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Low-temperature deformation mechanisms at a lithotectonic interface near the Sudbury Basin, Eastern Penokean Orogen, Canada

Riller, Ulrich, Schwerdtner, W.M., Robin, P.-Y.F.·1998·Tectonophysics
DOI 10.1016/s0040-1951(98)80061-9
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  • The Murray Fault System has a WNW trend in the west, swinging to an ENE trend in the east, and an E and NE trend through the Sudbury basin, where it evolves to include the South Range Shear Zone.

    “The Murray Fault System has a WNW trend in the W of the region, swinging round to an ENE trend in the E, and an E and NE trend through the Sudbury basin, where it evolves to include the South Range Shear Zone (SRSZ in Fig. 2; Riller et al. 1998).”

    From Tectonic influences on the morphometry of the Sudbury impact structure: Implications for terrestrial cratering and modeling (2004) · cites this paper as Riller et al. 1998

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Metadata

Authors
Riller, U., Schwerdtner, W. M., & Robin, P.-Y. F.
Venue
Tectonophysics
Publisher
Elsevier BV
Published
1998-03
Volume
287
Issue
1-4
Pages
59-75
ISSN
0040-1951
DOI
10.1016/s0040-1951(98)80061-9
Cited by
18
References
1
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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