> showing major Proterozoic basins, craton...
Published: 01 April 2013
Fig. 1.— Simplified map of peninsular India showing major Proterozoic basins, cratons, and tectonic zones. The names of the basins are abbreviated: VI  =  Vindhyan; CH  =  Chhattisgarh; PG  =  Pranhita–Godavari Valley; I  =  Indravati; KBB  =  Kaldagi–Badami–Bhima; and CU  =  Cuddapah
Journal Article
Journal: Geophysics
Published: 31 August 2007
Geophysics (2007) 72 (5): B133–B140.
... of the sedimentary history of the Singhora group of rocks, Chhattisgarh Super Group, Madhya Pradesh : Research in Geological Survey of India , 130 , Plate 6, 184 – 187 . Chouteau M. Zhang P. Chapellier D. , 1996 , Computation of apparent resistivity profiles from VLF-EM data using linear...
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Journal Article
Published: 13 June 2008
Geological Magazine (2009) 146 (1): 133–143.
... . Economic Geology and the Bulletin of the Society of Economic Geologists 77 , 1818 – 36 . Chakraborti , S. 1997 . Elucidation of the sedimentary history of the Singhora Group of rocks, Chhattisgarh Supergroup , M. P. Record, Geological Survey of India 130 , 180 – 7 . Clemens , J. D...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M43.21
EISBN: 9781862397194
... The unmetamorphosed Proterozoic rocks of Central India are located in the Vindhyan Basin, which spans the Mesoproterozoic and Neoproterozoic eras. The dominantly flat-lying sedimentary rock sequence shares a border with the Bundelkhand Craton in the north, the Aravalli belt to the NW, the Deccan...
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Journal Article
Published: 07 July 2021
Journal of the Geological Society (2021) jgs2020-222.
... and Walter 2000 ). The BSA is well documented in central Australia, Svalbard, northwestern Canada, Ethiopia ( Swanson-Hysell et al. 2012 , 2015 ; and references therein) and possibly India ( George et al. 2018 ). It is constrained by U–Pb zircon CA-TIMS ages to have initiated after 811.5 Ma ( Macdonald...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M43.12
EISBN: 9781862397194
... Abstract Understanding of the incompatibility of King’s three-fold classification of the Proterozoic (‘Purana’) rocks of the Pranhita–Godavari Valley, south India, and renewed mapping and stratigraphic studies, reveal that syn-depositional basin dynamics, with differential uplift and subsidence...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M43.23
EISBN: 9781862397194
... The intracratonic and dominantly marine Vindhyan Basin of central India (Palaeoproterozoic lower age limit, c. ≤600 Ma or possibly 900–1000 Ma upper age limit) unconformably overlies basement rocks and the Bijawar Basin, and is reviewed by Bose et al. (2015 and references therein). Lower...
FIGURES
Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M43.11
EISBN: 9781862397194
... Abstract The Bastar Craton of India is composed of Archaean nuclei of tonalite–trondhjemite–granodiorite gneisses, enveloped by an older granite–greenstone belt (>3000 Ma) with banded iron formation (BIF), and an auriferous younger granite–greenstone belt with BIF. Available geological...
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Journal Article
Journal: Economic Geology
Published: 01 March 2001
Economic Geology (2001) 96 (2): 425–428.
... fold belt, Southwest Rajasthan and Northern Gujarat— P.R. Golani, D. Bhattacharyya, S. Sanyal, I.R. Kirmani, G. Malhotra, S. Bhattacharyya, A.K. Grover, and J.L. Narang 149 Sulphur isotopic characteristics of pyrite and galena from the Singhora Group, Chhattisgarh Supergroup, India: Genetic...