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Arabian Peninsula, Gulf of Aden, Indian Ocean, Persian Gulf, Red Sea 1 Relative to the African plate The Arabian plate is a minor tectonic plate in the Northern and Eastern Hemispheres .
The Makran Trench is the physiographic expression of a subduction zone along the northeastern margin of the Gulf of Oman adjacent to the southwestern coast of Balochistan of Pakistan and the southeastern coast of Iran. In this region the oceanic crust of the Arabian plate is being subducted beneath the continental crust of the Eurasian plate.
The Persian Gulf Basin (Persian: آبخیز شاخاب پارس, Arabic: حوض الخليج الفارسی) is found between the Eurasian and the Arabian Plate.The Persian Gulf is described as a shallow marginal sea of the Indian Ocean that is located between the south western side of Zagros Mountains and the Arabian Peninsula and south and southeastern side of Oman and the United Arab Emirates.
Red Sea Rift between the African (Nubian) Plate and the Arabian plate The Red Sea Rift is a mid-ocean ridge between two tectonic plates , the African plate and the Arabian plate . It extends from the Dead Sea Transform fault system, and ends at an intersection with the Aden Ridge and the East African Rift , forming the Afar triple junction in ...
Aden-Sheba Ridge. The Aden Ridge is a part of an active oblique rift system located in the Gulf of Aden, between Somalia and the Arabian Peninsula to the north. The rift system marks the divergent boundary between the Somali and Arabian tectonic plates, extending from the Owen transform fault in the Arabian Sea to the Afar triple junction or Afar Plume beneath the Gulf of Tadjoura in Djibouti.
The Afar triple junction (also called the Afro-Arabian rift system) is located along a divergent plate boundary dividing the Nubian, Somali, and Arabian plates. This area is considered a present-day example of continental rifting leading to seafloor spreading and producing an oceanic basin .
Map of the Dead Sea Transform showing the main fault segments and motion of the Arabian plate relative to the African plate, [1] from GPS data The Dead Sea Transform (DST) fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run for about 1,000 km from the Marash triple junction (a junction with the East Anatolian Fault in southeastern Turkey) to the ...
The Maraş triple junction at the junction of the East Anatolian Fault and Dead Sea Transform. The Maraş triple junction is a geologic triple junction of three tectonic plates: the Anatolian plate, the African plate and the Arabian plate.