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Deformation history of competent interbeds in layered evaporites, waste isolation pilot plant (WIPP), SE New Mexico

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6683263

Evaporite sequence have been studied as hosts for radioactive wastes. In addition to halite, layered evaporites are characterized by anhydritic, dolomitic and argillitic interbeds. Such interbeds range in thickness from centrimeters to meters. Questions regarding such interbeds are: 1) are there structural events masked in halite but exhibited in the interbeds; 2) will the interbeds have structurally distinct behavior, relative to halite, during creep closure of a repository; 3) can fluid migrate in the interbeds. With the development of the WIPP site, an interbed was exposed in shafts and drillcore at 2200ft below ground level. Study of this interbed addresses the questions above. 1) Structural events: As exhibited in the anhydritic interbed, some structures formed during deposition and diagenesis. Depositional structures are evident in the reworking of the interbed during the transition back into halite deposition. Post-diagenetic fractures, now partially infilled by polyhalite and halite, formed in the interbed. Later-stage fluids have become concentrated in fractures of the interbed. Such fluids are pressurized but irregularly distributed. Such fluid concentrations, whether in the geologic past or in the present as a response to the mined environment, could result from the migration of in situ fluids down pressure gradients into a fracture system, as it propagated in the past and/or present.

Research Organization:
Sandia National Laboratories, Albuquerque, NM (USA)
OSTI ID:
6683263
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Vol. 17; ISSN GAAPB
Country of Publication:
United States
Language:
English

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