Relevant bibliographies by topics / Sudbury Basin

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Sudbury Basin'

Author: Grafiati
Published: 4 June 2021
Last updated: 3 February 2022

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Journal articles on the topic "Sudbury Basin"

1

Suorineni, F. T. "The Sudbury Basin stress tensor – a critical review." CIM Journal 11, no. 3 (2020): 198–212. http://dx.doi.org/10.1080/19236026.2020.1757986.

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Lowman, Paul D. "The Sudbury Structure as a terrestrial mare basin." Reviews of Geophysics 30, no. 3 (1992): 227. http://dx.doi.org/10.1029/92rg00755.

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Trotter, Don A. "Vertical crater retreat mining in the Sudbury Basin." Mining Science and Technology 13, no. 2 (1991): 131–43. http://dx.doi.org/10.1016/0167-9031(91)91301-w.

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4

Miao, Xiao‐Gui, Wooil M. Moon, and B. Milkereit. "A multioffset, three‐component VSP study in the Sudbury Basin." GEOPHYSICS 60, no. 2 (1995): 341–53. http://dx.doi.org/10.1190/1.1443770.

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A multioffset, three‐component vertical seismic profiling (VSP) experiment was carried out in the Sudbury Basin, Ontario, as a part of the LITHOPROBE Sudbury Transect. The main objectives were determination of the shallow velocity structure in the middle of the Sudbury Basin, development of an effective VSP data processing flow, correlation of the VSP survey results with the surface seismic reflection data, and demonstration of the usefulness of the VSP method in a crystalline rock environment. The VSP data processing steps included rotation of the horizontal component data, traveltime inversion for velocity analysis, Radon transform for wavefield separation, and preliminary analysis of shear‐wave data. After wavefield separation, the flattened upgoing wavefields for both P‐waves and S‐waves display consistent reflection events from three depth levels. The VSP-CDP transformed section and corridor stacked section correlate well with the high‐resolution surface reflection data. In addition to obtaining realistic velocity models for both P‐ and S‐waves through least‐square inversion and synthetic seismic modeling for the Chelmsford area, the VSP experiment provided an independent estimation for the reflector dip using three component hodogram analysis, which indicates that the dip of the contact between the Chelmsford and Onwatin formations, at an approximate depth of 380 m in the Chelmsford borehole, is approximately 10.5° southeast. This study demonstrates that multioffset, three‐component VSP experiments can provide important constraints and auxiliary information for shallow crustal seismic studies in crystalline terrain. Thus, the VSP technique bridges the gap between the surface seismic‐reflection technique and well‐log surveys.
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5

Heath, Andrew J., and Paul F. Karrow. "Northernmost (?) Glacial Lake Algonquin Series Shorelines, Sudbury Basin, Ontario." Journal of Great Lakes Research 33, no. 1 (2007): 264–78. http://dx.doi.org/10.3394/0380-1330(2007)33[264:nglass]2.0.co;2.

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6

Whitehead, R. E. S., J. F. Davies, and Wayne D. Goodfellow. "Lithogeochemical patterns related to sedex mineralization, Sudbury Basin, Canada." Chemical Geology 98, no. 1-2 (1992): 87–101. http://dx.doi.org/10.1016/0009-2541(92)90092-j.

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7

Hearst, R. B., and W. A. Morris. "Regional gravity setting of the Sudbury Structure." GEOPHYSICS 66, no. 6 (2001): 1680–90. http://dx.doi.org/10.1190/1.1487110.

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In the vicinity of Sudbury, Ontario, Canada, the boundary between the Southern and Superior tectonic provinces is overlain by the elliptical Sudbury Structure. On the basis of gravity modeling, genesis of the Sudbury Structure has been attributed to either a magmatic origin (having a dense hidden differentiate zone) or a meteorite impact origin (there being no dense hidden mass). The difference between the two gravity models centers on the problem of regional‐residual separation. As shown by numerous previous studies, any such separation of components is nonunique. This becomes especially problematic when, as in Sudbury, a portion of the near‐surface geology has a similar orientation and dimension to more deep‐seated source. In this paper, several numerical methods (upward continuation, downward continuation, wavelength filtering, trend‐surface analysis) for determining the regional component of the gravity field associated with the Sudbury Structure have been applied and evaluated. Of the numerical methods used, the upward and downward continuation operators provided the most insight into the deep structural controls of the Sudbury Basin. Our preferred interpretation of the regional gravity field invokes a two‐component structure. Underlying the southern half of the Sudbury Structure is a laterally continuous gravity anomaly that is probably associated with a zone of uplifted Huronian volcanics. The gravity anomaly under the northern portion of the Sudbury Structure has a more restricted spatial extent. The close association between the northern limit of the gravity anomaly and the surface outcrop of the Levack Gneiss suggests the source of this anomaly is probably a slab of dense Levack Gneiss. This interpretation favors a meteorite impact origin for the Sudbury Structure.
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8

Davies, J. F., M. V. Leroux, R. E. Whitehead, and Wayne D. Goodfellow. "Oxygen-isotope composition and temperature of fluids involved in deposition of Proterozoic sedex deposits, Sudbury Basin, Ontario." Canadian Journal of Earth Sciences 27, no. 10 (1990): 1299–303. http://dx.doi.org/10.1139/e90-139.

