SALT DIAPIRS OF IRAN AS A GEOMORPHOLOGICAL UNIT

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SERVATI M.R.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Journal: Desert Year:2001 | Volume:6 | Issue:1 Page(s): 87-106

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Title

SALT DIAPIRS OF IRAN AS A GEOMORPHOLOGICAL UNIT

Author(s)

SERVATI M.R. | Issue Writer Certificate

Keywords

GEOMORPHOLOGYQ3

SALT DOMEQ2

LANDFORMQ3

SOLUTIONQ4

SALT GLACIERSQ4

Abstract

Domal structures produced by intrusion of salt into rock strata, are one of the most important geomorphological unit of the earth surface in Iran. The main area of these LANDFORMes is folded and thrust zones of Zagros - Range and central - Iran. They are dated back from Precambrian to nebgene age. These salt plugs are a mixed up & complex assemblage of various magmatic, sedimentary & metamorphic rocks which have been cut, replaced, mixed, disordered along up lifting. The occurrence of these Diapirs is due to the main stress from tectonic activity and buyonancy effect of salt masses. There are exposed and hidden diapers in Iran and they have oval, circular, irregular dome, and etc. shapes. In SALT DOMEs, SOLUTION is a dominant process in LANDFORM development with resulting production of Karst Topography. In many SALT DOMEs, salt has moved downhill on the form of the salt flows or glaciers. Salt diapirs of Iran are a wonderfull landscape and they have economic significance.

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APA: Copy

SERVATI, M.R.. (2001). SALT DIAPIRS OF IRAN AS A GEOMORPHOLOGICAL UNIT. DESERT (BIABAN), 6(1), 87-106. SID. https://sid.ir/paper/5382/en

Vancouver: Copy

SERVATI M.R.. SALT DIAPIRS OF IRAN AS A GEOMORPHOLOGICAL UNIT. DESERT (BIABAN)[Internet]. 2001;6(1):87-106. Available from: https://sid.ir/paper/5382/en

IEEE: Copy

M.R. SERVATI, “SALT DIAPIRS OF IRAN AS A GEOMORPHOLOGICAL UNIT,” DESERT (BIABAN), vol. 6, no. 1, pp. 87–106, 2001, [Online]. Available: https://sid.ir/paper/5382/en

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