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Статті в журналах з теми "Eastern Ghats Belt"
Rao, V. Divakara, B. L. Narayana, M. V. Subba Rao, P. Rama Rao, J. Mallikharjuna Rao, N. N. Murthy, and G. L. N. Reddy. "Evolution of the Eastern Ghats Granulite Belt." Gondwana Research 1, no. 3-4 (October 1998): 416–19. http://dx.doi.org/10.1016/s1342-937x(05)70862-5.
Повний текст джерелаSimmat, Ralf, and Karen Rickers. "Wagnerite in high-MgAl granulites of Anakapalle, Eastern Ghats Belt, India." European Journal of Mineralogy 12, no. 3 (May 31, 2000): 661–66. http://dx.doi.org/10.1127/0935-1221/2000/0012-0661.
Повний текст джерелаDasgupta, Somnath, Sankar Bose, and Kaushik Das. "Tectonic evolution of the Eastern Ghats Belt, India." Precambrian Research 227 (April 2013): 247–58. http://dx.doi.org/10.1016/j.precamres.2012.04.005.
Повний текст джерелаMukhopadhyay, Dhruba, and Krishnapriya Basak. "The Eastern Ghats Belt … A polycyclic granulite terrain." Journal of the Geological Society of India 73, no. 4 (April 2009): 489–518. http://dx.doi.org/10.1007/s12594-009-0034-8.
Повний текст джерелаOKUDAIRA, T., T. HAMAMOTO, B. HARI PRASAD, and RAJNEESH KUMAR. "Sm–Nd and Rb–Sr dating of amphibolite from the Nellore–Khammam schist belt, SE India: constraints on the collision of the Eastern Ghats terrane and Dharwar–Bastar craton." Geological Magazine 138, no. 4 (July 2001): 495–98. http://dx.doi.org/10.1017/s001675680100543x.
Повний текст джерелаBiswal, T. K., and S. K. Jena. "Large Lateral Ramp in the Fold-Thrust Belts of Mesoproterozoic Eastern Ghats Mobile Belt, Eastern India." Gondwana Research 2, no. 4 (October 1999): 657–60. http://dx.doi.org/10.1016/s1342-937x(05)70232-x.
Повний текст джерелаKumar, K. Vijaya, C. Leelanandam, and W. G. Ernst. "Evolution of the Eastern Ghats Belt, India: A Magmatic Perspective." Journal of the Geological Society of India 97, no. 2 (February 2021): 217. http://dx.doi.org/10.1007/s12594-021-1657-7.
Повний текст джерелаMahapatro, S. N., A. K. Tripathy, J. K. Nanda, and S. C. Rath. "Petrology of the Udayagiri anorthosite complex, Eastern Ghats Belt, India." Journal of the Geological Society of India 82, no. 4 (October 2013): 319–29. http://dx.doi.org/10.1007/s12594-013-0159-7.
Повний текст джерелаNanda, J. K., and U. C. Pati. "Geochemistry and original nature of Precambrian khondalites in the Eastern Ghats, Orissa: a discussion." Transactions of the Royal Society of Edinburgh: Earth Sciences 82, no. 1 (1991): 87–88. http://dx.doi.org/10.1017/s0263593300007537.
Повний текст джерелаBhowmik, Santanu Kumar. "Multiple episodes of tectonothermal processes in the Eastern Ghats granulite belt." Journal of Earth System Science 106, no. 3 (September 1997): 131–46. http://dx.doi.org/10.1007/bf02839285.
Повний текст джерелаДисертації з теми "Eastern Ghats Belt"
Simmat, Ralf. "Identifizierung hochgradig metamorpher Krustenprovinzen im Indischen Eastern Ghats Belt mittels der Datierung von Monazit mit der Elektronenstrahl-Mikrosonde." [S.l.] : [s.n.], 2003. http://deposit.ddb.de/cgi-bin/dokserv?idn=968954170.
