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Cites:

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Information Journal Paper

Title

TECTONIC GEOMORPHOLOGY OF SALT STRUCTURES IN THE GARMSAR- LASJERD AREA

Pages

  75-84

Abstract

 Evaporitic (diapiric) bodies of the Garmsar-Lasjerd area have been investigated. Halokinesis is the trigger of DIAPIRISM but, early Pliocene OROGENIC PHASE, has been distinguished as an external trigger to diapiric development. On the other hand, SALT STRUCTURES of investigation area that have been emergent by fault generally, classified to four types: Salt stocks, Salt welts, Salt walls, Salt tongues.

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  • Cite

    APA: Copy

    ASADIAN, FARIDEH, POURKERMANI, M., & ARIAN, M.. (2007). TECTONIC GEOMORPHOLOGY OF SALT STRUCTURES IN THE GARMSAR- LASJERD AREA. GEOGRAPHICAL RESEARCH QUARTERLY, 39(60), 75-84. SID. https://sid.ir/paper/382088/en

    Vancouver: Copy

    ASADIAN FARIDEH, POURKERMANI M., ARIAN M.. TECTONIC GEOMORPHOLOGY OF SALT STRUCTURES IN THE GARMSAR- LASJERD AREA. GEOGRAPHICAL RESEARCH QUARTERLY[Internet]. 2007;39(60):75-84. Available from: https://sid.ir/paper/382088/en

    IEEE: Copy

    FARIDEH ASADIAN, M. POURKERMANI, and M. ARIAN, “TECTONIC GEOMORPHOLOGY OF SALT STRUCTURES IN THE GARMSAR- LASJERD AREA,” GEOGRAPHICAL RESEARCH QUARTERLY, vol. 39, no. 60, pp. 75–84, 2007, [Online]. Available: https://sid.ir/paper/382088/en

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