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Deep-water marine reservoirs (view source)
Revision as of 19:49, 17 August 2015
, 19:49, 17 August 2015→Production from channelized systems
==Production from channelized systems==
==Production from channelized systems==
The channel axes may act as pathways for the preferential ingress of water. This can result in the stranding of banked oil along the channel margin pinch-out edges ([[:File:M91FG194.JPG|Figure 2a]]) (Clark et al., 1997).
The channel axes may act as pathways for the preferential ingress of water. This can result in the stranding of banked oil along the channel margin pinch-out edges ([[:File:M91FG194.JPG|Figure 2a]]).<ref>Clark, M. S., J. D. Melvin, R. K. Prather, and A. W. Marino, 1997, Characterization and exploitation of the distal margin of a layered, low-permeability turbidite reservoir, Yowlumne field, San Joaquin Basin, California: Houston Geological Society Bulletin, v. 40, no. 4, p. 12–15.</ref>
[[File:M91FG194.JPG|thumb|300px|{{Figure number|2}}Features influencing fluid flow in deep-marine sandstones.]]
[[File:M91FG194.JPG|thumb|300px|{{Figure number|2}}Features influencing fluid flow in deep-marine sandstones.]]