Повний текст джерелаSarkar, Tapabrato [Verfasser]. "Formation and evolution of a Proterozoic magmatic arc – the Ongole domain of the Eastern Ghats Belt, India / Tapabrato Sarkar." Kiel : Universitätsbibliothek Kiel, 2014. http://d-nb.info/1052529240/34.
Повний текст джерелаSimmat, Ralf [Verfasser]. "Identifizierung hochgradig metamorpher Krustenprovinzen im Indischen Eastern Ghats Belt mittels der Datierung von Monazit mit der Elektronenstrahl-Mikrosonde / vorgelegt von Ralf Simmat." 2003. http://d-nb.info/968954170/34.
Повний текст джерелаGore, R. J. "Geochronological and sedimentological constraints of the Srisailam Formation, S.E. India." Thesis, 2011. http://hdl.handle.net/2440/96125.
Повний текст джерелаThe 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
Henderson, B. J. "The tectonic evolution of the Ongole Domain, India: a metamorphic and geochronological approach." Thesis, 2011. http://hdl.handle.net/2440/96173.
Повний текст джерелаThe Ongole Domain, situated in the southern Eastern Ghats Belt, exposes an assemblage of granulite facies metasedimentary and metaigneous rocks that preserve fundamental evidence for the Paleoproterozoic-Mesoproterozoic reconstruction of the supercontinent Nuna. LA-ICP-MS detrital zircon data from metasedimentary rocks constrain the timing of deposition for the sedimentary precursors, to between ca. 1850-1750 Ma. Lu-Hf isotopic data from detrital zircons provide a wide range of εHf values between -18 and +10, and TDM of ca. 3.2- 2.6 Ga. The Mesoarchean to Paleoproterozoic detrital components display geochemical similarities with the Napier Complex, the North Australian Craton and to a lesser extent, the North China Craton. U-Pb zircon and monazite geochronology have identified three episodes of metamorphism in the Ongole Domain; at ca. 1750, 1640 and 1590 Ma. Peak P-T estimates of 900 - 910°C and 9 - 9.2 kbar are calculated for metamorphism associated with collisional orogenesis, between ca. 1640-1590 Ma. Ti-in-zircon thermometry independently constrains the UHT conditions, yielding estimates of 935 ± 55°C. U-Pb geochronology and trace element analysis of zircon grains from metaigneous rocks confirm syn-tectonic magmatism occurred in the Ongole Domain between ca. 1640-1570 Ma. The results provide support for paleogeographic reconstructions that link the southern Eastern Ghats Belt and East Antarctica during the late Paleoproterozoic
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
Книги з теми "Eastern Ghats Belt"
Rao, A. T. A crustal section of eastern Dharwar craton-Godavari rift-Eastern Ghats mobile belt, India: Field excursion guide book. Bangalore: Geological Society of India, 1997.
Знайти повний текст джерелаWorkshop on Eastern Ghats Mobile Belt (1994 Vishakhapatnam, India). Proceedings of Workshop on Eastern Ghats Mobile Belt =: Istarna Ghāṭa Mobāila Belṭa ke Kāryaśālā para kāryavāhī. Calcutta: Geological Survey of India, 1998.
Знайти повний текст джерелаЧастини книг з теми "Eastern Ghats Belt"
Sharma, Ram S. "Eastern Ghats Mobile Belt." In Cratons and Fold Belts of India, 231–61. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-01459-8_7.
Повний текст джерелаVerma, R. K. "Gravity Studies in the Eastern Ghats Belt." In Gravity Field, Seismicity and Tectonics of the Indian Peninsula and the Himalayas, 76–90. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5259-1_6.
Повний текст джерелаGupta, Saibal, Ritabrata Dobe, Amol Dayanand Sawant, Surajit Misra, and William Kumar Mohanty. "The Northern Margin of the Eastern Ghats Mobile Belt: Evidence for Strike-Slip Tectonics Along a Craton-Mobile Belt Boundary." In Society of Earth Scientists Series, 153–74. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40593-9_7.
