|
Kansas Geological Survey Open-file Report 2001-38 |
Oolitic packstones and grainstones are the most prolific reservoir lithofacies for the Lansing-Kansas City in Kansas. Oolite shoal facies owe their wide distribution geographically within Kansas and stratigraphically within the Upper Pennsylvanian (especially in the L-KC) to bathymetry (nearly flat) and episodic sea level changes. The broad Kansas shallow shelf and oscillating sea level resulted in lateral migration of oolite shoal conducive environments.
|
e-mail : webadmin@kgs.ku.edu
Last updated December 2001
http://www.kgs.ku.edu/PRS/publication/OFR2001-38/P1-04.html