Crustal shortening is the predominant style of Cenozoic deformation in the Tian Shan, which propagated outward and rose progressively as a wedge-shaped block.
The Tian Shan propagated outward and rose progressively as a wedged-shaped block. Crustal shortening is the predominant style of Cenozoic deformation in the Tian Shan.
Crustal shortening is the predominant style of Cenozoic deformation in the Tian Shan. The Tian Shan propagated outward and rose progressively as a wedged-shaped block.
Crustal shortening is the predominant style of Cenozoic deformation in the Tian Shan. The Tian Shan propagated outward and rose progressively as a wedged-shaped block.