1887

Abstract

Summary

Thin planar sheets are useful target models for geological structures such as dykes and veins, which are essentially two-dimensional on survey scales. We derive the gravity potential, field and field gradient for such targets. We concentrate on triangular sheets, because these can be assembled into a drape surface, with continuous densities across the boundaries, so as to approximate general curved surfaces. We verify the correctness of the anomaly formulae via numerical testing, and model a scenario with dyke curvature and density compaction.

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/content/papers/10.3997/2214-4609.20140892
2014-06-16
2024-04-25
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References

  1. Holstein, H.
    [2003] Gravimagnetic anomaly formulas for polyhedra of spatially linear media. Geophysics, 68, 157–167.
    [Google Scholar]
  2. Holstein, H., Fitzgerald, D. and Anastasiades, C.
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    [Google Scholar]
  3. Holstein, H., Sherratt, E. and Reid, A.
    [2007] Gravimagnetic field tensor gradiometry formulas for uniform polyhedra. Proceedings of the 77th Annual Meeting of the Society of Exploration Geophysicists (San Antonio, Texas).
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