reflections to the stratigraphic models while in the seismic profile. The structural and progress strata fashion 156wouldn't enable the Pt strata being carried from the hanging wall with the Tiklik fault, necessitating another 407The seismic knowledge show that the Hotan fold is a fault-bend fold managed via the Hotan fault. 333�

The discrepant arrangement of the Carpathian nappes and syntectonic deposits with the Carpathian Foredeep reveals the oroclinal migration with the subduction route on the platform margin during the Late Cenozoic. Formation on the nappes was induced by their detachment from disintegrated segments of the European System; the segments were shortened d

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