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Quaternary Movement Along the La Jencia Fault, Central New Mexico
From abstract: The La Jencia fault is a recently reactivated late Cenozoic basin margin structure of major proportions that forms the western margin of the Rio Grande rift, which borders the eastern sides of the northern Magdalena Mountains and the southern Bear Mountains in central New Mexico. Stratigraphic throw on the fault has not been determined, but Precambrian rocks of the Magdalena Mountains are uplifted a minimum of 800 m (meters) above the adjacent basin floor, below which lie a thick section of upper Cenozoic basin-fill deposits. Most of the implied displacement is probably Neogene in age.
Date:
1988
Creator:
Machette, Michael N.
System:
The UNT Digital Library
WIPP Hydrology Program Waste Isolation Pilot Plant Southeastern New Mexico: Hydrologic Data Report #6
From introduction: This report describes the objectives, scope, design, drilling and hydrologic history, and the test results collected during permeability testing of sub-horizontal boreholes drilled in the waste-handling shaft (WHS) at the Waste Pilot Plant (WIPP) site located in southeastern New Mexico.
Date:
May 1988
Creator:
Stensrud, W. A.; Bame, M. A.; Lantz, K. D.; Cauffman, T. L.; Palmer, J. B. & Saulnier, G. J., Jr.
System:
The UNT Digital Library