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Information Journal Paper

Title

SEA LEVEL CHANGE INTERPRETATION OF CASPIAN SEA BY USING MAGNETIC SUSCEPTIBILITY DATA OF BOTTOM SEDIMENTS

Pages

  41-59

Abstract

 In this survey, in order to sedimentological studies and determine the CASPIAN SEA level fluctuations by variations in magnetic susceptibilities of the Caspian BOTTOM SEDIMENTS, 5 cores were taken from southeastern basin of the CASPIAN SEA. These samples have been analyzed for grain size, total organic carbon content, carbonate content, mineral composition and MAGNETIC SUSCEPTIBILITY. The results show a close relation between particle size distribution and MS magnitude due to variation in detrital influx, caused by SEA-LEVEL FLUCTUATIONS in different time. This process is reflected in increasing particle size and magnitude of MS simultaneously with sealevel rise and decreasing particle size and magnitude of MS simultaneously with sea-level fall. However such a relationship between magnitude of MS and carbonate and total organic carbon was not observed.

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    APA: Copy

    SHAHKARAMI, S., RAHIMPOUR BONAB, H., ALIZADEH KETEK LAHIJANI, H., LEROY, S., & SHAHHOSSEINI, M.. (2009). SEA LEVEL CHANGE INTERPRETATION OF CASPIAN SEA BY USING MAGNETIC SUSCEPTIBILITY DATA OF BOTTOM SEDIMENTS. SEDIMENTARY FACIES, 2(1), 41-59. SID. https://sid.ir/paper/199843/en

    Vancouver: Copy

    SHAHKARAMI S., RAHIMPOUR BONAB H., ALIZADEH KETEK LAHIJANI H., LEROY S., SHAHHOSSEINI M.. SEA LEVEL CHANGE INTERPRETATION OF CASPIAN SEA BY USING MAGNETIC SUSCEPTIBILITY DATA OF BOTTOM SEDIMENTS. SEDIMENTARY FACIES[Internet]. 2009;2(1):41-59. Available from: https://sid.ir/paper/199843/en

    IEEE: Copy

    S. SHAHKARAMI, H. RAHIMPOUR BONAB, H. ALIZADEH KETEK LAHIJANI, S. LEROY, and M. SHAHHOSSEINI, “SEA LEVEL CHANGE INTERPRETATION OF CASPIAN SEA BY USING MAGNETIC SUSCEPTIBILITY DATA OF BOTTOM SEDIMENTS,” SEDIMENTARY FACIES, vol. 2, no. 1, pp. 41–59, 2009, [Online]. Available: https://sid.ir/paper/199843/en

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