Results 131 to 140 of about 196 (164)
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Deep structure of the western coast of the Makran subduction zone, SE Iran
Tectonophysics, 2020Abstract The Makran subduction zone is one of the world's least well documented active subduction zones. We investigate the geometry of subsurface velocity interfaces across the western coastal Makran by means of teleseismic data for the first time. The data were gathered by two permanent and four temporary seismic stations.
Esmaeil Shabanian, Khalil Motaghi
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Environmental Monitoring and Assessment, 2018
Coastal tsunami amplitudes were calculated to identify areas susceptible to tsunami hazard at selected locations of the coast of Karnataka, west of India, due to earthquakes in the Makran Subduction Zone. This is the first time that the probabilistic tsunami hazard assessment along this study area has been attempted.
K S Jayappa, Sowmya K
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Coastal tsunami amplitudes were calculated to identify areas susceptible to tsunami hazard at selected locations of the coast of Karnataka, west of India, due to earthquakes in the Makran Subduction Zone. This is the first time that the probabilistic tsunami hazard assessment along this study area has been attempted.
K S Jayappa, Sowmya K
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Coastal boulders as evidence for high-energy waves on the Iranian coast of Makran
Marine Geology, 2011Abstract Coastal boulder deposits attesting to large waves are found along the rocky coast of Makran (Iran) from Chabahar to Lipar. Boulders are either scattered on the rocky coastal platform or accumulated in imbricated clusters. The boulders are mostly rectangular and composed of biogenic calcarenite deriving from the present coastal platform ...
Hamid Alizadeh Lahijani +2 more
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Marine Geodesy, 2011
While in recent years much attention has been focused on tsunamis in the Indian Ocean, generated near Indonesia, equally destructive tsunamis also could occur in the western part of the North Indian Ocean. Specifically, the last major tsunami in the Arabian Sea occurred in November 1945 due to an earthquake that originated in the Makran region.
T N Prakash, M V Ramana Murthy
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While in recent years much attention has been focused on tsunamis in the Indian Ocean, generated near Indonesia, equally destructive tsunamis also could occur in the western part of the North Indian Ocean. Specifically, the last major tsunami in the Arabian Sea occurred in November 1945 due to an earthquake that originated in the Makran region.
T N Prakash, M V Ramana Murthy
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Tectonophysics, 1979
(Accepted for publication June 8, 1978) ABSTRACT: Page, W.D., Alt, J.N., Cluff, L.S. and Plafker, G., 1979. Evidence for the recurrence of large-magnitude earthquakes along the Makran coast of Iran and Pakistan. In: C.A. Whitten, R. Green and B.K. Meade (Editors), Recent Crustal Movements, 1977. Tectonophysics, 52: 533-547.
George Plafker
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(Accepted for publication June 8, 1978) ABSTRACT: Page, W.D., Alt, J.N., Cluff, L.S. and Plafker, G., 1979. Evidence for the recurrence of large-magnitude earthquakes along the Makran coast of Iran and Pakistan. In: C.A. Whitten, R. Green and B.K. Meade (Editors), Recent Crustal Movements, 1977. Tectonophysics, 52: 533-547.
George Plafker
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Geological footprints of the 1945 Makran tsunami from the west coast of India
Marine Geology, 2022Archana Das +2 more
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A Preliminary Survey of Seaweeds from the Coast of Makran, Pakistan
Botanica Marina, 1996M Shameel, K Aisha
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Geology and Petroleum Potential of the Makran Coast, Pakistan
Proceedings of Offshore South East Asia Show, 1982Coastal Makran is generally acknowledged as a subduction zone where the Indian Ocean plate moves northward under continental crust. The geologic history deduced from facies and structures is complex and can be divided into three major episodes :A Middle Miocene and older phase dominated by turbidity currentdeposition on a vast deep-sea fan which ...
J.C. Harms, D.C. Francis
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Microplastics in the surface seawaters of Chabahar Bay, Gulf of Oman (Makran Coasts)
Marine Pollution Bulletin, 2019Current study aimed to evaluate the microplastics abundance in the surface waters of Chabahar Bay for the first time. 21 neuston net water samples were collected from 7 stations. Microplastics were visually counted by stereomicroscope, sorted into 4 size categories, 4 shape categories, and identified by ATR-FTIR spectroscopy.
Mojgan Khamarzadeh, Aliabad +2 more
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