About: Bayanhaote Basin

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The Bayanhaote Basin (simplified Chinese: 巴彦浩特盆地; traditional Chinese: 巴彥浩特盆地; pinyin: Bāyànhàotè Péndì), also known as Bayanhot Basin, is a geographic region located in the west-central part of Inner Mongolia Autonomous Region. It is a superimposed basin that underwent a long-term sedimentary evolution process from transgression to retrogression during the Carboniferous to Late Permian. It has been a self-flowing tectonic basin since the Mesozoic. In the early 1950s, oil and gas exploration in this area began.

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  • The Bayanhaote Basin (simplified Chinese: 巴彦浩特盆地; traditional Chinese: 巴彥浩特盆地; pinyin: Bāyànhàotè Péndì), also known as Bayanhot Basin, is a geographic region located in the west-central part of Inner Mongolia Autonomous Region. It is a superimposed basin that underwent a long-term sedimentary evolution process from transgression to retrogression during the Carboniferous to Late Permian. 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. It has been a self-flowing tectonic basin since the Mesozoic. In the early 1950s, oil and gas exploration in this area began. (en)
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  • Bayanhaote Basin (en)
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  • s (en)
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  • Bāyànhàotè Péndì (en)
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  • 巴彦浩特盆地 (en)
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  • 巴彥浩特盆地 (en)
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  • The Bayanhaote Basin (simplified Chinese: 巴彦浩特盆地; traditional Chinese: 巴彥浩特盆地; pinyin: Bāyànhàotè Péndì), also known as Bayanhot Basin, is a geographic region located in the west-central part of Inner Mongolia Autonomous Region. It is a superimposed basin that underwent a long-term sedimentary evolution process from transgression to retrogression during the Carboniferous to Late Permian. It has been a self-flowing tectonic basin since the Mesozoic. In the early 1950s, oil and gas exploration in this area began. (en)
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  • Bayanhaote Basin (en)
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