ISOSTASY Removal of material from the top will induce uplift at the surface. Removal of material from the bottom will produce subsidence. Thus, in the case of tectonic extension, isostasy will produce an effect that is opposite to thermal uplift.
DIVERGENT SETTING- RIFT Crustal thinning produces depocenters Half-graben geometry results in asymmetric patterns of deposition Sediments are typically immature, intercalated with volcanic rocks Distribution of sediment types over time records tectonic activity Older sedimentary layers have higher dips than younger layers
Continental margin sedimentation Siliciclastic systems Regionally extensive, tabular units Moderately mature sands - quartz dominant - grade to fine-grained pelagic seds Generally well developed bedding Carbonate systems Confined to low latitude, warm clear seas with little terriginous input Patterns affected by organisms, such as those that form reefs, not just sedimentation processes
CONVERGENT SETTINGS Elongate trends of thick sedimentary sequences associated with subduction zones Trench: Trench basins can be very deep, and the sedimentary fill depends primarily on whether they are intra-oceanic or proximal to a continent. Accretionary prism includes material carried to trench on downgoing slab; wedge-shaped, faulted and folded Trench-slope: (intra-slope basins) Hemipelagic sediments, turbidites, slumps Forearc Basin: Basin shoals upward, turbidites to delta and non-marine, shows unroofing sequence (input from progressively deeper rocks) Input of both immature sediments shed from eroding arc and volcanic materials increases with proximity to continent
QuickTime™ and a TIFF (Uncompressed) decompressor are needed to see this picture. An exhumed example from SW Japan Basic structural and sedimentological elements of an accretionary prism QuickTime™ and a TIFF (Uncompressed) decompressor are needed to see this picture.
CONVERGENT SETTINGS Foreland Basin: elongate regions of potential sediment accumulation that form on continental crust between contractional orogenic (fold and thrust) belt and craton (produced by thrust loading) Arch or bulge separates foreland from cratonic basin QuickTime™ and a TIFF (Uncompressed) decompressor are needed to see this picture.
CONVERGENT SETTINGS Thrust belt typically propagates into foreland basin, moving depocenter in the direction of thrust motion Piggyback Basin: basins that are on the hanging wall of a thrust fault and move with the hanging wall. Sediments evolve from fine-grained turbidites to shallow water continental seds over time QuickTime™ and a TIFF (Uncompressed) decompressor are needed to see this picture.