AN EVALUATION OF THE TYPE OF SEDIMENTARY ENVIRONMENT IN ISFAHAN REGION AND ZAYANDEHRUD RIVER AVULSION

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SOLTANI KOUPAEI S.

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Journal Paper

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Journal: IRANIAN JOURNAL OF NATURAL RESOURCES Year:2004 | Volume:56 | Issue:4 Page(s): 351-364

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Information Journal Paper

Title

AN EVALUATION OF THE TYPE OF SEDIMENTARY ENVIRONMENT IN ISFAHAN REGION AND ZAYANDEHRUD RIVER AVULSION

Author(s)

SOLTANI KOUPAEI S. | Issue Writer Certificate

Keywords

SEDIMENTARY ENVIRONMENTQ4

ALLUVIAL FANQ4

BARQ4

FLUVIAL ENVIRONMENTQ4

QUATERNARYQ4

TECTONICQ4

SEDIMENTARY LOADQ4

MID CHANNEL BARQ4

Abstract

This study has revealed that Isfahan region is a FLUVIAL ENVIRONMENT rather than an ALLUVIAL FAN. Morphology of the region shows a mid channel BAR and island. In the past, after Zyandehrud entered Isfahan, it was divided into two branches due to impact against Atomic energy mountains, decreasing bed slope, as well as remarkably widening the riverbed. The above feature has accumulated considerable amount of sedimentation in front of Atomic energy mountains and has formed the mid channel BAR. Topographic map of Isfahan, indicates a talweg in northern part of the region. This talweg is known as the old branch of Zayandehrud. Increasing SEDIMENTARY LOAD and uplifting of the river bed has eliminated this branch from Zayandehrud.

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References

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APA: Copy

SOLTANI KOUPAEI, S.. (2004). AN EVALUATION OF THE TYPE OF SEDIMENTARY ENVIRONMENT IN ISFAHAN REGION AND ZAYANDEHRUD RIVER AVULSION. IRANIAN JOURNAL OF NATURAL RESOURCES, 56(4), 351-364. SID. https://sid.ir/paper/22990/en

Vancouver: Copy

SOLTANI KOUPAEI S.. AN EVALUATION OF THE TYPE OF SEDIMENTARY ENVIRONMENT IN ISFAHAN REGION AND ZAYANDEHRUD RIVER AVULSION. IRANIAN JOURNAL OF NATURAL RESOURCES[Internet]. 2004;56(4):351-364. Available from: https://sid.ir/paper/22990/en

IEEE: Copy

S. SOLTANI KOUPAEI, “AN EVALUATION OF THE TYPE OF SEDIMENTARY ENVIRONMENT IN ISFAHAN REGION AND ZAYANDEHRUD RIVER AVULSION,” IRANIAN JOURNAL OF NATURAL RESOURCES, vol. 56, no. 4, pp. 351–364, 2004, [Online]. Available: https://sid.ir/paper/22990/en

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