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Academic literature on the topic 'Cuddapah Basin'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Cuddapah Basin"

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Bhoopathi, Vishnu, S. Niranjan Kumar, R. S. N. Sastry, and B. Srinivas. "Surface radioactive anomalies at Srisailam sub basin, Cuddapah basin, India." Chinese Journal of Geochemistry 34, no. 2 (March 10, 2015): 265–71. http://dx.doi.org/10.1007/s11631-015-0046-6.

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SAHOO, DEBIDARSANI, KAMAL LOCHAN PRUSETH, DEWASHISH UPADHYAY, SAMEER RANJAN, DIPAK C. PAL, RAHUL BANERJEE, and SHEKHAR GUPTA. "New constraints from zircon, monazite and uraninite dating on the commencement of sedimentation in the Cuddapah basin, India." Geological Magazine 155, no. 6 (April 4, 2017): 1230–46. http://dx.doi.org/10.1017/s0016756817000140.

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AbstractThe Cuddapah basin in southern India, consisting of the Palnad, Srisailam, Kurnool and Papaghni sub-basins, contains unmetamorphosed and undeformed sediments deposited during a long span of time in the Proterozoic. In the absence of robust age constraints, there is considerable confusion regarding the relative timing of sedimentation in these sub-basins. In this study, U–Pb isotopic dating of zircon and U–Th–Pbtotaldating of monazite and uraninite from the gritty quartzite that supposedly belongs to the formation Banganapalle Quartzite have been used to constrain the beginning of sedimentation in the Palnad sub-basin. Magmatic and detrital zircons recording an age of 2.53 Ga indicate that the sediments were derived from the granitic basement or similar sources and were deposited after 2.53 Ga. Hydrothermally altered zircons both in the basement and the cover provide concordant ages of 2.32 and 2.12 Ga and date two major hydrothermal events. Thus, the gritty quartzite must have been deposited sometime between 2.53 and 2.12 Ga and represents the earliest sediments in the Cuddapah basin. Monazite and uraninite give a wide spectrum of ages between 2.5 Ga and 150 Ma, which indicates several pulses of hydrothermal activity over a considerable time span, both in the basement granite and the overlying quartzite. The new age constraints suggest that the gritty quartzite may be stratigraphically equivalent to the Gulcheru Quartzite that is the oldest unit in the Cuddapah basin, and that a sedimentary/erosional hiatus exists above it.
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Venkatakrishnan, Ramesh, and Firoz E. Dotiwalla. "The Cuddapah Salient: a tectonic model for the Cuddapah Basin, India, based on Landsat image interpretation." Tectonophysics 136, no. 3-4 (May 1987): 237–53. http://dx.doi.org/10.1016/0040-1951(87)90027-8.

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Babu, H. V. Ram. "Basement structure of the Cuddapah Basin from gravity anomalies." Tectonophysics 223, no. 3-4 (August 1993): 411–22. http://dx.doi.org/10.1016/0040-1951(93)90148-d.

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Chakrabarti, Gopal, Debasish Shome, Subhasish Kumar, George M. Stephens, and Linda C. Kah. "Carbonate platform development in a Paleoproterozoic extensional basin, Vempalle Formation, Cuddapah Basin, India." Journal of Asian Earth Sciences 91 (September 2014): 263–79. http://dx.doi.org/10.1016/j.jseaes.2013.09.028.

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Konda, Shankar, Prasanta K. Patro, and C. K. Rao. "Geoelectric signatures of Palnad sub basin and Nallamalai Fold Belt, Cuddapah Basin, India." Journal of the Geological Society of India 86, no. 4 (October 2015): 377–82. http://dx.doi.org/10.1007/s12594-015-0325-1.

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Chetty, T. R. K. "Tectonics of proterozoic Cuddapah Basin, southern India: A conceptual model." Journal of the Geological Society of India 78, no. 5 (November 2011): 446–56. http://dx.doi.org/10.1007/s12594-011-0109-1.

