Browsing by Author "Shuhail, M."
Now showing items 1-5 of 5
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Formation and evolution of the Chain-Kairali Escarpment and the Vishnu Fracture Zone in the Western Indian Ocean
Shuhail, M.; Yatheesh, V.; Bhattacharya, G.C.; Muller, R.D.; KameshRaju, K.A.; Mahender, K. (Elsevier, 2018)Published models for the plate tectonic evolution of the Western Indian Ocean suggest that the Southern Mascarene Basin opened by oceanic crustal accretion between the continental margins of southwestern India and southeastern ... -
Morphotectonics of the Raman-Panikkar-Wadia seamount chain in the Laxmi Basin, Eastern Arabian Sea
Savio, J.J.; Yatheesh, V.; Bijesh, C.M.; Mahender, K.; Aswini, K.K.; Badesab, F.K.; Shuhail, M.; Sriram, G.; Twinkle, D.; Kumar, Raj (Elsevier, 2024)The Laxmi Basin, which is a deep ocean basin situating adjoining to the northwestern continental margin of India, contains a linear seamount chain consisting of the Raman Seamount, Panikkar Seamount and the Wadia Guyot, ... -
Nature of the Ambient Noise, Site Response, and Orientation of Ocean?Bottom Seismometers (OBSs): Scientific Results of a Passive Seismic Experiment in the Andaman Sea
Dewangan, P.; Reddy, R.; KameshRaju, K.A.; Singha, P.; Aswini, K.K.; Yatheesh, V.; Samudrala, K.; Shuhail, M. (Seismological Society of America, 2018)We analyze the nature of the ambient noise and site response for ocean?bottom seismometers (OBSs) deployed in the Andaman region. The probabilistic power spectral densities of the OBSs show that the noise level in the ... -
Plate tectonic reconstruction of India and Madagascar closing through the Mascarene Basin
Shuhail, M. (Ocean Society of India, 2015)The western continental margin of India was formed due to the rifting and drifting among India, Madagascar and Seychelles. Several researchers provided relative configuration of India and Madagascar in their pre-break-up ... -
The tectonic stress field evolution of India since the Oligocene
Müller, R.D.; Yatheesh, V.; Shuhail, M. (Elsevier, 2015)A multitude of observations suggest neotectonic deformation in and around India, but its causes and history are unknown. We use a 2 dimensional finite element model with heterogeneous elastic strengths in continental regions ...