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The AAPG/Datapages Combined Publications Database

AAPG Bulletin

Abstract


Volume: 37 (1953)

Issue: 5. (May)

First Page: 961

Last Page: 974

Title: Upper Cretaceous Rocks of Galisteo-Tonque Area, North-Central New Mexico

Author(s): Charles E. Stearns (2)

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°.

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