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摘要:
The study area?is located in the north Tehran, Iran. Calculation of transverse topographic symmetry factor (T) is suitable for rapid assessment of active tectonics. Therefore, transverse topographic symmetry factors have?beencalculated for the Darakeh stream. The study area is located in the Tehran Piedmont and transverse topographic symmetry factor?is calculated for it. Based on values of this index, there is high relative tectonic activity level. This condition can be related to existence of a blind north-south striking fault which it may be buried by alluvium of the Darakeh stream. Dendritic drainage pattern of Darakeh stream and the fact that the western tributaries are longer than the eastern tributaries provide indirect evidence of ground tilting toward the east. Also, based on our results, most part of the study area have got high tectonic activity that it is compatible with its tectonic setting on the Tehran in north Iran.
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篇名 The Transverse Topographic Symmetry Factor of Darakeh Stream in the North Tehran, Iran
来源期刊 地质学期刊(英文) 学科 医学
关键词 TRANSVERSE Topographic SYMMETRY FACTOR Darakeh TEHRAN Iran
年,卷(期) 2015,(11) 所属期刊栏目
研究方向 页码范围 770-779
页数 10页 分类号 R73
字数 语种
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研究主题发展历程
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TRANSVERSE
Topographic
SYMMETRY
FACTOR
Darakeh
TEHRAN
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
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585
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