Proximal and distal braided alluvial facies in the lower braided interval of the Dakota Sandstone, northeastern New Mexico
— George B. Asquith and J. L. Gilbert
Abstract:
The study area is located in the northeastern corner of New Mexico. Approximate boundaries are the Texas-Oklahoma-New Mexico border, the Colorado-New Mexico border, the extreme eastern edge of the Sangre de Cristo Mountains, and Interstate Highway 40.
Full-text (760 KB PDF)
Recommended Citation:
- Asquith, George B.; Gilbert, J. L., 1976, Proximal and distal braided alluvial facies in the lower braided interval of the Dakota Sandstone, northeastern New Mexico, in: Vermejo Park, Ewing, Rodney C.; Kues, Barry S., New Mexico Geological Society, Guidebook, 27th Field Conference, pp. 153-155. https://doi.org/10.56577/FFC-27.153