Повний текст джерелаBose, Sankar, Kaushik Das, Supriya Chakraborty, and Hiroyuki Miura. "Petrology and Geochemistry of Metamorphosed Basic Intrusives from Chilka Lake Granulites, Eastern Ghats Belt, India: Implications for Rodinia Breakup." In Dyke Swarms:Keys for Geodynamic Interpretation, 241–61. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-12496-9_14.
Повний текст джерелаSengupta, Pulak, and Somnath Dasgupta. "Modelling of Metamorphic Textures with C-Space: Evidence of Pan-African High-grade Reworking in the Eastern Ghats Belt, India." In Physics and Chemistry of the Earth’s Interior, 29–39. New York, NY: Springer New York, 2009. http://dx.doi.org/10.1007/978-1-4419-0346-4_2.
Повний текст джерелаPrakash, Divya, and Deepak. "High Pressure and Ultrahigh Temperature Metamorphism at Diguva Sonaba, Eastern Ghats Mobile Belt (India): New Constraints from Phase Equilibria Modelling." In Geostatistical and Geospatial Approaches for the Characterization of Natural Resources in the Environment, 527–31. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-18663-4_79.
Повний текст джерелаYadav, Pawan Kumar, Manorama Das, and Sradhanjali Subhadarshini. "Manganese Mineralization in Manganiferous Quartzite in the Boringpadar-Amath Area, Eastern Ghats Mobile Belt, Odisha, India: Implication for Climatic Changes." In Springer Climate, 195–220. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-16254-1_9.
Повний текст джерелаValdiya, K. S. "Mesoproterozoic Eastern Ghat Mobile Belt." In Society of Earth Scientists Series, 185–204. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-25029-8_6.
Повний текст джерелаRoy, A. B., and Ritesh Purohit. "Eastern Ghats Granulite Belt." In Indian Shield, 237–48. Elsevier, 2018. http://dx.doi.org/10.1016/b978-0-12-809839-4.00011-4.
Повний текст джерелаChetty, TRK. "The Eastern Ghats Mobile Belt." In Proterozoic Orogens of India, 119–210. Elsevier, 2017. http://dx.doi.org/10.1016/b978-0-12-804441-4.00003-1.
Повний текст джерелаТези доповідей конференцій з теми "Eastern Ghats Belt"
Behera, Soumya Ranjan, Lopamudra Saha, D. K. Pal, and A. K. Champati. "Proterozoic Tectonics from the Northern Domain of the Eastern Ghats Belt." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.156.
Повний текст джерелаBehera, Soumyaranjan, and Lopamudra SAHA. "How strong are the Pan-African signatures from the northern part of the Eastern Ghats Belt?" In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12119.
Повний текст джерелаSaikia, Dicton. "Growth of coronal garnet in Koraput Anorthosite Pluton, Eastern Ghats Belt (Domain 2), India, and implications for Gondwanaland assembly." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.8537.
Повний текст джерелаChatterjee, Amitava, Suresh Chandra Patel, and Chang Whan Oh. "The Amalgamation of the Eastern Ghats Belt with the Dharwar Craton, India: Constraints from SHRIMP Zircon and EPMA Monazite Dating." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.367.
Повний текст джерелаBanerjee, Aparupa, Proloy Ganguly, Sankar Bose, Das Kaushik, and Nilanjana Sorcar. "Two-stage metamorphism of the Angul-Tikarpada area, Eastern Ghats Belt and its implications on the India-East Antarctica correlation." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.8912.
Повний текст джерелаKrishnamacharyulu, S., and K. Vijaya Kumar. "Geophysical Signatures on Mesoproterozoic Chimakurti Anorthosite-Gabbro (CAG) complex, Eastern Ghat Belt, India - Understanding the Magmatic Processes." In 1st Conference on Geophysics for Geothermal-Energy Utilization and Renewable-Energy Storage. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902497.
Повний текст джерела