Kahramanmaraş Havzası'nın jeomorfolojisi
Geomorphology of Kahramanmaraş Basin
- Tez No: 97033
- Danışmanlar: PROF. DR. ALİ SELÇUK BİRİCİK
- Tez Türü: Yüksek Lisans
- Konular: Coğrafya, Geography
- Anahtar Kelimeler: Belirtilmemiş.
- Yıl: 2000
- Dil: Türkçe
- Üniversite: Marmara Üniversitesi
- Enstitü: Sosyal Bilimler Enstitüsü
- Ana Bilim Dalı: Coğrafya Eğitimi Ana Bilim Dalı
- Bilim Dalı: Belirtilmemiş.
- Sayfa Sayısı: 252
Özet
Özet yok.
Özet (Çeviri)
ABSTRACT Kahramanmaraş basin was of appearance of transition in view of geographic position and geomorphological properties. It was located just in the southern part of intersection point of the Anatolia and Arabia salbs. For this reason, it reflects the intersection effects of these two salbs. In the basin, in the erea starting from Precambrian to Quaternary, a diversity developed in different facies and a stowage showing a disorder existed. This layer formed a quite complex structure being twisted and cracked because of the effect of serious tectonism continuing from, especially, Miocene to mouadap. In the basin, the oldest orogeneze traces were seen in the core units of the North Amanos Mountains. Caledonian and Hersinien orogenze affected these units. Alp Orogenze became effective in the whole basin in the from term. At the result of intersection of Arabia and Anatolia slaben in the bellow and middle maestrich, compressional stress directed to the north and south became effective in the basin. Because of this stress, allocation units located in upper Kretase by loading to basin from north. The basin gainet its main structural properties by this loading. This loading ocarried at the early Alpin term, caused to imprecate, crake, twist and imprecate on the Pre Alpin formation of the North Amanos Mountains. The North - South directed compresional stress extending from upper Kretase to upper Miocene faced the imprecate, loading and faults in the basin. In the upper Miocene, this stress caused to from death sea and the Eastern Anatolia faults having side base. The roof of graben forming the present basin came out by the effective of side faults and the other occurring at the same time. By the effective of Neotektonism contouring from upper Miocene to Quaternary also, the basin had gained current geomorphologic properties. Thus, two big geomorphologic units, the basin of basin and its around, developed. Among these, at the base of basin, Narh, Türkoğlu, Maraş plaes; secondary horst featured plateau distinguishing these pleas from each other and lower swell areas exist. The around of the basin, consists of the North Amanos, Başkonuş - Kubah, Ahır, Kartalkaya, mountains and hilly areas and plateus in the various altitude steps. 206In the developing of present relief in Kahramanmaraş basin, as well as tectonic events, the common effects of climatic, hydrographic, vegetative and pedeologial factors also exist. The current properties of Kahramanmaraş basin formed the problems for human activities in some areas. These problems showed differencies at the base of basin and the somewhat higher areas in its around. While floods, slugs and drawn out formed the most important problems in the plains at the base of basin, the main problems of high areas were erosion and soil motion. The earthquakes are common problems of all the basin. Active systems such as death sea and Eastern Anatolia faults increased the risk of earthquake. Residence's in the basin were generally centralised on alluviums around resources ranging through these fault lines. Since houses in here were far away from standard structure required for an active fault region, even dameges to be arised from an earthquake with middle degree might reach very important dimensions. 2Q7
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