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The Analysis of Transverse Topographic Symmetry Factor (T Index) in the Chekene-Mazavand, North East Iran

机译:伊朗东北部Chekene-Mazavand的横向地形对称因子(T指数)分析

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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.
机译:T指数是在伊朗东北部的Chekene-Mazavand地区计算得出的。该指数表明横向倾斜可能与活动构造有关。卡沙弗罗德河的所有河流都有许多溪流,并且已经计算出横向地形对称因子。首先,基于数字高程模型,将研究区域划分为28个子流域。然后为每个计算横向地形对称因子。该值在0.14至0.57之间,因此,相对的构造活动水平较低,中等和较高。在子盆地中没有发现构造活动相对较低的地区。 14、15和24,在sub-basinsno发现中等程度的相对构造活动。 2、5、6、7、9、10、13、16、18、19、21、22、23、25、27和28以及在盆地中发现的相对构造活动较高。 1、3、4、8、11、12、17、20和26。结果表明,平原地区的构造活动程度低至中等,而断层地区的构造活动程度较高。这件事与其在伊朗东北部的科佩特大带的构造背景相符。

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