In this study, we have examined the morphology of alluvial fans, and this examination has taken place in Meyamey fault zone located on the southern slopes of the eastern Alborz and Central Iran. The reason of this study is learned about the young tectonic activity on that area.
Semnan is located in northern Iran, and Shahrud-Bastam is located in the north to the North East. The geographical location of the study area is 54˚30'00'' to 55˚30'00'' east longitude and 36˚00'00'' to 36˚30'00'' north latitude (Figure 1).
According to the topographic map (Figure 2) the North West and East have the highest height, and the highest point is Chaluiy Mountain with an altitude of 3750 meters above sea level. The lowest section is located in the southwestern region and with height of 1080 meters.
Figure 1. Location map of the study area, based on Srtm image and the location of alluvial fans.
Figure 2. Topographic map of the area based on Srtm images   .
The most important research taking place in the region is research  , with the study of earthquakes in the twentieth century, he managed to divided Alborz into several seismic states and concluded that seismic activity in Alborz can be shown short time activities.  concluded that Meyamey faulthad, until the last stages of folding in the Pliocene Alpine has a right state.  concluded that the highest movement is potential in the area, mainly fault zones in north of Semnan and Sorkhe.  concluded that the fault is along the East-Northeast Meyamey steep slope to the south, and has a reverse mechanism with right turn slip component.  concluded that the maximum possible magnitude of earthquakes on Mullah, Tazareh and Damghan, faults tens are respectively, 6/9, 7/3 and 7/4.  examined the Quaternary activity of the region, and they managed to prove quaternary activity of boundary fault zone with sinisterly component.  concluded that, through independent factors, the variables area, En-Closed Area, during the basin, total length of waterways, the main stream watersheds and drainage density catchment have the greatest impact on the development of alluvial fans. This study will fallow measuring 16 indicators morphotectonic on 79 alluvial fans and 46 catchments by using16 indexes of morphotectonic methods (Table 1).
2. Geological Framework
The geological characteristics of this study belongs to two states in eastern Alborz and central Iran, Thus, the northern region belongs to structure of Alborz
Table 1. Morphotectonic indicators used in the area.
and central and southern regions belongs to structure of central Iran state. Trending of mountains in this area are ‘east-west mountain ranges’ that are relatively Wriggler mainly located in the north of Iran and south of Lake Caspian and their performances show orogenic events. These mountains they self are some part of Alpine-Himalaya orogeny in the north side in west Asia, this area we are talking about is limited to Caspian blocks from north and Central Iranian Plateau from sought. These mountains in their sought sides, not only have the geological structure similar to central Iran, but they have the same stratigraphy with the whole sought. Whereas the north side of Alborz have very different looks, in stratigraphy and geological structure with sought side of it  and  .
According to (Figure 3), the oldest unit of the Pre-Cambrian and Paleozoic units is in the vicinity of the fault Tazareh and, in the western part of the region. Paleozoic units, in the western part of the region, mainly in the North East- South West apartments available for modest expansion in southern and south― can be seen at eastern region. Mesozoic units in the north and northwest and the eastern parts are visible. Paleogene units in the North West and fault between Meyamey, Armiyan and Qods are located in the eastern part of the region. Neogene units, parts of the Northwest and East region have been widely, meanwhile, units of the Quaternary have formed a large part of the area.
3. Regional Structure
As shown in Figure 4, the region is composed of eight faults. However, because of the relationship between alluvial fans and some of the faults formed, we are going to mention the most important regional fault.
Figure 3. Simplified geological map of the study area, based on the geological map at a scale of 1: 100,000-Shahrud and Bastam.
Shahrud Thrust Fault: Shahrud Thrust fault in its north side has an approximate length of 55 km and it is a left on fault. The above fault has a northwest-southeast trend and it is dip to the north-north east. During the Shahrud fault zone we have measured 24 alluvial fans and 15 Catchment (Figure 4).
