Zobrazeno 1 - 10
of 54
pro vyhledávání: '"V. Vijaya Rao"'
Autor:
V. Vijaya Rao, Damodara Nara
Publikováno v:
Geosystems and Geoenvironment, Vol 1, Iss 4, Pp 100071- (2022)
Cratons are the stable portions of the continents for at least the past two billion years. Their longevity is generally attributed to their thick, cold, rheologically strong and chemically depleted subcrustal mantle lithosphere. The lithosphere achie
Externí odkaz:
https://doaj.org/article/a4b0e1c46a204b02826b168c715d7966
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-14 (2021)
Abstract Plateaus, located far away from the plate boundaries, play an important role in understanding the deep-rooted geological processes responsible for the epeirogenic uplift and dynamics of the plate interior. The Karnataka plateau located in th
Externí odkaz:
https://doaj.org/article/d950132f7a0c44d498bbd7a39d8c10f3
Autor:
Damodara Nara, V. Vijaya Rao
Publikováno v:
Geological and Geo-Environmental Processes on Earth ISBN: 9789811641213
The Earth is a dynamic planet with a large number of geological processes taking place inside it. The internal processes lift and build the Earth’s surface, whereas the external processes tend to destroy the shape of the Earth’s relief by weather
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca12f396f1e38f97782e91c8cceaf6bb
https://doi.org/10.1007/978-981-16-4122-0_5
https://doi.org/10.1007/978-981-16-4122-0_5
Publikováno v:
Scientific Reports
Scientific Reports, Vol 11, Iss 1, Pp 1-14 (2021)
Scientific Reports, Vol 11, Iss 1, Pp 1-14 (2021)
Plateaus, located far away from the plate boundaries, play an important role in understanding the deep-rooted geological processes responsible for the epeirogenic uplift and dynamics of the plate interior. The Karnataka plateau located in the Dharwar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a3da71e0ba5338215b7900991a886eef
https://pubmed.ncbi.nlm.nih.gov/33452325
https://pubmed.ncbi.nlm.nih.gov/33452325
Autor:
Y. J. Bhaskar Rao, V. Vijaya Rao, Sree Bhushan Raju, Mrinal K. Sen, D. Sarkar, P. Karuppannan, Biswajit Mandal
Publikováno v:
Geophysical Journal International. 212:777-794
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b527fce40d1f15c4f6c43cbda81cc564
https://doi.org/10.1093/gji/ggx427
https://doi.org/10.1093/gji/ggx427
Publikováno v:
Precambrian Research. 356:106110
The East Gondwana was formed by the assembly of continental fragments, namely India, Madagascar, Sri Lanka, and Antarctica, with the evolution of 2000 km long East African Orogen around 550 Ma. Lack of knowledge on the subsurface structure of the oro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4829f5cdb3899fbcf8bbe22c53052db3
https://doi.org/10.1016/j.precamres.2021.106110
https://doi.org/10.1016/j.precamres.2021.106110
Akademický článek
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Publikováno v:
Geophysical Journal International. 208:1490-1507
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::24704c5857d54a60676bb50fb638e938
https://doi.org/10.1093/gji/ggw461
https://doi.org/10.1093/gji/ggw461
Autor:
V. Vijaya Rao, N. Prem Kumar, Dipankar Sarkar, A. S. N. Murty, V. Sridher, Y. J. Bhaskar Rao, Prakash Khare, Mrinal K. Sen, A. S. S. S. R. S. Prasad, S. Raju, Gautam Rao, Karuppannan
Publikováno v:
Precambrian Research. 266:282-295
The Dharwar Craton in the southern part of the Indian shield comprises two distinct blocks viz. the Meso-Neoarchean western and the predominantly Neoarchean eastern blocks, which are popularly referred to as Western Dharwar Craton (WDC) and Eastern D
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::26f472bdd8997903dd4be2010d190e45
https://doi.org/10.1016/j.precamres.2015.05.006
https://doi.org/10.1016/j.precamres.2015.05.006
Publikováno v:
Geophysical Journal International. 200:652-663
Imaging shallow crustal structure is essential to extend the geological information from surface mapping to a depth and to develop tectonic models. We applied seismic tomography modelling to refraction data acquired along a 200-km-long line in the Dh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::757f8dfac82df45f03fbf9f999803870
https://doi.org/10.1093/gji/ggu425
https://doi.org/10.1093/gji/ggu425