Tectonic-Geomorphology Analysis in Dorungar River

Dorungar River Basin is located at  Koppet Dagh Mountains in the north of Khorasan Razavi. Basin.  Geomorphologic evidences show the continuousness of neo-tectonic activities in the Polio-Quaternary era. The purpose of this study is to evaluate active neo-tectonic area and to compare the results of...

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Main Authors: saeedeh Azam Mabaqi, Seyedreza Hosseinzadeh
Format: Article
Language:fas
Published: University of Sistan and Baluchestan 2017-12-01
Series:جغرافیا و توسعه
Subjects:
Online Access:https://gdij.usb.ac.ir/article_3458_c55b34563019593fe3b837f637d972f4.pdf
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author saeedeh Azam Mabaqi
Seyedreza Hosseinzadeh
author_facet saeedeh Azam Mabaqi
Seyedreza Hosseinzadeh
author_sort saeedeh Azam Mabaqi
collection DOAJ
description Dorungar River Basin is located at  Koppet Dagh Mountains in the north of Khorasan Razavi. Basin.  Geomorphologic evidences show the continuousness of neo-tectonic activities in the Polio-Quaternary era. The purpose of this study is to evaluate active neo-tectonic area and to compare the results of geomorphic index and geomorphologic evidences such as Modern fault escarpments, lack of foothill, premorse and translocation alluvial fan, drainage basin asymmetry in Dorungar River, rejuvenation terrace and river and its influence on the river drainage network. The study used Landforms’ field visit, geomorphic index (Hi, Bs, AF, Smf, S, VF and SL), IAT classifying indices, topography & geology maps, Remote sensing images and Dem to analyze the neo-tectonic activities in the area. Results showed that the data acquired by geomorphic index and analyzed Geomorphologic evidence, proves that neo-tectonic in the area is active; and based on IAT classifying indices, the area is one of the active area neo-tectonically.
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spelling doaj.art-050c3a25b2c34456b89729a104d8c3d02023-06-13T20:22:10ZfasUniversity of Sistan and Baluchestanجغرافیا و توسعه1735-07352676-77912017-12-01154916318810.22111/gdij.2017.34583458Tectonic-Geomorphology Analysis in Dorungar Riversaeedeh Azam Mabaqi0Seyedreza Hosseinzadeh1دانش آموخته ژئومورفولوژی دانشگاه فردوسی مشهددانشیار ژئومورفولوژی دانشگاه فردوسی مشهدDorungar River Basin is located at  Koppet Dagh Mountains in the north of Khorasan Razavi. Basin.  Geomorphologic evidences show the continuousness of neo-tectonic activities in the Polio-Quaternary era. The purpose of this study is to evaluate active neo-tectonic area and to compare the results of geomorphic index and geomorphologic evidences such as Modern fault escarpments, lack of foothill, premorse and translocation alluvial fan, drainage basin asymmetry in Dorungar River, rejuvenation terrace and river and its influence on the river drainage network. The study used Landforms’ field visit, geomorphic index (Hi, Bs, AF, Smf, S, VF and SL), IAT classifying indices, topography & geology maps, Remote sensing images and Dem to analyze the neo-tectonic activities in the area. Results showed that the data acquired by geomorphic index and analyzed Geomorphologic evidence, proves that neo-tectonic in the area is active; and based on IAT classifying indices, the area is one of the active area neo-tectonically.https://gdij.usb.ac.ir/article_3458_c55b34563019593fe3b837f637d972f4.pdfneo tectonicgeomorphic indexgisgeomorphologic evidencedorungar river basin
spellingShingle saeedeh Azam Mabaqi
Seyedreza Hosseinzadeh
Tectonic-Geomorphology Analysis in Dorungar River
جغرافیا و توسعه
neo tectonic
geomorphic index
gis
geomorphologic evidence
dorungar river basin
title Tectonic-Geomorphology Analysis in Dorungar River
title_full Tectonic-Geomorphology Analysis in Dorungar River
title_fullStr Tectonic-Geomorphology Analysis in Dorungar River
title_full_unstemmed Tectonic-Geomorphology Analysis in Dorungar River
title_short Tectonic-Geomorphology Analysis in Dorungar River
title_sort tectonic geomorphology analysis in dorungar river
topic neo tectonic
geomorphic index
gis
geomorphologic evidence
dorungar river basin
url https://gdij.usb.ac.ir/article_3458_c55b34563019593fe3b837f637d972f4.pdf
work_keys_str_mv AT saeedehazammabaqi tectonicgeomorphologyanalysisindorungarriver
AT seyedrezahosseinzadeh tectonicgeomorphologyanalysisindorungarriver