Özet:

The work area covers the Raman and Gercush anti-clinals within the boundary curves system located in the front of the Southeast Toros (sout). All the continuous and seasonal flows on the field are thrown into the Dicle River, which runs in the synchronous occurrence between the Raman and the Gercush anti-clinals. The current structural characteristics and tectonic formation of the Raman and Gercüş curvation systems occurred with Alpine orogenesis. Jura-type curves are in the work area that occur depending on the fasting movements in the northward direction. These curved structures were formed in recent times (Alt-Miyosen) and spread in the direction of D-B. In the synchronous basin between the Raman and Gercüş anticlinals in Pliyosen, the Dicle River is placed as "consistent to the size". After the establishment of the Dicle River, side arms linked to the river by a straight angle from the anti-clinical stairs have been placed. These side arms continued the activity of discharge, while the benefits that occurred facilitated, accelerated these activities. Fluvial processes linked to the Dicle River and their arms on the Raman and Gercüş anti-clinals have produced original examples of different drainage properties. These are consistent in height, subsequent depression, clusters and rivers, anti-clinal valley, cafes drainage and catching events. Although the work area was not very wide, the capture occurred in three separate points. These capture events occurred as a result of the activity of reversing the Dicle River and its side arms. Keywords: Raman and Gercüş anticlinali, Dicle river, drainage characteristics, covering events. ABSTRACT The research area comprises Raman and Reality anticlinals, including edge folding system which is in front of the South Estern Taurus (southern side) All continuous and seasonal streams in the zone flow into the Dicle river which flow synclinal channel among Raman and Reality anticlinals The present structural properties of Raman and Reality folding systems and tectonic formation has been executed with Alpines orogenesis. The occuring foldings are Jura type foldings which happens in North and South directions bound to jammed movements. These folding structures have been formed in nearby times (lowermiddle Miosen ), and it is in the way of N-S (North South). The Dicle river is situated in the Pliosen as "lengthwise consecuent" between Raman and Gercüş anticlinals in the sinclinal basin. After the establishment of the Dicle River, side tributaries have been added to the slopes of the anticlinals in the position of the right angle. As the side tributaries goes on corrosion activities, the occured faults have facilitated and accelerated these activities. The fluvial periods dependent on the Dicle River and its tributaries on the Raman and the Raman anticlinals, have occured original samples at different drainage properties. These are the lengthywise consecutive, subsecant depressions, cluses and ruzes, anlticlinal valley, latticed drainage, and capture events. Even though the work area is very vast the capture event has been executed in three different points. These captures, have been executed after the side tributaries of the Dicle River's back corrosion activities. Keys words: Raman and Anticlinal, Dicle River, Drainage Properties, Capture Events