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Thomas, P. K., Tresa Thomas, Jugina Thomas, M. S. Pandian, Rahul Banerjee, P. V. Ramesh Babu, Shekhar Gupta, and Rajiv Vimal. "Role of hydrothermal activity in uranium mineralisation in Palnad Sub-basin, Cuddapah Basin, India." Journal of Asian Earth Sciences 91 (September 2014): 280–88. http://dx.doi.org/10.1016/j.jseaes.2014.02.013.

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R, Maheswararao, Srinivasa Gowd S, Harish Vijay G, Krupavathi C, and Pradeep Kumar B. "Geomorphological studies of the Sedimentary Cuddapah Basin, Andhra Pradesh, South India." International Journal of Geoinformatics and Geological Science 7, no. 2 (June 25, 2020): 14–20. http://dx.doi.org/10.14445/23939206/ijggs-v7i2p102.

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Prasad, M., B. Muralidhara Reddy, V. Sunitha, M. Ramakrishna Reddy, and Y. Sudharshan Reddy. "Inventory data on the sinkhole occurrences from Proterozoic Cuddapah Basin, India." Data in Brief 25 (August 2019): 104054. http://dx.doi.org/10.1016/j.dib.2019.104054.

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Dissertations / Theses on the topic "Cuddapah Basin"

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Anand, M. "Tectono-magmatic evolution of the intra-cratonic Cuddapah Basin, India." Thesis, University of Cambridge, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.595495.

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Mafic-ultramafic igneous rocks from the Early Proterozoic intra-cratonic Cuddapah Basin of southern India have been studied for their petrological and geochemical characteristics. A field reconnaissance survey was accompanied by sample collection from several stratigraphic horizons in the sedimentary basin. 40Ar-39Ar laser fusion age determinations on phlogopite mica in the Tadpatri mafic-ultramafic sills have provided firm constraints on the age of the earliest phase of the mafic magmatism in the basin at 1.9 Ga. Petrographical and mineralogical studies of the Vempalle have Tadpatri sills from the Cuddapah Basin have provided some insight into the complex magma chamber processes that may have modified their parental melt compositions. This has been further investigated by studying variations in the major, trace and rare-earth element concentrations of the lavas and sills. Geochemical modelling using the major and trace element concentrations of mafic rocks from the Cuddapah Basin has provided firm constraints for the melt generation processes during the Early Proterozoic. Both forward and inverse geochemical modelling of the lavas and sills suggest that the former were generated by ~ 8-12% partial melting of a lherzolite mantle source whereas the sills were generated by larger degrees (~ 12-18%) of partial melting at a mantle potential temperature (Tp) of ~ 1500oC. The thickness of the mechanical boundary layer predicted by the geochemical modelling, after lithospheric stretching, is 70 km with a minimum initial lithospheric thickness of 120 km. This corresponds to a lithospheric stretching factor (β) of 1.6-1.8.
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Chalapathi, Rao Nittala Venkata. "Petrogenesis of Proterozoic kimberlites and lamproites from the Cuddapah Basin and Dharwar craton, southern India." Thesis, University of Cambridge, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.627224.

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Macintosh, J. N. "Age and basin evolution of the Cuddapah Supergroup, India." Thesis, 2010. http://hdl.handle.net/2440/103376.

