تعیین زمین ساخت فعال با استفاده از مورفولوژی مسیر رودخانه ها با نگرشی ویژه بر راندگی زردکوه و تاقدیس پز (جنوب شرقی استان لرستان)

Alluvial channels are phenomenon that are very sensitive to the changes of river flow and specifications of sedimentary load and many 

changes that occur in channel morphology during time can be related to that mensioned changes. The deformations of rivers channel 

can be observed in various ways but usually the first effect will berevealed locally in decrease or increase of channel bed ramp and/or 

deflection or cutting of channel, bed boring or deposition. In many cases, resolution of the effects as a result of active tectonic 

movements from the effects as a resul of river flow changes and  specifications of sesimentary load on the channel morphology on this 

fact that we should not judge about district activation by using varioes evidences and also their corresp on dence state in relation to 

each other. In general, in regions  hat the earth crust was unstable for long periods of time, active response. In this paper, we dealed 

with examination of active tectonic of zardkooh thrust and pez anticline and morphology located on southeastern of lorestan province 

and was Compared with simillar studies in other regions of Iran (fig. ۱)

کلید واژه ها: زمینساخت مورفولوژی زردکوه لرستان رودخانهآبذالکی تکتونیک سایر موارد