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Rubidium-strontium and related studies of the Salado Formation, southeastern New Mexico

Technical Report ·
OSTI ID:5790851

The Salado Formation, a member of the Ochoa Series, is a bedded salt deposit which is found in the Delaware Basin of southeastern New Mexico and west Texas. It is comprised primarily of halite and sylvite with minor amounts of sulfate minerals. Rubidium-strontium age determinations of the evaporite minerals in the Salado indicate an age of final equilibration of 214 +- 15 m.y. This age is fairly consistent with the geologic age of the formation, precluding substantial alkali-alkaline earth migration since deposition. Polyhalite and anhydrite samples from the Salado give /sup 87/Sr//sup 86/Sr values of about .7078, which are consistent with reported values for Permian seawater. The REE and trace element concentrations of the polyhalite and anhydrite samples are very low, reflecting the composition of seawater. Rubidium-strontium age determinations of the clay minerals extracted from the salt suggest a minimum age of 390 +- 77 m.y. This age probably represents the minimum age of the provenance of the clay minerals. The REE and trace element concentrations as well as the mineralogy of the clay minerals indicate a detrital origin for the clay minerals with some clay-brine interaction. Clay minerals seem generally depleted in the light REE (relative to NAS) which most likely were replaced by Ca/sup 2 +/ and Na/sup +/ from the evaporitic brines.

Research Organization:
Sandia National Labs., Albuquerque, NM (USA); New Mexico Univ., Albuquerque (USA). Dept. of Geology
DOE Contract Number:
AC04-76DP00789
OSTI ID:
5790851
Report Number(s):
SAND-81-7072; ON: DE82006832
Country of Publication:
United States
Language:
English

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