About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The Spring Coulee well is located 40 miles south and west of Lethbridge, Alberta. The glacial drift here is underlain by the St. Mary River formation, Subsurface formations penetrated by the well are the marine Foxhills sandstone, the marine Bearpaw shale, the Belly River group, the marine Colorado shale, the Blairmore formation, the marine Fernie shale, and the upper Paleozoic limestone. The stratigraphy of these formations is described and correlations are suggested.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
|Protected Document: $10|
|Internal PDF Document: $14|
|Open PDF Document: $24|
Members of AAPG receive access to the full AAPG Bulletin Archives as part of their membership. For more information, contact the AAPG Membership Department at [email protected].