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Information Journal Paper

Title

TSUNAMI IN OMAN SEA

Pages

  33-46

Abstract

 The earthquakes in MAKRAN and OMAN SEA and the historical Tsunamies such as one that happened on 27 November 1945 in MAKRAN coast are main reasons for insecurity because of Tsunamie's wave affected in the mentioned area. Also the geophysical interpretation supports this fact. Because of various seismic in this region; it is divided into two areas in this research.The data of earthquakes were used in the current century and historical earthquakes to estimate the Gutenberg–Rishter parameters and the earthquake cycle (recurrence intervals).The DISTRIBUTION OF SEISMIC ENERGY released have been drown and analysed. By depth information, slop state of deposit has been analysed and the SPEED OF TSUNAMI in different places in comparison with different depths of OMAN SEA has been evaluated. Landslide possibility and height of Tsunamie's wave have been compared in different coast of the OMAN SEA.

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    Cite

    APA: Copy

    AZIMI, FERDOS. (2008). TSUNAMI IN OMAN SEA. JOURNAL OF THE EARTH, 3(1), 33-46. SID. https://sid.ir/paper/193074/en

    Vancouver: Copy

    AZIMI FERDOS. TSUNAMI IN OMAN SEA. JOURNAL OF THE EARTH[Internet]. 2008;3(1):33-46. Available from: https://sid.ir/paper/193074/en

    IEEE: Copy

    FERDOS AZIMI, “TSUNAMI IN OMAN SEA,” JOURNAL OF THE EARTH, vol. 3, no. 1, pp. 33–46, 2008, [Online]. Available: https://sid.ir/paper/193074/en

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