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Crustal evolution of the Laurentian continental margin from the Paleo- through Mesoproterozic: A zircon U–Pb and Hf transect through the western Grenville Province, Ontario, Canada

Culshaw, Nicholas, Van De Kerckhove, Samantha, Slagstad, Trond, Marsh, Jeff, Easton, Robert Michael·2023·Precambrian Research
DOI 10.1016/j.precamres.2023.106963
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Abstract

The Great Proterozoic Accretionary Orogeny along the southern and southeastern margin of Laurentia is arguably the first long-lived, modern-style active plate margin on Earth, representing significant crustal growth and reworking. Here, we present new detrital zircon U–Pb and Hf data, along with zircon and monazite metamorphic ages, from tectonic domains in the southwestern Grenville Province that represent depositional basins formed and reworked during a series of events between 2.2 and 1.2 Ga. As such, the data allow a glimpse into the evolution and assembly of this extensive margin. The Nepewassi domain contains Archean basement overlain by mature sandstone characterized by near-unimodal, ca. 2.7–2.6 Ga detrital zircon peaks and likely correlative with Superior Province basement and its Huronian cover. The Nepewassi domain underwent both Archean (ca. 2.65 Ga) and Killarnean (ca. 1.76 Ga) metamorphism. In addition, all units preserve evidence of Grenvillian high-grade metamorphism between ca. 1.05 and 0.99 Ga. The structurally highest parts of the Nepewassi domain also contain younger sedimentary rocks that received detritus from Killarnean sources, with evolved Hf isotopic compositions indicative of reworked Archean crust. Sedimentary rocks in the Tomiko domain preserve detrital zircon of Penokean and Killarnean age (1.9–1.7 Ga) with evolved Hf compositions, along with Labradorian (1.7–1.6 Ga) grains of more juvenile composition. Detrital zircon from the Kiosk domain yield…

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  • The Shawinigan orogeny is included by some authors in the Grenvillian orogeny sensu lato.

    “and is included by some authors in the Grenvillian orogeny sensu lato (e.g., Corrigan and Hanmer 1997;Culshaw et al. 2023).”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Culshaw et al. 2023

  • The Shawinigan orogeny follows cessation of arc-related calc-alkalic magmatism (at ca.1.20 Ga) in the Grenville Province.

    “The Shawinigan orogeny follows cessation of arc-related calc-alkalic magmatism (at ca.1.20 Ga) in the Grenville Province”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Culshaw et al. 2023

  • The 1.50-1.35 Ga domains in the west have mixed Nd model ages and continental arc affinities with some juvenile remnants, correlated with the Granite-Rhyolite Province.

    “mixed Nd model ages and continental arc affinities with some juvenile remnants in the west (e.g., Culshaw et al. 2023), correlated with the Granite-Rhyolite Province (Fig. 1a; Slagstad et al. 2009).”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Culshaw et al. 2023

  • The southern part of the Parautochthonous Belt in Ontario preserves a record of mid- to late-Ottawan ages including ca.1035 Ma in southern Britt domain and 1040-1032 Ma in Tomico domain.

    “the southern part of the Parautochthonous Belt in Ontario preserves record of mid-to late-Ottawan ages including ca.1035 Ma in southern Britt domain (U-Pb monazite Corrigan et al. 1994) and 1040-1032 Ma in Tomico domain (U-Pb monazite, LA-ICP-MS; Culshaw et al. 2023)”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Culshaw et al. 2023

  • Late-Ottawan metamorphic ages were reported in Parautochthonous domains next to the hinterland in the western Grenville Province in Ontario (e.g., Britt and Tomico domains).

    “Late-Ottawan metamorphic ages were reported in Parautochthonous domains next to the hinterland in western Grenville Province in Ontario (e.g., Britt and Tomico domains; Culshaw et al. 2023)”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Culshaw et al. 2023

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Flagged first, then by citations

