Tectonics and sedimentation

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Sedimentary facies and depositional environment in pheripheral basins Shallowing upward p ard trend up-section
Thin- versus thick- sckinned ddeformation f i • Typical (continuous) foreland basins develop in association with thin-skinned thrust belts: – i.e. where sedimentary cover rocks are shortened by folding and thrusting above undeformed basement.
Page 1 and 2: Tectonics and sedimentation
Page 3 and 4: Basins related to convergent margin
Page 5 and 6: Foreland The Himalayan orogeny The
Page 7 and 8: Example of ocean-continent collisio
Page 9 and 10: Isostasy • Based on Archimede pri
Page 11 and 12: Airy model
Page 13 and 14: Local vs. Flexural or Regional isos
Page 15 and 16: In practice • For a buoyant solid
Page 17 and 18: Implication for mountain ranges •
Page 20: Geohistory analysis
Page 25: Cratonic Catocbas basin Time Strike
Page 29 and 30: Preconditions to form a continuous
Page 31 and 32: Component of tectonic subsidence ii
Page 33 and 34: Example of broken foreland: the Roc
Page 35: Sediments in foreland basins • RR

Tectonics and sedimentation

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