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U-Pb zircon geochronology indicates deposition of the Cuddapah Supergroup, Cuddapah Basin, India occurred for at least 986 million years. Deposition started after 2502±17 Ma with the deposition of the Gulcheru Formation and ended after 913±11 Ma with the deposition of the Cumbum Formation. Maximum depositional ages have been found for individual formations within the Cuddapah Supergroup; the Pulivendla Formation has a maximum deposition of 1899±19 Ma and the Bairenkonda Formation has a maximum depositional age of 1660±22 Ma. Thermal events during the Palaeoproterozoic present a possible cause of basin formation. At this early stage of the Cuddapah Basin’s evolution the provenance of sediments was the Dharwar Craton, which currently underlies the basin and borders it on the north, south and west sides. The uplift of the Eastern Ghats on the eastern margin affected the evolution of the Cuddapah Basin, changing the shape and the sediments of the basin. Uplift and deformation events in the Eastern Ghats folded the eastern side of the Cuddapah Basin and are responsible for its present crescent shape. The formation of the Eastern Ghats caused increased subsidence to the east, creating an asymmetry in the depth of the basin. The provenance of the sediments of the Cuddapah Supergroup changed to the Eastern Ghats for the deposition of the youngest stratigraphic group, the Nallamalai Group.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
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Falster, G. M. "Geochronological and sedimentological constraints on the evolution of the lower Cuddapah Basin, India." Thesis, 2011. http://hdl.handle.net/2440/96124.

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The Palaeo- to Mesoproterozoic Cuddapah Supergroup was deposited in the Cuddapah Basin, which is one of a number of Proterozoic volcano-sedimentary basins that overlie the Indian Shield. On the south-western margin of the basin, the stratigraphic succession in the basal Papaghni and Chitravati groups is initially composed of gravelly fluvial deposits with dominant sediment input coming from the western foreland. These are succeeded by shallow-water stromatolitic dolomite and shale with a significantly reduced siliciclastic component, and finally by sub-tidal laminated silt and sand. A detailed facies analysis of these rocks suggests that deposition occurred initially in an active extensional setting which subsequently developed into a passive extensional setting. Stable isotope geochemistry of dolomites in the Vempalle Formation of the Papaghni Group indicates that deposition of the formation may initially have occurred in a restricted setting where δ13C varied according to fractionation via environmental processes. Whether the Vempalle Formation was deposited in a shallow marine or lacustrine milieu is equivocal; δ13C values may correlate with the conclusion of the global oceanic “Lomagundi” positive δ13C excursion around 2100 Ma, however, this inference requires the carbonates to have been precipitated in oceanic water, and have retained their primary isotopic signature during pervasive dolomitisation. U-Pb dating of detrital zircon grains from the Gandikota Formation – previously thought to be the uppermost formation of the Chitravati Group – yields a maximum depositional age of 1207 ± 22 Ma. This is significantly younger than intrusive igneous rocks within the Cuddapah Supergroup and it is therefore likely that the Gandikota Formation is part of the overlying Meso- to Neoproterozoic Kurnool Group. The detrital zircon age spectrum of the Gandikota Formation indicates significant sediment input from the east, which is likely to be a result of the thrusting of the Eastern Ghats Belt onto the Eastern Dharwar Craton and a reversal of the prevailing extensional regime in the Cuddapah Basin. A number of authors have proposed a genetic link between the Cuddapah Basin and several other Proterozoic basins of the Indian Shield. This study provides no reason to directly correlate the temporally and spatially distinct basins.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
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Gore, R. J. "Geochronological and sedimentological constraints of the Srisailam Formation, S.E. India." Thesis, 2011. http://hdl.handle.net/2440/96125.

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The Proterozoic Cuddapah Basin contains the poorly constrained Srisailam Formation, which presumably lies unconformably over the Nallamalai Group. The Cuddapah Basin is thought to have initiated as a rift basin > 1900 Ma before developing into a foreland basin due to uplift of the Eastern Ghats Belt (EGB) at ~1600 Ma. U-Pb geochronology indicates deposition of the Srisailam Formation commenced after 1660 Ma and ceased prior to the deposition of the Kurnool Group which was deposited < 1090 Ma. The Srisailam Formation was deposited in a tidal flat/shallow marine environment as it contains tidal and storms influences, glauconitic sandstones, along with bimodal east-west paleocurrents, which suggest links with an open seaway. Detrital zircon Hf isotope data combined with detrital zircon U-Pb data suggest the Dharwar Craton as a dominant source region with a mixed crustal evolution (ɛHf -11 to +8). Detrital zircon age peaks at ~3200 Ma, ~2700-2400 Ma and ~2300 Ma imply that sediments are dominantly sourced from 3400-3000 Ma tonalite-trondhjemite-granodiorite (TTG), 3000-2500 Ma volcanosedimentary greenstone belts and 2600-2500 Ma calc-alkaline to K-rich granitic intrusions. Trace element data suggests zircon grains are sourced from granitoids with zircon crystallisation at ~860˚C. This study reveals that the Srisailam Formation is quite possibly a lateral equivalent of the Nallamalai Group.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
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Books on the topic "Cuddapah Basin"

