Himalayan Foreland: Folded Ridges and Rapid Uplift Zones
喜马拉雅前陆：褶皱山岭与快速隆升带
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South of the main Himalayan range lies a narrow but tectonically intense foreland zone of folded sedimentary rocks.
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Crustal shortening here exceeds 20 mm per year, making it one of Earth’s most rapidly deforming regions.
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