Tazareh Thrust Fault: Tazareh Thrust fault is located in the west side, has an approximate length of 30 km, it has a northwest-southeast trend and it is dip to the north east. Kinematic measurements show thrust left on fault movement along this fault implies. During the Tazareh fault zone we have measured 27 alluvial fans and 9 Catchment (Figure 4).
Armiyan fault and Qods fault: Armiyan faults, with an approximate length of 52 km and Qods fault with 53 km length, located in the eastern part of the region, the approximate trends northeast-southwest and has strike-slip components, However, the mechanism of these faults has not been exactly determined. These faults in the surface, measured tilt 65 degrees to 75 degrees to north and northeast. In general, Armiyan and Qods fault zone have 28 alluvial fans and 25 Catchment (Figure 4).
Anticline and syncline buildings, forming a major part of regional folding, some of the most important folds of the region are noted as follows:
Deh Molla syncline: It is an asymmetric steeped in the western part of the region, this syncline has a NE-SW direction parallel thrusts Shahrud and Tazareh, and it is aligned with the western part of the watershed. North limb of this syncline has been cut by large drift of Shahrud fault (Figure 4).
Syncline among the Shoqal Mountain and Bineh Mountain: syncline among the Shoqal Mountain and Bine Mountain is located almost in the
Figure 4. Distribution map of the region based on the geological maps with a scale of 1:100,000 Shahrud-Bastam.
center of the study area towards the East. The hiding central effect of this syncline is toward the north East-southwest, and aligned with the direction of alluvial fans and watershed in the east side (Figure 4).
Tal anticline: this asymmetric anticline is taken place in the western part of the study area, with parallel drift along the NE-SW West and Drift of Meyamey fault. The southern edge of the Tal anticline has been cut by Meyamey faults. Zigzag folding is also well visible in the subsequence (Figure 4).
Sanjavan anticline: This anticline is located in the easternmost part of the study area and they made a anticlinal structure in the southern side of Qods village. And effect of its axial is to north, north-east-south and south West. In addition, this anticline is aligned Fans and watershed that have arisen in the eastern part of the study area (Figure 4).
Kamar Syah anticline: Kamar Syah anticline located almost in the middle of the study area and effect of its axial is to east-west (Figure 4).
Reviews carried out of the 16 indicators morphotectonic on 79 alluvial fans and 46 watersheds in the study area and the information obtained from the calculations of reviews, can be followed in Table 2 and Figure 4.
Using the values calculated from the slope of the alluvial fans, alluvial fans radius, En-Closed area of alluvial fans and watershed area measured in the study area, graphs were plotted in three general methods.
1) There is an inverse relationship between the slope of the alluvial fan and the Watershed En-Closed area of the region (Chart 1).
2) Whatever the length radius of alluvial fans in the area increased, its slope reduced (Chart 2).
3) There is a direct relationship between, En-Closed area of alluvial fan and, En-Closed area of the Watershed (Chart 3).
According to the position of alluvial fans and watershed plotted in the range of faults (Figure 4), the area is divided into three major zones: Tazareh fault zone in the western part of the region, and Shahrud fault zone in the western part of the region, and Armiyan and Qods fault zone in the eastern part of region (Figure 5). To this end, maximum, minimum and average 11 indicators related to regional tectonic morphotectonic like( process Fans of fractionated, As, Smf, Vf, FCI, Fmf, Fd, Af, T, SL, Bs) , are placed in Table 3. In addition, the red color represents high tectonic activity, yellow represents moderate tectonic activity and green represents weak tectonic activity.
Thus, according to measurements taken of each index, summarizing the index is (Table 3):
1) Four indicators (process fractionated alluvial fans, Fmf, T, Bs) show that Armiyan-Qods fault zone with high construction activities, Tazareh fault zone with moderate tectonic activities and Shahrud fault zone with low tectonic activities in the region.
Table 2. Morphotectonic data from indices used in the area.
Chart 1. The relationship between the slope of the alluvial fan and, en-closed area watershed in the region.
