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土耳其西南部的橄榄岩可分为北部单元和南部单元。从达特查半岛向东延伸,每一单元的面积超过700平方公里。安迭士利克-捷坶巴拉利克(Andizlik-Zimparalk)位于北部单元东,端弗提耶之北40公里处。本区是一个铬矿经济资源地。橄榄岩体总的走向为NW-SF。岩体南北与沉积围岩以倾向橄榄岩的冲断层带相接触。沉积岩未变质,主要由古生代和中生代灰岩及中新世复理层所组成。
Peridotites in southwestern Turkey can be divided into northern and southern units. Extending eastward from the Dhitha Peninsula, each unit has an area of more than 700 square kilometers. Andizlik-Zimparalk is located 40 km north of Fethiye on the north east of the unit. This area is a chromium ore economic resources. The general trend of peridotite is NW-SF. The north and south of the rock body are in contact with the sedimentary rock in the thrust zone of the peridotite. Sedimentary rocks are not metamorphosed, mainly composed of Paleozoic and Mesozoic limestone and Miocene flysch.