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Saxena, Praveen Raj. Project completion report: title of project, "Ore potentiality of granitoids along the eastern margin of Cuddapah Basin, A.P. a petrographic & geochemical approach". Hyderabad, A.P: Dept. of Applied Geochemistry, University College of Science, Osmania University, 1991.

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Book chapters on the topic "Cuddapah Basin"

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Goutham, M. R., K. V. Subbarao, C. V. R. K. Prasad, J. N. Walsh, and V. Damodara Reddy. "Proterozoic Mafic Dykes from the Southern Margin of Cuddapah Basin, India: Part 1 – Geochemistry and Petrogenesis." In Dyke Swarms:Keys for Geodynamic Interpretation, 47–71. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-12496-9_4.

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Goswami, Sukanta, and P. K. Upadhyay. "Tectonic History of the Granitoids and Kadiri Schist Belt in the SW of Cuddapah Basin, Andhra Pradesh, India." In Tectonics and Structural Geology: Indian Context, 253–78. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99341-6_8.

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Goutham, M. R., K. V. Subbarao, C. V. R. K. Prasad, J. D. A. Piper, and D. P. Miggins. "Proterozoic Mafic Dykes from the Southern Margin of Cuddapah Basin, India: Part 2 – Palaeomagnetism and Ar/Ar Geochronology." In Dyke Swarms:Keys for Geodynamic Interpretation, 73–93. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-12496-9_5.

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Goswami, Sukanta, P. K. Upadhyay, and V. Natarajan. "Importance of Fracturing in Uranium Mineralization in Gulcheru Quartzite Host: A Case from Ambakapalle Area, Cuddapah Basin, Andhra Pradesh, India." In Structural Geology and Tectonics Field Guidebook — Volume 1, 577–98. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60143-0_19.

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Tripathy, Vikash, Satyapal, S. K. Mitra, and V. V. Sesha Sai. "Fold-Thrust Belt Architecture and Structural Evolution of the Northern Part of the Nallamalai Fold Belt, Cuddapah Basin, Andhra Pradesh, India." In Tectonics and Structural Geology: Indian Context, 219–52. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99341-6_7.

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Sai, V. V. Sesha. "Petrology and Mineral Chemistry of Picrite Sill from Peddakudala-Velpula Area, in Southwestern Part of the Proterozoic Cuddapah Basin, Andhra Pradesh, India." In Dyke Swarms:Keys for Geodynamic Interpretation, 115–24. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-12496-9_7.

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Reddy, Y. Sudharshan, V. Sunitha, and B. Suvarna. "Physical and Hydro Geochemical Impact Assessment of Inactive Mines in and Around Southwestern Part of Cuddapah Basin Using a Conceptual Site Model (CSM)." In Lecture Notes in Civil Engineering, 793–807. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-0304-5_55.

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Dasgupta, P. K., A. Biswas, and R. Mukherjee. "11. Cyclicity in paleoproterozoic to neoproterozoic cuddapah supergroup and its significance in basinal evolution." In Cyclic Development of Sedimentary Basins, 313–54. Elsevier, 2005. http://dx.doi.org/10.1016/s0070-4571(05)80013-5.

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