Research works printed but not linked: 105

  1. Bédard, 2014, Neoarchean disaggregation and reassembly of the Superior craton, Geology, 42, 951, 10.1130/G35770.1 · DOI
  2. Bouvier, 2008, The Lu–Hf and Sm–Nd isotopic composition of CHUR: constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets, Earth Planet. Sci. Lett., 273, 48, 10.1016/j.epsl.2008.06.010 · DOI
  3. Bowins, 1991, Age and timing of igneous activity in the Temagami greenstone belt, Ontario: a preliminary report, Can. J. Earth Sci., 28, 1873, 10.1139/e91-167 · DOI
  4. Card, 1979, Regional geological synthesis, central Superior Province. Current Research, Geol. Surv. Can. Pap., 79–1A, 87
  5. Carr, 2000, Geologic transect across the Grenville orogen of Ontario and New York, Can. J. Earth Sci., 37, 193, 10.1139/e99-074 · DOI · Paper page
  6. Cawood, 2012, Detrital zircon record and tectonic setting, Geology, 40, 875, 10.1130/G32945.1 · DOI
  7. Chen, 1995, Neoarchean trondhjemitic and tonalitic orthogneisses identified within the northern Grenville Province in Ontario by precise U-Pb dating and petrologic studies, Precambr. Res., 72, 263, 10.1016/0301-9268(94)00094-8 · DOI
  8. Chen, 2022, Intraplate continental basalts over the past billion years track cooling of the mantle and the onset of modern plate tectonics, Earth Planet. Sci. Lett., 597, 10.1016/j.epsl.2022.117804 · DOI
  9. Collins, 2002, Hot orogens, tectonic switching, and creation of continental crust, Geology, 30, 535, 10.1130/0091-7613(2002)030<0535:HOTSAC>2.0.CO;2 · DOI
  10. Collins, 2003, Slab pull, mantle convection, and Pangean assembly and dispersal, Earth Planet. Sci. Lett., 205, 225, 10.1016/S0012-821X(02)01043-9 · DOI
  11. Colpron, 2015, Birth of the northern Cordilleran orogen, as recorded by detrital zircons in Jurassic synorogenic strata and regional exhumation in Yukon, Lithosphere, 7, 541, 10.1130/L451.1 · DOI
  12. Condie, 2013, Preservation and Recycling of Crust during Accretionary and Collisional Phases of Proterozoic Orogens: A Bumpy Road from Nuna to Rodinia, Geosciences, 3, 240, 10.3390/geosciences3020240 · DOI · Paper page
  13. Corfu, 1986, A U-Pb age for mineralized Nipissing diabase, Gowganda, Ontario, Can. J. Earth Sci., 23, 107, 10.1139/e86-011 · DOI
  14. Corfu, 1995, U-Pb geochronology of the Mazinaw terrane, an imbricate segment of the Central Metasedimentary Belt, Grenville Province, Ontario, Can. J. Earth Sci., 32, 959, 10.1139/e95-081 · DOI
  15. Corfu, 2001, U-Pb evidence for polymetamorphic history of Huronian rocks within the Grenville front tectonic zone east of Sudbury, Ontario, Canada, Chem. Geol., 172, 149, 10.1016/S0009-2541(00)00241-2 · DOI · Paper page
  16. Corrigan, 1994, Pre-Grenvillian evolution and Grenvillian overprinting of the Parautochthonous Belt in Key Harbour, Ontario: U-Pb and field constraints, Can. J. Earth Sci., 31, 583, 10.1139/e94-051 · DOI · Paper page
  17. Coutts, 2019, Assessment of widely used methods to derive depositional ages from detrital zircon populations, Geosci. Front., 10, 1421, 10.1016/j.gsf.2018.11.002 · DOI
  18. Craddock, 2013, Detrital Zircon Geochronology and Provenance of the Paleoproterozoic Huron (∼2.4–2.2 Ga) and Animikie (∼2.2–1.8 Ga) Basins, Southern Superior Province, J. Geol., 121, 623, 10.1086/673265 · DOI
  19. Culshaw, 2006, The orogenic superstructure-infrastructure concept: Revisited, quantified, and revived, Geology, 34, 733, 10.1130/G22793.1 · DOI
  20. Culshaw, 1997, Sand Bay gneiss association, Grenville Province, Ontario: A Grenvillian rift- (and -drift) assemblage stranded in the Central Gneiss Belt?, Precambr. Res., 85, 97, 10.1016/S0301-9268(97)00036-3 · DOI
  21. Culshaw, 2000, Structural evolution of the Makkovik Province, Labrador, Canada: Tectonic processes during 200 Myr at a Paleoproterozoic active margin, Tectonics, 19, 961, 10.1029/1999TC001156 · DOI
  22. Culshaw, 2013, Geochemical, geochronological and isotopic constraints on the origin of members of the allochthonous Shawanaga and basal Parry Sound domains, Central Gneiss Belt, Grenville Province, Ontario, Precambr. Res., 228, 131, 10.1016/j.precamres.2013.01.012 · DOI
