Cited by 33

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Integrated seismic and borehole geophysical study of the Sudbury Igneous Complex

Milkereit, B., Green, A., Wu, J., White, D., Adam, E.·1994·Geophysical Research Letters

Abstract

Reflection seismic and borehole geophysical data place important constraints on the subsurface geometry of the Sudbury Structure, which is the site of the world's largest Ni‐Cu camp. Seismic reflections can be traced from outcrop within the Sudbury North Range to about 4.5 km depth beneath the center of the Sudbury Basin, where the layer thickens abruptly from 1 to 3 km. Further south the North Range norite can be followed to about 10 km depth beneath the South Range. Borehole studies show systematic variations of p‐ and s‐wave velocity, Poisson's ratio and density within the Igneous Complex. Quartz‐rich granophyre is distinguished from the norite and footwall rocks by relatively low Poisson's ratios (0.20–0.23 versus 0.23–0.25). These changes in physical rock properties define an important subdivision of the Igneous Complex, compatible with a simple model involving differentiation of melted crustal rock into dominantly felsic and mafic components. This study documents the importance of interlayering to the seismic reflection response of the crystalline crust.

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  • The most obvious current expression of the center of the Sudbury structure is the elliptical ~30 × 60 km Sudbury Basin bounded by the folded SIC, which dips ~30° to the south in the North Range and is subject to relatively high-angle reverse faulting (South Range Shear Zone) in the South Range.

    “The net result is that the most obvious current expression of the center of the structure is the elliptical ~30 × 60 km Sudbury Basin bounded by the folded SIC, which dips ~30° to the south in the so-called North Range and is subject to relatively high-angle reverse faulting (South Range Shear Zone) in the so-called South Range (Fig. 5; Milkereit et al. 1992Milkereit et al. , 1994)).”

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Research works printed but not linked: 6

  1. 10.1029/92RG00755 · DOI
  2. 10.1130/0091-7613(1992)020<0807:DGOTSS>2.3.CO;2 · DOI
  3. 10.1029/JB088iB03p02345 · DOI
  4. Naldrett A. J., 1984, The Geology of Ore Deposits of the Sudbury Structure, 533
  5. 10.1139/e91-037 · DOI · Paper page
  6. 10.1029/92JB01744 · DOI

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Metadata

Authors
Milkereit, B., Green, A., Wu, J., White, D., & Adam, E.
Venue
Geophysical Research Letters
Published
1994-05-15
Volume
21
Issue
10
Pages
931-934
ISSN
  • 0094-8276
  • 1944-8007
Cited by
33
References
0
Language
en

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