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摘要:
T index has been calculated in the Chekene-Mazavand region in the NE Iran. This index shows lateral tilting may be related to active tectonics. There are many streams and transverse topographic symmetry factor has been calculated for all streams of Kashafroud river. Firstly, based on digital elevation model, the study area was divided into 28 sub-basins. Then transverse topographic symmetry factor was calculated for each one. The values are between 0.14 and 0.57 and so, there are low, moderate and high levels of relative tectonic activities. The areas with low relative tectonic activities have found in sub-basins?no. 14, 15 and 24, moderate relative tectonic activities have found in sub-basinsno. 2, 5, 6, 7, 9, 10, 13, 16, 18, 19, 21, 22, 23, 25, 27 and 28 and high relative tectonic activities have found in sub-basins?no. 1, 3, 4, 8, 11, 12, 17, 20 and 26. The results show that the?plains have got low to moderate level of tectonic activity and faulted areas have got high tectonic activity. This matter is compatible with its tectonic setting on the Kopet Dagh belt in north east Iran.
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篇名 The Analysis of Transverse Topographic Symmetry Factor (T Index) in the Chekene-Mazavand, North East Iran
来源期刊 地质学期刊(英文) 学科 医学
关键词 TRANSVERSE Topographic SYMMETRY FACTOR Chekene-Mazavand TECTONIC Iran
年,卷(期) 2015,(11) 所属期刊栏目
研究方向 页码范围 809-820
页数 12页 分类号 R73
字数 语种
DOI
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研究主题发展历程
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TRANSVERSE
Topographic
SYMMETRY
FACTOR
Chekene-Mazavand
TECTONIC
Iran
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研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
地质学期刊(英文)
月刊
2161-7570
武汉市江夏区汤逊湖北路38号光谷总部空间
出版文献量(篇)
585
总下载数(次)
0
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0
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