Academic literature on the topic 'Eastern Ghats Mobile Belt'
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Journal articles on the topic "Eastern Ghats Mobile Belt"
Biswal, 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.
Full textChetty, T. R. K. "The Eastern Ghats Mobile Belt, India: A Collage of Juxtaposed Terranes (?)." Gondwana Research 4, no. 3 (July 2001): 319–28. http://dx.doi.org/10.1016/s1342-937x(05)70332-4.
Full textNanda, 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.
Full textJana, Niptika, Arun Singh, Ashwani Kant Tiwari, Chandrani Singh, and Rahul Biswas. "Mantle deformation patterns and signatures of rift, beneath Eastern Ghats Mobile Belt." Physics of the Earth and Planetary Interiors 289 (April 2019): 20–33. http://dx.doi.org/10.1016/j.pepi.2019.01.009.
Full textBiswal, T. K., and Suspa Sinha. "Deformation history of the NW salient of the Eastern Ghats Mobile Belt, India." Journal of Asian Earth Sciences 22, no. 2 (October 2003): 157–69. http://dx.doi.org/10.1016/s1367-9120(02)00182-7.
Full textJana, Niptika, Astha Singh, Ashwani Kant Tiwari, Tuna Eken, Arun Singh, Chandrani Singh, and Uma Shankar. "Seismic anisotropy and mantle deformation beneath Eastern Ghats Mobile Belt using direct-S waves." Precambrian Research 360 (July 2021): 106215. http://dx.doi.org/10.1016/j.precamres.2021.106215.
Full textSingh, Saurabh, Rajeev Kumar Pandey, Divya Prakash, and Chandra Kant Singh. "Geochronology of the Polycyclic Granulite Terrain of The Eastern Ghats Mobile Belt: An Overview." JOURNAL OF SCIENTIFIC RESEARCH 66, no. 01 (2022): 33–40. http://dx.doi.org/10.37398/jsr.2022.660104.
Full textSENGUPTA, P., S. DASGUPTA, P. K. BHATTACHARYA, M. FUKUOKA, S. CHAKRABORTI, and S. BHOWMICK. "Petro-tectonic Imprints in the Sapphirine Granulites from Anantagiri, Eastern Ghats Mobile Belt, India." Journal of Petrology 31, no. 5 (October 1, 1990): 971–96. http://dx.doi.org/10.1093/petrology/31.5.971.
Full textChalapathi Rao, N. V. "Glimmeritic enclave in a lamprophyre from the Settupalle alkaline pluton, Eastern Ghats mobile belt." Journal of the Geological Society of India 75, no. 6 (June 2010): 783–90. http://dx.doi.org/10.1007/s12594-010-0073-1.
Full textMahapatro, S. N., A. K. Tripathy, J. K. Nanda, and Abhinaba Roy. "Coexisting ultramylonite and pseudotachylyte from the eastern segment of the Mahanadi shear zone, Eastern Ghats Mobile Belt." Journal of the Geological Society of India 74, no. 6 (December 2009): 679–89. http://dx.doi.org/10.1007/s12594-009-0184-8.
Full textDissertations / Theses on the topic "Eastern Ghats Mobile 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.
Full textSarkar, 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.
Full textNethenzheni, Sedzani Shane. "The geochemistry, geochronology and petrogenetic characteristics of two granitic suites on the eastern margin of the Namaqua Sector, Namaqua-Natal Mobile Belt, South Africa." Thesis, University of the Western Cape, 2016. http://hdl.handle.net/11394/5209.
