Bachu Rise is the fore-bulge of the Kunlun late Cz foreland basin system.
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Ca. 65, 23, 5, 3–2 and <1.5 Ma faulting phases identified out in W Tarim.
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Ca. 65 Ma faulting phase formed under the far-field effect of the Lhasa-Asia collision.
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The other faulting phases formed under the far-field effect of the India-Asia collision.
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The late Cz faulting in the W Tarim Basin is characterized with pulse thrust.
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