Английская Википедия:Bayanhaote Basin

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Шаблон:Short description Шаблон:Infobox valley

The Bayanhaote Basin[1] (Шаблон:Zh), also known as Bayanhot Basin,[2] is a geographic region located in the west-central part of Inner Mongolia Autonomous Region.[3] It is a superimposed basin that underwent a long-term sedimentary evolution process from transgression to retrogression during the Carboniferous to Late Permian.[4]

The Bayanhot Basin is a composite and superimposed basin developed in the crossing zone of the Qinlin-Qilian-Helan trifurcate rift system (秦、祁、贺三叉裂谷系) during the beginning of Early Palaeozoic Era (早古生代早期) of crossover zone.[5]

It has been a self-flowing tectonic basin since the Mesozoic. [6] In the early 1950s, oil and gas exploration in this area began.[7]

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Шаблон:China-geo-stub