About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The AAPG/Datapages Combined Publications Database
AAPG Bulletin
Abstract
Volume:
Issue:
First Page:
Last Page:
Title:
Author(s):
Abstract:
Dakota(?) formation, Graneros shale, Greenhorn limestone, and Carlile shale are locally mappable units of regional extent. Local subdivisions of the Niobrara formation, a lower dark shale and an upper sandy shale, can also be mapped. The Cano sandstone member of the Mesaverde formation is a tongue interbedded with Niobrara shales and occurs only in the Tonque Valley. A principal member of the Mesaverde formation occurs throughout the area, but the base of the member is Niobrara in age in the Tonque Valley and southern Galisteo Lowland, Montana in age in the Galisteo Monocline.
Upper Cretaceous rocks were gently warped and eroded in pre-Galisteo (pre-late Eocene) time. Maximum indicated dips are about 2°.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
Watermarked PDF Document: $14 | |
Open PDF Document: $24 |
AAPG Member?
Please login with your Member username and password.
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].