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Fold origin of the NE-lobe of the Sudbury Basin, Canada: Evidence from heterogeneous fabric development in the Onaping Formation and the Sudbury Igneous Complex
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The Sudbury structure has been extensively tectonized following the impact.
“The structural situation is further complicated by the fact that the Sudbury structure has been extensively tectonized following the impact (Riller 2005;Klimczak et al. 2007).”
From Observations and interpretations at Vredefort, Sudbury, and Chicxulub: Towards an empirical model of terrestrial impact basin formation (2008) · cites this paper as Klimczak et al. 2007
Given that the northeast lobe of the SIC represents a fold and the SIC in the East Range has been extensively deformed by the Penokean orogeny, and given the relatively crude nature of the scaling of Vredefort structures to Sudbury, this is not necessarily an inconsistency.
“In as much as the northeast lobe of the SIC represents a fold (Klimczak et al. 2007) and the SIC in the East Range has been extensively deformed by the Penokean orogeny, e.g., it dips ~70° towards the center of the Sudbury Basin (Riller 2005), and given the relatively crude nature of the scaling of Vredefort structures to Sudbury, this is not necessarily an inconsistency.”
From Observations and interpretations at Vredefort, Sudbury, and Chicxulub: Towards an empirical model of terrestrial impact basin formation (2008) · cites this paper as Klimczak et al. 2007
Citations
Cites
Spray, J. G., Butler, H. R., & Thompson, L. M. (2004) · Meteoritics & Planetary Science · doi:10.1111/j.1945-5100.2004.tb00341.x · Cited by 75
Schwerdtner, W. M., & van Berkel, J. T. (1991) · Precambrian Research · doi:10.1016/0301-9268(91)90055-f · Cited by 19
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Research works printed but not linked: 40
- Avermann, 1999, The Green Member of the Onaping Formation, the collapsed fireball layer of the Sudbury impact structure, Ontario, Canada, vol. 339, 323
- Bailey, 2004, Mazatzal–Labradorian-age (1.7–1.6Ga) ductile deformation of the South Range Sudbury impact structure at the Thayer Lindsley mine, Ontario, Canadian Journal of Earth Sciences, 41, 1492, 10.1139/e04-098 · DOI
- Boerner, 2000, Seismic images and three-dimensional architecture of a Proterozoic shear zone in the Sudbury structure (Superior Province, Canada), Tectonics, 19, 397, 10.1029/1999TC900060 · DOI
- Bray, 1966, Shatter cones at Sudbury, Journal of Geology, 74, 243, 10.1086/627158 · DOI
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- Card, 1984, The Sudbury Structure: its regional geological and geophysical setting, vol. 1, 25
- Coleman, A.P., 1905. The Sudbury Nickel region. Ontario Bureau of Mines Annual Report 14 (3), 1–188.
- Coleman, 1907, The Sudbury laccolith sheet, Journal of Geology, 15, 759, 10.1086/621473 · DOI
- Collins, 1935, Life history of the Sudbury Nickel Irruptive. Part II. Intrusion and deformation, Transactions of the Royal Society of Canada, 29, 27
- Cowan, 1999, Magnetic fabric constraints on the initial geometry of the Sudbury Igneous Complex: a folded sheet or a basin-shaped igneous body?, Tectonophysics, 307, 135, 10.1016/S0040-1951(99)00123-7 · DOI
- Cowan, 1999, Emplacement geometry of the Sudbury Igneous Complex: structural examination of a proposed impact melt-sheet, vol. 339, 399
- Cowan, E.J., Schwerdtner, W.M., 1994. Fold origin of the Sudbury Basin. In: Ontario Geological Survey Special Paper, vol. 5, 45–55.
- Deutsch, 1995, The Sudbury Structure (Ontario, Canada): a tectonically deformed multi-ring basin, Geologische Rundschau, 84, 697, 10.1007/s005310050034 · DOI
- Doman, 2007, The importance of discontinuous deformation in the eastern Sudbury Igneous Complex, Geophysical Research Abstracts, 9, 10220
- Dressler, 1984, General geology of the Sudbury Structure, vol. 1, 57
- Dressler, 1984, The effects of the Sudbury event and the intrusion of the Sudbury Igneous Complex on the footwall rocks of the Sudbury structure, vol. 1, 97
- Ferry, 1979, Reaction mechanisms, physical conditions, and mass transfer during hydrothermal alteration of mica and feldspar in granitic rocks from south-central Maine, USA, Contributions to Mineralogy and Petrology, 68, 125, 10.1007/BF00371895 · DOI
- Fitz Gerald, 1993, Deformation of granitoids at low metamorphic grades. I. Reactions and grain size reduction, Tectonophysics, 221, 269, 10.1016/0040-1951(93)90163-E · DOI
- Fleet, 1987, Prograde metamorphism of the Sudbury Igneous Complex, Canadian Mineralogist, 25, 499
- Grieve, 1991, The Sudbury Structure: controversial or misunderstood?, Journal of Geophysical Research, 96, 22753, 10.1029/91JE02513 · DOI · Paper page
- Ivanov, 1999, Sudbury impact event: cratering mechanics and thermal history, vol. 339, 389
- Klimczak, C., 2006. Deformation of the Onaping Formation in the NE-lobe of the Sudbury Igneous Complex, Ontario, Canada. Unpublished Diploma thesis. Free University Berlin, Germany, 72 pp.
