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摘要:
Atrak River region, northeast Iran is a quaternary tectonically active region. There are many geologic structures that they are formed by the collision of the Arabian and Eurasian plates. This area has extended from north east Iran to the of kope dagh zone. The study area is Atrak river basin and it has been divided to 56 Sub-basin for calculation of 6 geomorphic indices. Finally, this region was classified in 4 relative tectonic activity classes.
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篇名 Tectonic Geomorphology of Atrak River, NE Iran
来源期刊 地质学期刊(英文) 学科 医学
关键词 Atrak Kope Dagh GEOMORPHOLOGY RIVER BASIN Iran
年,卷(期) 2015,(3) 所属期刊栏目
研究方向 页码范围 106-114
页数 9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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Atrak
Kope
Dagh
GEOMORPHOLOGY
RIVER
BASIN
Iran
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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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0
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