Full textThe group of granites on the eastern margin of the Mesoproterozoic Namaqua sector of the polydeformed and highly metamorphosed Namaqua-Natal Province of southern Africa is known as the Keimoes Suite. The suite includes mixtures of diverse rock types not belonging to a single intrusive series and so it should be subdivided into more than one intrusive suite. The exact definition, extent, distribution and petrogenesis of these granites have been poorly defined in the past, with various authors defining the suite differently due to the lack of proper geochronology and geochemical data. The exact contact between the Namaqua sector and Kaapvaal Craton together with the role of the suite to the Namaqua tectonic evolution is still unclear. The granites of the Keimoes Suite are thought to mark the contact between the Namaqua sector and the Kaapvaal Craton. This study seeks to address the above mentioned problems by making use of new geochronology, isotope, major and trace element geochemistry together with petrography. The granites of the Keimoes Suite were previously grouped based on their degree of deformation. The geochronology, undertaken as part of this study, has proven that this classification is unfounded. The degree of foliation in these granites appears to be largely controlled by the abundance of platy minerals, such as biotite and muscovite, together with the intrusion mechanism, with deformational processes, such as shearing, playing a secondary role. The geochronology, together with geochemistry has helped to redefine the previously defined Keimoes Suite so that two well defined separate suites are recognized and the third is poorly defined due to lack of more samples of that age group. The new classification or grouping of the granites of the eastern Namaqua sector allows a more detailed examination of the tectonic evolution of this region. A member of the 1225 to 1200 Ma early syn-tectonic granites, the Josling Granite, shows a strongly developed foliation and was derived from a depleted source with a relatively low continental crustal component. This granite intruded during the time of arc accretion, and is associated with, and partly responsible for the D₁ deformation and M₁ metamorphism recognized in most of the rocks of the eastern terranes of the Namaqua sector. In terms of age, the syn-tectonic granites of the Augrabies Suite extend from 1200 to 1120 Ma and were largely derived from depleted sources with variable but more substantial amounts of continental crustal components as compared to the early syn-tectonic granite. The granites of this suite intruded during the period of peak D₂ deformation with peak magmatism between 1180 - 1135 Ma, and particularly around 1150 Ma, during the peak of metamorphism (M₂) caused by, and associated with these voluminous intrusions. The Keimoes Suite can now be defined as comprising granites of late- to post-tectonic age relative to the 1.2 - 1.08 Ga Namaquan Orogeny with magmatism occurring on the western side of the Kaapvaal Craton. The 1116 to 1066 Ma Keimoes Suite intruded during the stage of the Namaquan Orogeny in which there was continued indentation of the Kaapvaal Craton into the Namaqua sector with wrenching and shearing causing the development of rifting into which the granites intruded. The Keimoes Suite granites were derived from continental crustal sources and incorporated varying degrees of depleted source components. The intrusives and extrusives of this age occured after the main collisional event between the Namaqua Sector and the Kaapvaal Craton and are associated with the D₃ deformational event, imparting the thermal conditions leading to the M₃ metamorphic event of the rocks within both the Kakamas and Areachap Terranes. The suites mark the suture between the Archean Kaapvaal Craton and the Proterozoic Namaqua sector. The compositions of the granites of the individual suites were mainly controlled by the source with the degree of partial melting exerting a major control. The proportion of entrained peritectic assemblages and accessory minerals played a major role in controlling the compositions of the granites, particularly those of the trace elements. Variations within the compositions of the same suite are due to source heterogeneities. Generally, fractionation processes played a secondary role in influencing the composition of the granites.
Council for Geoscience and National Research Foundation
Simmat, 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.
Full textGore, R. J. "Geochronological and sedimentological constraints of the Srisailam Formation, S.E. India." Thesis, 2011. http://hdl.handle.net/2440/96125.
Full textThe 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.
Full textThe 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
Books on the topic "Eastern Ghats Mobile 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.
Find full textWorkshop 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.
Find full textBook chapters on the topic "Eastern Ghats Mobile 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.
Full textValdiya, 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.
Full textGupta, 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.
Full textPrakash, 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.
Full textYadav, 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.
Full textVerma, 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.
Full textBose, 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.
Full textSengupta, 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.
Full textSingh, S., and A. K. Prasad. "Delineation of Regional Scale Gold Prospective Zones within the North Singhbhum Mobile Belt, Eastern India: An Integrated Approach Through Geospatial Technologies." In Geospatial Infrastructure, Applications and Technologies: India Case Studies, 413–25. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-2330-0_30.
Full textChetty, 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.
Full textConference papers on the topic "Eastern Ghats Mobile 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.
Full textBehera, 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.
Full textSaikia, 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.
Full textChatterjee, 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.
Full textBanerjee, 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.
Full textElobaid, Elnaiem Ali, Fadhil Sadooni, and Hamad Al Saad. "Tectonic and Geologic Settings of Halul and Al-Alyia Offshore Islands, Examples of Different Evolution Models, Within the Emergence of the Arabian Gulf Geosyncline: A Review." In Qatar University Annual Research Forum & Exhibition. Qatar University Press, 2020. http://dx.doi.org/10.29117/quarfe.2020.0044.
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