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Sedex Cu–Pb–Zn deposits in the Sudbury Basin were deposited on the sea floor from fluids in which δ18O = −1‰ and at temperatures around 170 °C. Distal Mn-bearing sediments were deposited in seawater in which δ18O ≈ −3‰ and at temperatures around 125 °C. The fluids at the vent site (δ18O ≈ −1‰) probably represent a mixture of normal seawater and isotopically positive hydrothermal fluid generated in the substrate by seawater–rock reactions. The heat source responsible for convection and venting onto the sea floor and into the water column was the underlying Sudbury Irruptive, which was emplaced immediately following deposition of the Onaping Formation, directly above which the sedex deposits lie.
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9

Jeremic, M. L. "Possible technological changes in mining in the sudbury basin, Canada." Mining Science and Technology 2, no. 3 (1985): 163–70. http://dx.doi.org/10.1016/s0167-9031(85)90109-4.

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10

Lowman, P. D. "Correction to “The Sudbury Structure as a terrestrial mare basin”." Reviews of Geophysics 30, no. 4 (1992): 355. http://dx.doi.org/10.1029/92rg02600.

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Dissertations / Theses on the topic "Sudbury Basin"

1

Siddorn, James P. "Differential uplift of the Archean basement north of the Sudbury Basin, petrographic evidence from the Matachewan dyke swarm." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0003/MQ45527.pdf.

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2

Clark, Martin David Verfasser], and Ulrich [Akademischer Betreuer] [Riller. "The tectonic evolution of the East Range of the Sudbury Basin, Ontario, Canada / Martin David Clark ; Betreuer: Ulrich Riller." Hamburg : Staats- und Universitätsbibliothek Hamburg, 2017. http://d-nb.info/1129359360/34.

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Books on the topic "Sudbury Basin"

1

Donegan, Rosemary. The Sudbury basin: Industrial topographies = Topographies industrielles du bassin de Sudbury. Art Gallery of Sudbury = Galerie d'art de Sudbury, 1999.

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2

Butler, Hadyn R. Tectonics of impact basin formation: The Sudbury example. Geological Association of Canada, 1999.

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3

Dorfman, Richard S. The Sudbury River Basin water quality management plan, 1988. Dept. of Environmental Quality Engineering, Massachusetts Division of Water Pollution Control, Technical Services Branch, 1988.

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Butler, Hadyn R. Tectonics of impact basin information: The Sudbury example ; field trip A4 guidebook, May 25, 1999. Geological Association of Canada (GAC), Mineralogical Association of Canada (MAC), 1999.

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5

Gray, Michael J. The geological setting of the Vermilion Zn-Cu-Pb-Ag-Au massive sulphide deposit, Sudbury Basin, Ontario, Canada. Laurentian University, 1995.

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6

Stoness, Jill A. The stratigraphy, geochemistry, and depositional environment of the palaeoproterozoic Vermilion and Onwatin formations, and their relationship to the Zn-Cu-Pb massive sulphide deposits in the Sudbury Basin. Laurentian University, 1994.

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7

Zarriello, Phillip J. Effects of water use and land use on streamflow and aquatic habitat in the Sudbury and Assabet River Basins, Massachusetts. U.S. Dept. of the Interior, U.S. Geological Survey, 2010.

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8

Cowan, Ewen Jun. Deformation of the eastern Sudbury Basin. 1996.

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9

Industrial communities of the Sudbury Basin: Copper Cliff, Victoria Mines, Mond and Coniston. Sudbury & District Historical Society, 1986.

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10

Riller, Ulrich Peter. Tectonometamorphic episodes affecting the southern footwall of the Sudbury Basin and their significance for the origin of the Sudbury Igneous Complex, Central Ontario, Canada. 1996.

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Book chapters on the topic "Sudbury Basin"

1

Bunch, Ted E., Luann Becker, David Des Marais, et al. "Carbonaceous matter in the rocks of the Sudbury Basin, Ontario, Canada." In Large meteorite impacts and planetary evolution; II. Geological Society of America, 1999. http://dx.doi.org/10.1130/0-8137-2339-6.331.

