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The study presents minimum shortening estimates of 130-200 km across the western Greater Caucasus Mountains, suggesting a thin-skinned structural style of deformation rather than the previously assumed thick-skinned model. This research utilizes line-length and area balanced cross sections to analyze the geological structure and highlights the potential for additional shortening. The findings contribute to the understanding of the tectonic evolution of the region, which is influenced by the ongoing collisio

Author

demur.merkviladze0

Language

EN