Zobrazeno 1 - 10 of 39 pro vyhledávání: '"K A Kamesh Raju"'
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Akademický článek
Megafaunal community structure of Andaman seamounts including the Back-arc Basin--a quantitative exploration from the Indian Ocean.
Autor: Sabyasachi Sautya, Baban Ingole, Durbar Ray, Sabine Stöhr, Kiranmai Samudrala, K A Kamesh Raju, Abhay Mudholkar
Publikováno v: PLoS ONE, Vol 6, Iss 1, p e16162 (2011)
Species rich benthic communities have been reported from some seamounts, predominantly from the Atlantic and Pacific Oceans, but the fauna and habitats on Indian Ocean seamounts are still poorly known. This study focuses on two seamounts, a submarine
Externí odkaz: https://doaj.org/article/acfb13bc77a144b59c1c02c15ee1bc3c
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2
Microbathymetry inferences from two AUV dives over a short segment of the Central Indian Ridge between 10°18′ and 10°57′S, Indian Ocean
Autor: K. A. Kamesh Raju, V. Yatheesh, A. Srinivas Rao, L. Surya Prakash, Durbar Ray, Abhay Mudholkar, Kiranmai Samudrala, Nico Augustin, P. John Kurian
The topographic fabric of the rift valley floor has been analyzed using the multibeam echosounder data obtained by the autonomous underwater vehicle (AUV) Abyss at two locations over a short segment of the slow-spreading Central Indian Ridge between
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::df6e71a25cd158a6b4749261dd79a775
https://link.springer.com/article/10.1007/s00367-022-00742-x
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4
An integrated geophysical study east of the southern Chagos Laccadive Ridge Complex, Central Indian Ocean Basin: Implications for the Rodriguez Triple Junction dynamics in the Late Cretaceous
Autor: K. A. Kamesh Raju, T. Ramprasad, M. Desa
Publikováno v: Marine Geology. 414:47-63
The Central Indian Ocean Basin, east of the southern Chagos Laccadive Ridge complex has evolved due to seafloor spreading in the N-S direction since the Late Cretaceous. The trace of the Rodriguez Triple Junction (RTJ) has been inferred in this basin
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3209b35d165ae6b5413d5448c725b326
https://doi.org/10.1016/j.margeo.2019.05.007
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5
Detailed Structure and Plate Reconstructions of the Central Indian Ocean Between 83.0 and 42.5 Ma (Chrons 34 and 20)
Autor: G.C. Bhattacharya, Jean-Yves Royer, K. A. Kamesh Raju, Y. Choi, V. Yatheesh, Philippe Patriat, K. Srinivas, T. Ramprasad, A.K. Chaubey, Jérôme Dyment
Publikováno v: Journal of Geophysical Research : Solid Earth
Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2019, 124 (5), pp.4305-4322. ⟨10.1029/2018JB016812⟩
Journal Of Geophysical Research-solid Earth (2169-9313) (Amer Geophysical Union), 2019-05, Vol. 124, N. 5, P. 4305-4322
International audience; The Central Indian Ocean, namely the Central Indian, Crozet, and Madagascar basins, formed by rifting and subsequent drifting of India (now Capricorn), Antarctica, and Africa (now Somalia). We gathered a comprehensive set of s
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ea852384da480abaf0be7a2676b0bc3d
https://doi.org/10.1029/2018jb016812
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7
Sub-surface magma movement inferred from low-frequency seismic events in the off-Nicobar region, Andaman Sea
Autor: K. K. Aswini, V. Yatheesh, Pabitra Singha, T. Ramakrushana Reddy, K. A. Kamesh Raju, Lalit Arya, Pawan Dewangan
Publikováno v: Scientific Reports
Monitoring volcanic activity along the submarine volcanoes that are usually induced by subsurface magmatism is a challenge. We present fresh set of Ocean Bottom Seismometer (OBS) data that shows geophysical evidence indicative of subsurface magmatism
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6211b72ff2c3518f7800f90bc27d476
http://europepmc.org/articles/PMC7719189
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8
Late Quaternary Sedimentation and Slope Failure Events on the Costa Rican Margin
Autor: B. Nagender Nath, V. Yatheesh, A. Kazip Yazing, Avinash Borker, K. A. Kamesh Raju, Surabhi R. Prabhu, Dhananjai Pandey
Publikováno v: Dynamics of the Earth System: Evolution, Processes and Interactions ISBN: 9783030406585
The Costa Rican margin is an erosional convergent margin formed by subduction of the Cocos Plate under the Caribbean Plate along the Middle America Trench. The Integrated Ocean Drilling Program (IODP) Expedition 334 was conducted for drilling long se
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6fef7cbecbc5490ee16721a6cfe0a08f
https://doi.org/10.1007/978-3-030-40659-2_9
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9
Tectonics of the Andaman Backarc Basin—Present Understanding and Some Outstanding Questions
Autor: K. K. Aswini, K. A. Kamesh Raju, V. Yatheesh
Publikováno v: Society of Earth Scientists Series ISBN: 9783030398422
The Andaman Backarc Basin is characterized by active seafloor spreading spurred by the right stepping dextral shear imposed on the trans-basinal Sagaing-Andaman-Nicobar- Sumatra fault system and presents a complex tectonic history owing to some uniqu
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::24bb82d212245470c946c899fc7d7055
https://doi.org/10.1007/978-3-030-39843-9_12
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