Chart 2. The relationship between the slope and radius alluvial fans in the region.
Chart 3. The relationship between en-closed area of alluvial fan and, en-closed area of the watershed of the region.
Figure 5. Map index measured based on the overall outcome of the fault zone in the region.
2) Two indicators (FCI, Smf) show that Tazareh fault zone with high tectonic activities, Armiyan-Qods fault zones with moderate Construction activities and Shahrud fault zone with less tectonic activities in the region.
3) two indicators (Af, SL), show that Tazareh fault zone has high tectonic activities, Shahrud fault zone moderate earth construction of tectonic activities, and Armiyan-Qods fault zones have low activities in the region.
4) Indicator (As), it shows the Shahrud fault zone with the high construction activities, Armiyan-Qods fault zones with normal tectonic activities and Tazareh fault zone with low tectonic activities in the region.
5) Index (Vf), showst Armiyan-Qods fault zone with high tectonic activities, Shahrud fault zone with moderate Tectonic activities and Tazareh fault zone with low Tectonic activities, in region.
Table 3. Zoning and draw conclusions from data to calculate indicators used in the area morphotectonic.
6) Index (Fd), shows Armiyan-Qods fault zone with high tectonic activity, Tazareh fault zone with low tectonic activity in region.
According to Figure 6, compression, and earthquakes, in the north-west (Tazareh and Shahrud faults) increases. But in Armiyan-Qods fault zone in eastern district, despite high morphometry activity (Figure 5), Low density and seismic activity in the region. But in this area, there are a number of minor structures. The greatest depth recorded Earthquake occurred was 32 km to the ground and in the eastern part of the region. There focal mechanisms registered in the eastern part of the region in relation to earthquakes of magnitude 4.5(Arrow in Figure 6), reverse faults trending north-east Meyamey and South West in the region proves and movement in the compression zone.
5.1. Pluralization Geomorphic Indicators
Given the importance of Tazareh fault zone, Armiyan-Qods fault zones, Shahrud faults zone in associated with alluvial fans and Catchment area, tectonic activity was measured using 11 indicators according to the conclusions of the index Mentioned fault zone in the region that are divided as follows (Table 3 and Figure 5):
1―Armiyan-Qods fault zones, with 6 indicators (process fractionated alluvial fans, Fmf, Fd, Vf, T, Bs) and frequency of 54/54 Percent, high tectonic activity, with 3 index (As, Smf, FCI) and frequency of 27/27% with an average yield of tectonic and 2 Index (Af, SL) and the frequency of 18/18% with low-yield earth, represents the most active tectonic fault zone in the study area (Table 3).
2―Tazareh fault zone, with 4 index (Smf, FCI, Af, SL) with a frequency of 36/36%, the high tectonic activity, with 4 indicators (alluvial Fans of fractionated
Figure 6. Seismotectonic map of the study area, adapted from Tehran University Geophysics Institute  .
process, Bs, Fmf, T) with a frequency of 36/36%, with 3 tectonic activity indexes (Vf, As, Fd) with a frequency of 27/27% with low tectonic activity, shows this fault zone with moderate activity in the studied area (Table 3).
3―Shahrud Fault zone, with one indicator (As) with the frequency of 9/09%, and high tectonic activity, with 3 indexes (Vf, Af, SL) with The frequency of 27/27 percent, and with average tectonic activity and 6 indexes (process fractionated alluvial fans, Fmf, Smf, T, FCI , Bs) with a frequency of 54/54% and low tectonic activity. This table shows that this fault zone compared with Armiyan- Qods zone faults and Tazareh fault zone is significantly different and indicates low tectonic activity (Table 3).
5.2. Check Subsidence or Rising in the Region
Subsidence and rising in the region can be examined via index As. The data extracted from the index show that rising alluvial fans in the 83/54 percent, has specific effect on subsidence of the alluvial fan to 10/12% and high subsidence tectonic to 6/32 percent in the affected area. So, these high percents show high isostatic and tectonic impact in the region.