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Title: Mineralogy of the Culebra Dolomite Member of the Rustler Formation

Technical Report ·
DOI:https://doi.org/10.2172/5524095· OSTI ID:5524095
; ;  [1]
  1. New Mexico Univ., Albuquerque, NM (USA)

This report characterizes the mineralogy of the Culebra Member of the Rustler Formation based on studies of samples from cores of eight boreholes surrounding the WIPP repository. This investigation has three main goals: to obtain accurate modal compositions of all the samples selected; to investigate both the lateral and vertical variation of the mineralogy of the Culebra unit; and, to characterize water-bearing fracture surfaces in particular detail. The Culebra Dolomite member of the Rustler Formation is mineralogically and texturally heterogeneous, both vertically and horizontally. Although the predominant mineral is dolomite, important constituents of the formation are clay, quartz, gypsum, and calcite. Trace minerals include halite, phyllosilicates of metamorphic origin, feldspar, and pyrite. 24 refs., 90 figs., 27 tabs.

Research Organization:
Sandia National Lab. (SNL-NM), Albuquerque, NM (United States); New Mexico Univ., Albuquerque, NM (USA)
Sponsoring Organization:
USDOE; USDOE, Washington, DC (USA)
DOE Contract Number:
AC04-76DP00789
OSTI ID:
5524095
Report Number(s):
SAND-90-7008; ON: DE91014327; TRN: 91-018468
Country of Publication:
United States
Language:
English

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