nalysis Dorud fault(southwest Iran) using by Morphotectonic and Geomorphologic fans

Geomorphologic indices are used as a tool for identifying new structures and activated influenced by the movement of tectonic. In this study the topographic maps, geology, satellite imagery and digital elevation model (DEM) and IRS satellite images of the region, as the main research data were used....

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Main Authors: zahra kamali, magmodreza Hayhat, hamid nazari, Mohamadmahdi Khatib
Format: Article
Language:fas
Published: University of Sistan and Baluchestan 2018-12-01
Series:جغرافیا و توسعه
Subjects:
Online Access:https://gdij.usb.ac.ir/article_4150_4458c6c0e9bcdce69e6a1d5fb0757101.pdf
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author zahra kamali
magmodreza Hayhat
hamid nazari
Mohamadmahdi Khatib
author_facet zahra kamali
magmodreza Hayhat
hamid nazari
Mohamadmahdi Khatib
author_sort zahra kamali
collection DOAJ
description Geomorphologic indices are used as a tool for identifying new structures and activated influenced by the movement of tectonic. In this study the topographic maps, geology, satellite imagery and digital elevation model (DEM) and IRS satellite images of the region, as the main research data were used. Evidence Morphotectonic indicates that neither the fault that along with passing of units of different ages show different behavior, and the amount of angle Rick obtained along the fault is different according to the results achieved in three segment to different long can be divided, so that angle Rick segments 1 and 2 respectively 16/60° and 22/81° and long segments respectively 18 and 48 kilometer, to notice the high values of Rick (more of 10°) the two segments have a dominant effect of the component dip- slip relative to strike- slip but the angle Rick 2/74° in segment 3 indicate of the action component strike slip that the units alluvial are plain Silakhor this segment long is 44 kilometer ,index associated with alluvial fans, including fan of bending β, fanning coefficient and longitudinal profile was calculated. In the result dates derived from analysis of topography, geomorphology evidence from field observations and the obtained data of geomorphic indicators and survey evidence of active neo-tectonics in the region and the case studied basis of the classification LAT is placed in class 1 that represents is high Neotectonic activities in the area and alluvial fan in the basin is formed in an active tectonic environment.
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spelling doaj.art-ad82ffd8e03d430a981cafd32c4444b02023-06-13T20:22:58ZfasUniversity of Sistan and Baluchestanجغرافیا و توسعه1735-07352676-77912018-12-011653516810.22111/gdij.2018.41504150nalysis Dorud fault(southwest Iran) using by Morphotectonic and Geomorphologic fanszahra kamali0magmodreza Hayhat1hamid nazari2Mohamadmahdi Khatib3دانشجوی دکتری زمین‌شناسی، دانشگاه بیرجند، بیرجند، ایرانAssociate Professor Birjand univetsityدانشیار پژوهشکده علوم زمین، سازمان زمین‌شناسی و اکتشافات معدنی کشور، تهران، ایراناستاد زمین‌شناسی، دانشگاه بیرجند، بیرجند، ایرانGeomorphologic indices are used as a tool for identifying new structures and activated influenced by the movement of tectonic. In this study the topographic maps, geology, satellite imagery and digital elevation model (DEM) and IRS satellite images of the region, as the main research data were used. Evidence Morphotectonic indicates that neither the fault that along with passing of units of different ages show different behavior, and the amount of angle Rick obtained along the fault is different according to the results achieved in three segment to different long can be divided, so that angle Rick segments 1 and 2 respectively 16/60° and 22/81° and long segments respectively 18 and 48 kilometer, to notice the high values of Rick (more of 10°) the two segments have a dominant effect of the component dip- slip relative to strike- slip but the angle Rick 2/74° in segment 3 indicate of the action component strike slip that the units alluvial are plain Silakhor this segment long is 44 kilometer ,index associated with alluvial fans, including fan of bending β, fanning coefficient and longitudinal profile was calculated. In the result dates derived from analysis of topography, geomorphology evidence from field observations and the obtained data of geomorphic indicators and survey evidence of active neo-tectonics in the region and the case studied basis of the classification LAT is placed in class 1 that represents is high Neotectonic activities in the area and alluvial fan in the basin is formed in an active tectonic environment.https://gdij.usb.ac.ir/article_4150_4458c6c0e9bcdce69e6a1d5fb0757101.pdfmorphological"" neotectonic""alluvial fan""fault dorud"
spellingShingle zahra kamali
magmodreza Hayhat
hamid nazari
Mohamadmahdi Khatib
nalysis Dorud fault(southwest Iran) using by Morphotectonic and Geomorphologic fans
جغرافیا و توسعه
morphological"
" neotectonic"
"alluvial fan"
"fault dorud"
title nalysis Dorud fault(southwest Iran) using by Morphotectonic and Geomorphologic fans
title_full nalysis Dorud fault(southwest Iran) using by Morphotectonic and Geomorphologic fans
title_fullStr nalysis Dorud fault(southwest Iran) using by Morphotectonic and Geomorphologic fans
title_full_unstemmed nalysis Dorud fault(southwest Iran) using by Morphotectonic and Geomorphologic fans
title_short nalysis Dorud fault(southwest Iran) using by Morphotectonic and Geomorphologic fans
title_sort nalysis dorud fault southwest iran using by morphotectonic and geomorphologic fans
topic morphological"
" neotectonic"
"alluvial fan"
"fault dorud"
url https://gdij.usb.ac.ir/article_4150_4458c6c0e9bcdce69e6a1d5fb0757101.pdf
work_keys_str_mv AT zahrakamali nalysisdorudfaultsouthwestiranusingbymorphotectonicandgeomorphologicfans
AT magmodrezahayhat nalysisdorudfaultsouthwestiranusingbymorphotectonicandgeomorphologicfans
AT hamidnazari nalysisdorudfaultsouthwestiranusingbymorphotectonicandgeomorphologicfans
AT mohamadmahdikhatib nalysisdorudfaultsouthwestiranusingbymorphotectonicandgeomorphologicfans