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  2. Qinling - Wikipedia

    en.wikipedia.org/wiki/Qinling

    The Qinling (simplified Chinese ... To the west is the line of mountains along the northern edge of the Tibetan Plateau. To the east are the lower Funiu and Dabie ...

  3. Tibetan Plateau - Wikipedia

    en.wikipedia.org/wiki/Tibetan_Plateau

    The Tibetan Plateau, [a] also known as Qinghai–Tibet Plateau [b] and Qing–Zang Plateau, [c] is a vast elevated plateau located at the intersection of Central, South, and East Asia. [d] Geographically, it is located to the north of Himalayas and the Indian subcontinent, and to the south of Tarim Basin and Mongolian Plateau.

  4. Qinling orogenic belt - Wikipedia

    en.wikipedia.org/wiki/Qinling_Orogenic_Belt

    The Qinling orogenic belt is a tectonic feature that evolved throughout the Proterozoic and Phanerozoic eons due to a variety of tectonic activities. [3]

  5. Geography of China - Wikipedia

    en.wikipedia.org/wiki/Geography_of_China

    The Qinling and Dabashan ranges form a major north-south divide across China Proper, the traditional core area of China. Southeast of the Tibetan Plateau and south of the Sichuan Basin is the Yunnan-Guizhou Plateau, which occupies much of southwest China. This plateau, with an average elevation of 2,000 m, is known for its limestone karst ...

  6. Dabie-Sulu orogeny - Wikipedia

    en.wikipedia.org/wiki/Dabie-Sulu_orogeny

    The Dabie-Sulu orogeny also termed Qinling-Dabie-Sulu or Dabie Shan-Sulu was a mountain building event in the Triassic from 240 to 220 million years ago caused by the collision of the North China and South China cratons.

  7. Altyn Tagh fault - Wikipedia

    en.wikipedia.org/wiki/Altyn_Tagh_fault

    The Altyn Tagh Fault (ATF) is a 2,000 km long, [1] [2] active, sinistral (left lateral) strike-slip fault that forms the northwestern boundary of the Tibetan Plateau with the Tarim Basin. It is one of the major sinistral strike-slip structures that together help to accommodate the eastward motion of this zone of thickened crust , relative to ...

  8. Geology of China - Wikipedia

    en.wikipedia.org/wiki/Geology_of_China

    The Tibetan Plateau is unstable and as its sides move away extension is occurring in its center. This east–west extension is accommodated on north–south trending normal faults. [8] The Tian Shan are a mountain range north of the Tibetan Plateau and the Taklamakan Desert. Uplift of these mountains began 24 million years ago.

  9. Altun Shan National Nature Reserve - Wikipedia

    en.wikipedia.org/wiki/Altun_Shan_National_Nature...

    Altun Shan National Nature Reserve (simplified Chinese: 阿尔金山; traditional Chinese: 阿爾金山; pinyin: Ā'ěr jīnshān) (literally, "O You Golden Mountain") is a large, arid area in the southeast of Xinjiang Autonomous Region, on the northern edge of the Tibetan plateau and the southern edge of the Tarim Basin in northwest China.