Diverse basin-floor settings under marine and fresh water result in a wide variety of sizes and shapes of deep-sea-fan deposits (Table 4-1). Throughout all discussions about deep-sea fans it is important to keep this in mind, that the scale of fan size and associated morphologic features varies greatly for different fans ranging in size from a few kilometers in radius to over 2,500 km in radius.
In terms of area covered, the most common modern setting for deep-sea fans is on the continental rise at the base of the continental margin in the open ocean basin (Figs. 4-1 and 4-2; Plate 1). The continental rise during the present high eustatic sea level is separated from the coastal sediment sources by a broad, flat shelf and the continental slope (Figs. 4-2 and 4-3). During low sea levels only the relatively steep and narrow continental slope separates the rise from coastal sediment sources. The continental rise gradients are much less than those on the continental slope and the rise typically extends for the greatest distance of any margin environment. The continental-rise setting of deep-sea fans is different from the shelf and slope areas because it overlies transitional or oceanic crust rather than continental crust.
Deep-sea fans occur in greatest numbers in marginal- and continental-borderland-basin settings, but these are much smaller in size than fans on the open-ocean floor (Plate 1). The main constraint to fan size is the generally confined or restricted basin size found in these marginal-sea and continental-borderland settings
Figures & Tables
Modern and Ancient Deep-Sea Fan Sedimentation
This course of modern and ancient deep-sea fan sedimentation provides the framework for understanding the morphology, physiography, geometry, depositional processes and reservoir potential of deep-sea fan deposits. Focus is chiefly on the principles that control fan sedimentation and the resultant morphology of fans deposited in various types of settings. Through the comparison of modern and ancient examples of deep-sea fan sedimentation, the authors hope to increase understanding of the principal characteristics of fans. The course is divided into four parts (1) the Introduction, which covers the organization of the course and history of fan studies, (2) modern deep-sea fan deposits, (3) ancient deep-sea fan deposits, and (4) the synthesis, in which the results of the separate modern and ancient examinations of deep-sea fan deposits are synthesized into models that may be applicable to petroleum exploration.