1887

Abstract

Summary

The Yucca Flat is located in the Basin and Range province and it was one of four major nuclear test regions of the Nevada National Security Site. In the past decades, many gravity stations were acquired in this site, along with an unusually high number of boreholes. This dataset is here modelled by the ITRESC method, based on the building of a depth-gravity relationship, for which a set of depth constraints (i.e., estimates of the depth to basement at some locations) are needed. The main difference between this method and most of the approaches commonly used to model the basement morphology is that the density function is not required as an input, but it is instead a product of the interpretation process. The resulting model displays many details more than previous interpretations. The maximum thickness of sediments is found to be about 1.2 km. Information about the presence of horizontal density contrasts in the sediment filling, a complexity that the method cannot take into account, can be obtained from the misfit between the basement model and the borehole depths to basement.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201901497
2019-06-03
2024-04-16
Loading full text...

Full text loading...

References

  1. Byers, F.M., Carr, W.W., Orkild, P., Quinliven, W.D. and Sargent, K. A.
    [1976] Volcanic suites and related cauldrons of Timber Mountain-Oasis Valley caldera complex, southern Nevada. U.S. Geol. Surv. Prof. Paper, 919.
    [Google Scholar]
  2. Cole, J.C.
    [1987] Breakup of an allochthonous slab: origin of the Yucca Flat Basin, Nevada Test Site. Geological Society of America Abstracts with Programs, 19, 7, p. 623.
    [Google Scholar]
  3. Healey, D.L.
    [1966] Gravity and seismic study of Yucca Flat, Nevada Test Site, Nye County, Nevada. In Harrison, D.A. and others (eds.), Mining Geophysics: Case Studies. Society of Exploration Geophysicists, 1, 84–93.
    [Google Scholar]
  4. Healey, D.L., Harris, R.N., Ponce, D.A. and Oliver, H.W.
    [1987] Complete Bouguer gravity map of the Nevada test site and vicinity, Nevada. USGS Open-File Report 87–506.
    [Google Scholar]
  5. Florio, G.
    [2018a] ITRESC: A fast and efficient method to recover the basement morphology from potential fields data. SEG 88th annual Meeting and International Exposition, 1415–1419.
    [Google Scholar]
  6. [2018b] Mapping the Depth to Basement by Iterative Rescaling of Gravity or Magnetic Data. Journal of Geophysical Research: Solid Earth, 123, 9101–9120.
    [Google Scholar]
  7. Phelps, G.A., Langenheim, V.E. and Jachens, R.C.
    [1999] Thickness of Cenozoic Deposits of Yucca Flat Inferred from Gravity Data, Nevada Test Site, Nevada. USGS Open-File Report 99–310.
    [Google Scholar]
  8. Phelps, G.A. and Graham, S.E.
    [2002] Preliminary gravity inversion model of Frenchman Flat basin, Nevada Test Site, Nevada. USGS Open-File Report 02–363.
    [Google Scholar]
  9. Ridsdill-Smith, T. and Dentith, M.
    [2000] Drape corrections of aeromagnetic data using wavelets. Exploration Geophysics, 31(2), 39–46.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201901497
Loading
/content/papers/10.3997/2214-4609.201901497
Loading

Data & Media loading...

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error