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Tectonics of the Tian Shan : ウィキペディア英語版 | Tectonics of the Tian Shan
The Tian Shan is a mountain range in central Asia that extends through western China, Kazakhstan, and Kyrgyzstan.〔 The Tian Shan is long, and up to high. Throughout the Tian Shan there are several intermontane basins separated by high ranges.〔 Plate tectonic theory makes the assumption that deformation is concentrated along plate boundaries. However, active deformation is observed in the Tian Shan, far from plate boundaries. This contradiction of plate tectonic theory makes the Tian Shan a key place to study the dynamics of intracontinental deformation.〔 ==Tectonic history==
The intracontinental weakness of Asia's interior has caused deformation in the Tian Shan Range after the collision of India into Asia.〔 However, the Tian Shan was uplifted prior to the Cenozoic Indo-Asia collision.
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Tectonics of the Tian Shan」の詳細全文を読む
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