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propagation of thrusting in this phase, suggesting the detachment layers played an essential 482
would not allow the Pt strata to get carried while in the hanging wall with the Tiklik fault, demanding One more 407
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into the south by the Tiklik fault and Paleozoic strata (D, C and P) crop out on the Main from the 427
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The India-Eurasian collision has created a wide zone of intracontinental deformation that extends 46
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unconformities, Whilst N1 sits above C within the north of Buya and N2 overlies earlier mentioned Pt to farther 437
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earthquake: seismic hazards of the Energetic blind wedge thrust program in the Western Kunlun range 600
Cenozoic tectonic rotations in several parts of the NE Pamir: implications for that evolution in the arcuate orogen
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