By G. Shanmugam
ISBN-10: 0444563350
ISBN-13: 9780444563354
This instruction manual is key for knowing the foundation of deep-water sandstones, emphasizing sandy-mass delivery deposits (SMTDs) and bottom-current remodeled sands (BCRSs) in petroleum reservoirs. This state of the art point of view, a practical replacement to the normal turbidite techniques, is important as the turbidite paradigm is outfitted on a doubtful beginning with no empirical facts on sandy turbidity currents in glossy oceans. within the absence of facts for sandy turbidity currents in traditional environments, stylish theoretical types and experimental observations of turbidity currents are inappropriate substitutes for explaining the starting place of sandy deposits as ''turbidites.'' In documenting glossy and historical SMTDs (sandy slides, sandy slumps, and sandy debrites) and BCRSs (deposits of thermohaline [contour] currents, wind-driven currents, and tidal currents), the writer describes and translates middle and outcrop (1:20 to 1:50 scale) from 35 case reviews all over the world (which contain 32 petroleum reservoirs), totaling greater than 10,000 m in cumulative thickness, performed prior to now 36 years (1974-2010). The publication dispels myths in regards to the significance of sea point lowstand and offers much-needed readability at the triggering of sediment disasters by means of earthquakes, meteorite affects, tsunamis, and cyclones with implications for the distribution of deep-water sandstone petroleum reservoirs.
- Promotes pragmatic interpretation of deep-water sands utilizing substitute possibilities
- Validates the industrial significance of SMTDs and BCRS in deep-water exploration and production
- Rich in empirical info and well timed new views
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Extra info for New Perspectives on Deep-water Sandstones: Origin, Recognition, Initiation and Reservoir Quality
Example text
Sandy debris flow Lower Cambrian, Bunkers Outcrop Sandstone, Donkey Bore Syncline, Officer Basin, Australia Reilly and Lang (2003); Payenberg et al. (2005) 65. Sandy debris flow and “high-density turbidity current” (massive sand)b Seventy examples, Precambrian to recent, worldwide Outcrop and core Stow and Johansson (2000, their Table 1) 66. Sandy debris flow and submarine “landslide” Neoproterozoic/Lower Cambrian, Phe Formation, Northeast Himalaya Outcrop Draganits et al. ” Some of these papers were published before the introduction of the concept of sandy debris flow by Hampton (1972).
2009) 27. Sandy debris flow and sandy slump Pliocene, Edop Field, offshore Nigeria Conventional core Shanmugam (1997b) 28. 43) Pliocene, Zafiro Field, Equatorial Guinea Conventional core Shanmugam (2006a) 29. Sandy slump and sandy debris flow Pliocene and Pleistocene, Conventional Gulf of Mexico core Shanmugam and Zimbrick (1996) 30. Sandy debris flow Upper Miocene, Navidad Outcrop (massive sandstone Formation South-central with floating clasts Chile (up to 1 m in diameter), armored mudstone balls, and granules) Encinas et al.
In evaluating high-velocity (3 m s21) turbidity currents inferred by Dengler et al. (1984), Middleton (1993, p. 100) commented that “. . ” Khripounoff et al. 4 cm s21. But they did not provide the critical data on vertical sediment concentration profiles with grain-size variations. Again, velocity is not the defining criterion of turbidity currents. Parsons et al. (2003, p. ” But the authors did not provide any information on sediment concentration in establishing turbidity currents. Nor did they provide information on the Reynolds number of the resuspension.
New Perspectives on Deep-water Sandstones: Origin, Recognition, Initiation and Reservoir Quality by G. Shanmugam
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