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2

Wang, C., X. Zhang, and H. Zhang. "Experimental study of the temperature-pressure effect on gas transport in peridotite sample from Sudbury Basin, Canada." In Rock Stress and Earthquakes. CRC Press, 2010. http://dx.doi.org/10.1201/9780415601658-136.

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Wang, C., X. Zhang, and H. Zhang. "Experimental study of the temperature-pressure effect on gas transport in peridotite sample from Sudbury Basin, Canada." In Rock Stress and Earthquakes. CRC Press, 2010. http://dx.doi.org/10.1201/b10555-136.

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4

Spray, John G., and Marc B. Biren. "Distinguishing friction- from shock-generated melt products in hypervelocity impact structures." In Large Meteorite Impacts and Planetary Evolution VI. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2550(06).

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ABSTRACT Field, microtextural, and geochemical evidence from impact-related melt rocks at the Manicouagan structure, Québec, Canada, allows the distinction to be made between friction-generated (pseudotachylite) and shock-generated melts. Making this distinction is aided by the observation that a significant portion of the impact structure’s central peak is composed of anorthosite that was not substantially involved in the production of impact melt. The anorthosite contrasts with the ultrabasic, basic, intermediate, and acidic gneisses that were consumed by decompression melting of the >60 GPa portion of the target volume to form the main impact melt body. The anorthosite was located below this melted volume at the time of shock loading and decompression, and it was subsequently brought to the surface from 7–10 km depth during the modification stage. Slip systems (faults) within the anorthosite that facilitated its elevation and collapse are occupied by pseudotachylites possessing anorthositic compositions. The Manicouagan pseudotachylites were not shock generated; however, precursor fracture-fault systems may have been initiated or reactivated by shock wave passage, with subsequent tectonic displacement and associated frictional melting occurring after shock loading and rarefaction. Pseudotachylites may inject off their generation planes to form complex intrusive systems that are connected to, but are spatially separated from, their source horizons. Comparisons are made between friction and shock melts from Manicouagan with those developed in the Vredefort and Sudbury impact structures, both of which show similar characteristics. Overall, pseudotachylite has compositions that are more locally derived. Impact melts have compositions reflective of a much larger source volume (and typically more varied source lithology inputs). For the Manicouagan, Vredefort, and Sudbury impact structures, multiple target lithologies were involved in generating their respective main impact melt bodies. Consequently, impact melt and pseudotachylite can be discriminated on compositional grounds, with assistance from field and textural observations. Pseudotachylite and shock-generated impact melt are not the same products, and it is important not to conflate them; each provides valuable insight into different stages of the hypervelocity impact process.
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Conference papers on the topic "Sudbury Basin"

1

Suorineni, Fidelis, and Farid Malek. "The Sudbury Basin stress tensor – myth or reality?" In Seventh International Conference on Deep and High Stress Mining. Australian Centre for Geomechanics, Perth, 2014. http://dx.doi.org/10.36487/acg_rep/1410_43_suorineni.

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Landry, David, and Eliot Reimer. "Failure mechanisms and ground support observations at Coleman mine, Sudbury Basin." In Ninth International Symposium on Ground Support in Mining and Underground Construction. Australian Centre for Geomechanics, Perth, 2019. http://dx.doi.org/10.36487/acg_rep/1925_16_landry.

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3

Zajch, A., B. Milkereit, and N. Eyles. "High Resolution Marine Seismic Surveying in the Sudbury Basin, Ontario, Canada." In Near Surface Geoscience 2016 - Second Applied Shallow Marine Geophysics Conference. EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201602166.

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4

Miao, X. G., W. M. Moon, and B. Milkerit. "Seismic reflection imaging of the crustal structure in the northwest of the Sudbury Basin." In SEG Technical Program Expanded Abstracts 1994. Society of Exploration Geophysicists, 1994. http://dx.doi.org/10.1190/1.1931976.

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Fullagar, P. K., P. Zhang, Y. Wu, and M. ‐J Bertrand. "Application of radio frequency tomography to delineation of nickel sulphide deposits in the Sudbury Basin." In SEG Technical Program Expanded Abstracts 1996. Society of Exploration Geophysicists, 1996. http://dx.doi.org/10.1190/1.1826585.

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6

Milkereit, B., B. Roberts, E. Adam, and A. King. "Integrated borehole geophysical and 3‐D seismic study of a deep massive sulfide deposit, Sudbury Basin, Canada." In SEG Technical Program Expanded Abstracts 1998. Society of Exploration Geophysicists, 1998. http://dx.doi.org/10.1190/1.1820587.

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