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  • At present, deformation around the margins of the basin is resulting in the microcontinental crust being underthrust beneath the Tian Shan to the north, and the Kunlun Shan to the south. A thick succession of Paleozoic, Mesozoic and Cenozoic. — “Tarim Basin - Wikipedia, the free encyclopedia”,
  • Honshu itself is formed from the island arc developed over the subducting plate.[1] The an unusually thick section of fluid-rich sedimentary rocks to be deeply underthrust. — “Nankai megathrust earthquakes - Wikipedia, the free encyclopedia”,
  • The width and depth of the foreland basin is determined by the flexural rigidity of the on the plate that is subducted or underthrust during plate collision (i.e. the outer arc. — “Foreland basin - Wikipedia, the free encyclopedia”,


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