Spatial and temporal controls on the development of heterolithic, Lower Jurassic tidal deposits (Upper Are and Tilje Formations), Haltenbanken area, Offshore Norway.
The stratigraphic organization of clastic successions deposited during the early synrift phase is controlled by the rates of tectonic subsidence and the growth of the master faults, which, coupled with eustatic sea-level changes, control the generation of accommodation. The highly heterolithic, Lowe...
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| Language: | en en |
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2012
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| Online Access: | http://hdl.handle.net/1974/7196 |