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The Arabian plate is a minor tectonic plate in the Northern and Eastern Hemispheres.. It is one of the three continental plates (along with the African and Indian plates) that have been moving northward in geological history and colliding with the Eurasian plate.
The Eurasian plate is a tectonic plate that includes most of Eurasia (a landmass consisting of the traditional continents of Asia and Europe), with the notable exceptions of the Arabian Peninsula, the Indian subcontinent, and the area east of the Chersky Range in eastern Siberia.
For purposes of this list, a minor plate is any plate with an area less than 20 million km 2 (7.7 million sq mi) but greater than 1 million km 2 (0.39 million sq mi). Amurian microplate – A minor tectonic plate in eastern Asia; Arabian plate – Minor tectonic plate – 5,000,000 km 2 (1,900,000 sq mi)
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.
Obduction zones occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates favours subduction of the oceanic plate. This causes the oceanic plate to buckle and usually results in a new mid-ocean ridge forming and turning the obduction into subduction. [citation needed]
The belt is the result of Mesozoic-to-Cenozoic-to-recent closure of the Tethys Ocean and process of collision between the northward-moving African, Arabian, and Indian plates with the Eurasian plate. [1] Each collision results in a convergent boundary, a topic covered in plate tectonics.
The Iranian plateau [1] or Persian plateau [2] [3] is a geological feature spanning parts of the Caucasus, Central Asia, South Asia, and West Asia.It makes up part of the Eurasian plate, and is wedged between the Arabian plate and the Indian plate.
The Alpine orogeny is caused by the continents Africa, Arabia and India and the small Cimmerian Plate colliding (from the south) with Eurasia in the north. Convergent movements between the tectonic plates (the African Plate, the Arabian Plate and the Indian Plate from the south, the Eurasian Plate and the Anatolian Sub-Plate from the north, and many smaller plates and microplates) had already ...