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- W2185434523 abstract "The Grande Cache area in west-central Alberta contains numerous folds that change geometry or orientation along trend. This change tends to be associated with the presence of channels or a lateral transition to sandstone-dominated strata. An example of this changing geometry is seen in a secondary fold on the MacEvoy anticline that changes from a cylindrical to a box fold over a distance of 300 m. This change is accompanied by secondary structures and variations in the fracture patterns." @default.
- W2185434523 created "2016-06-24" @default.
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- W2185434523 date "2010-01-01" @default.
- W2185434523 modified "2023-09-27" @default.
- W2185434523 title "Effects of Channels on Fold Geometry and Fracture Patterns in the Grande Cache Area, West-Central Alberta" @default.
- W2185434523 hasPublicationYear "2010" @default.
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