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Eurasian, Anatolian, and Arabian (purple coloring) plates. The Arabian plate consists mostly of the Arabian Peninsula; it extends westward to the Sinai Peninsula and the Red Sea and northward to the Levant. The plate borders are: East, with the Indo-Australian plate, at the Owen fracture zone; South, with the African plate to the west and the ...
Anatolian plate. The Anatolian sub-plate [1] [2] is a continental tectonic plate that is separated from the Eurasian plate and the Arabian plate by the North Anatolian Fault and the East Anatolian Fault respectively. Most of the country of Turkey is located on the Anatolian plate. [3]
The Karliova triple junction is a geological intersection point located in eastern Turkey, where the boundaries of the Arabian plate, the Eurasian plate, and the African plate meet. It is a complex structure with multiple faults and fractures, resulting from the collision and convergence of these tectonic plates.
Tectonic plates in Turkey; the Anatolian sub-plate, the African plate, the Arabian plate, and the Eurasian plate. Except for a relatively small portion of its territory along the Syrian border that is a continuation of the Arabian plate, Turkey geologically is part of the great Alpide belt that extends from the Atlantic Ocean to the Himalaya ...
The Maraş triple junction is found where the side-by-side African and Arabian plates, both drifting north and demarcated by the north–south trending Dead Sea Transform (itself an extension of the African Rift Valleys), come up against the Anatolian plate lying across their path at the East Anatolian Fault.
The East Anatolian Fault (EAF; Turkish: Doğu Anadolu Fay Hattı) is a ~700 km long major strike-slip fault zone running from eastern to south-central Turkey.It forms the transform type tectonic boundary between the Anatolian sub-plate and the northward-moving Arabian plate. [1]
The Anatolian plate is moving towards the Arabian plate due to horizontal sliding, he suggested. The quake, he said, generated a type of fault that seismologists call “shallow transcurrent ...
The Ga'ara Formation and the Chia Zairi Limestone Formation deposited in the Permian. Chia Zairi rocks are particularly thick—up to 800 meters—and include the 61 meter Satina Evaporite Member, interpreted as the beginning of splitting of the Arabian plate into the Anatolian plate and Iranian plate.
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