- Krogh, 1982, Two high-precision U–Pb zircon ages for the Sudbury Nickel Irruptive, Canadian Journal of Earth Sciences, 19, 723, 10.1139/e82-061 · DOI
- Krogh, 1984, Precise U–Pb Zircon and Baddeleyite ages for the Sudbury area, vol. 1, 431
- Milkereit, 1992, Deep geometry of the Sudbury structure from seismic reflection profiling, Geology, 20, 807, 10.1130/0091-7613(1992)020<0807:DGOTSS>2.3.CO;2 · DOI
- Muir, 1984, The Onaping Formation, vol. 1, 139
- Peredery, 1984, Discussion of the origin of the Sudbury structure, vol. 1, 491
- Prevec, 2002, Thermal evolution and interaction between impact melt sheet and footwall: a genetic model for the contact sublayer of the Sudbury Igneous Complex, Canada, Journal of Geophysical Research, 107, 2176, 10.1029/2001JB000525 · DOI
- Riller, 2005, Structural characteristics of the Sudbury impact structure, Canada: impact-induced versus orogenic deformation – a review, Meteoritics & Planetary Science, 40, 1723, 10.1111/j.1945-5100.2005.tb00140.x · DOI · Paper page
- Riller, 1997, Mid-crustal deformation at the southern flank of the Sudbury Basin, central Ontario, Canada, Geological Society of America Bulletin, 109, 841, 10.1130/0016-7606(1997)109<0841:MCDATS>2.3.CO;2 · DOI
- Riller, 1998, Low-temperature deformation mechanisms at a lithotectonic interface near the Sudbury Basin, Eastern Penokean Orogen, Canada, Tectonophysics, 287, 59, 10.1016/S0040-1951(98)80061-9 · DOI · Paper page
- Riller, 1999, Transpressive tectonism in the eastern Penokean orogen, Canada: consequences for Proterozoic crustal kinematics and continental fragmentation, Precambrian Research, 93, 51, 10.1016/S0301-9268(98)00097-7 · DOI
- Rousell, 1984, Structural geology of the Sudbury basin, vol. 1, 83
- Schwerdtner, 1998, Graphic derivation of the local sense of shear of shear strain components in stretched walls of lithotectonic boundaries, Journal of Structural Geology, 20, 957, 10.1016/S0191-8141(98)00019-4 · DOI
- Schwerdtner, 2005, Structural testing of tectonic hypotheses by field-based analysis of distributed tangential shear: concrete examples from major high-strain zones in the Grenville Province and other parts of the southern Canadian Shield, Canadian Journal of Earth Sciences, 42, 1905, 10.1139/e05-047 · DOI
- Shanks, 1991, Structural analysis of the central and southwestern Sudbury Structure, Southern Province, Canadian Shield, Canadian Journal of Earth Sciences, 28, 411, 10.1139/e91-037 · DOI · Paper page
- Spray, 1995, Friction melt distribution in a multi-ring impact basin, Nature, 373, 130, 10.1038/373130a0 · DOI · Paper page
- Stipp, 2002, The eastern Tonale fault zone: a ‘natural laboratory’ for crystal plastic deformation of quartz over a temperature range from 250 to 700°C, Journal of Structural Geology, 24, 1861, 10.1016/S0191-8141(02)00035-4 · DOI
- Therriault, 2002, The Sudbury Igneous Complex, a differentiated impact melt sheet, Economic Geology, 97, 1521, 10.2113/gsecongeo.97.7.1521 · DOI · Paper page
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Cited by
Sorted by citations
GRIEVE, R. A. F., REIMOLD, W. U., MORGAN, J., RILLER, U., & PILKINGTON, M. (2008) · Meteoritics & Planetary Science · doi:10.1111/j.1945-5100.2008.tb01086.x · Cited by 90
Self-citation
Metadata
- Authors
- Klimczak, C., Wittek, A., Doman, D., & Riller, U.
- Venue
- Journal of Structural Geology
- Publisher
- Elsevier BV
- Published
- 2007-11
- Volume
- 29
- Issue
- 11
- Pages
- 1744-1756
- ISSN
- 0191-8141
- Cited by
- 22
- References
- 2
- Language
- en
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