  23. Culshaw, 2016, Kiosk domain, Central Gneiss Belt, Grenville Province, Ontario: A Labradorian palimpsest preserved in the ductile deep crust, Precambr. Res., 280, 249, 10.1016/j.precamres.2016.05.002 · DOI · Paper page
  24. Davey, 2019, Ni-Cu-PGE potential of the Nipissing sills as part of the ca. 2.2 Ga Ungava large igneous province, Targeted Geoscience Initiative: 2018 report of activities; Geological Survey of Canada, Open File, 8549, 403
  25. Davidson, 2008, Late Paleoproterozoic to mid-Neoproterozoic history of northern Laurentia: An overview of central Rodinia, Precambr. Res., 160, 5, 10.1016/j.precamres.2007.04.023 · DOI
  26. Davidson, A., van Breemen, O., 2001. Mid-Mesoproterozoic granitoid rocks in the North Bay area, Grenville Province, Ontario. Radiogenic Age and Isotopic Studies: Report 14. Geological Survey of Canada, Current Research 2001-F8, 15. · DOI
  27. Davidson, 1992, Circa 1.75 Ga ages for plutonic rocks from the Southern province and adjacent Grenville Province: What is the expression of the Penokean orogeny? Radiogenic Age and Isotopic Studies: Report 6, Geol. Surv. Can. Pap., 92–2, 107
  28. Davis, 2002, U-Pb geochronology of Archean metasedimentary rocks in the Pontiac and Abitibi subprovinces, Quebec, constraints on timing, provenance and regional tectonics, Precambr. Res., 115, 97, 10.1016/S0301-9268(02)00007-4 · DOI
  29. Dickin, 2000, Crustal formation in the Grenville Province: Nd-isotopic evidence, Can. J. Earth Sci., 37, 165, 10.1139/e99-039 · DOI
  30. Dickin, 1992, Sm/Nd evidence for a major 1.5 Ga crust-forming event in the central Grenville province, Geology, 20, 137, 10.1130/0091-7613(1992)020<0137:SNEFAM>2.3.CO;2 · DOI
  31. Dickin, 1989, Nd model age mapping of the southeast margin of the Archean foreland in the Grenville province of Ontario, Geology, 17, 299, 10.1130/0091-7613(1989)017<0299:NMAMOT>2.3.CO;2 · DOI
  32. Dickin, 2007, The Central Metasedimentary Belt (Grenville Province) as a failed back-arc rift zone: Nd isotope evidence, Earth Planet. Sci. Lett., 259, 97, 10.1016/j.epsl.2007.04.031 · DOI
  33. Dickin, 2008, Isotopic mapping of the Allochthon Boundary Thrust in the Grenville Province of Ontario, Canada, Precambr. Res., 167, 260, 10.1016/j.precamres.2008.08.007 · DOI
  34. Dickin, 2010, The extent of juvenile crust in the Grenville Province: Nd isotope evidence, GSA Bull., 122, 870, 10.1130/B26381.1 · DOI
  35. Dickin, 2017, A revised model for the crustal structure of the SW Grenville Province, Ontario, Canada, Geol. Mag., 154, 903, 10.1017/S001675681700005X · DOI
  36. Dickin, 2019, Nd isotope mapping of the Grenvillian Allochthon Boundary Thrust in Algonquin Park, Ontario, Can. J. Earth Sci., 56, 101, 10.1139/cjes-2018-0142 · DOI
  37. Easton, 2000, Metamorphism of the Canadian Shield, Ontario, Canada, I. The Superior Province. Canadian Mineralogist, 38, 287, 10.2113/gscanmin.38.2.287 · DOI
  38. Easton, R.M., 1992. The Grenville Province and the Proterozoic history of central and southern Ontario, in: Thurston, P.C., Williams, H.R., Sutcliffe, R.H., Stott, G.M. (Eds.), Geology of Ontario, Ontario Geological Survey Special Volume 4, Part 2, pp. 715-904.
  39. Ernst, R., Bleeker, W., 2010. Large igneous provinces (LIPs), giant dyke swarms, and mantle plumes: significance for breakup events within Canada and adjacent regions from 2.5 Ga to the PresentThis article is one of a selection of papers published in this Special Issue on the the theme Lithoprobe—parameters, processes, and the evolution of a continent.Lithoprobe Contribution 1482. Geological Survey of Canada Contribution 20100072. Canadian Journal of Earth Sciences 47, 695-739. · DOI
  40. Fisher, 2011, Synthetic zircon doped with hafnium and rare earth elements: A reference material for in situ hafnium isotope analysis, Chem. Geol., 286, 32, 10.1016/j.chemgeo.2011.04.013 · DOI
  41. Galbraith, 1993, Statistical models for mixed fission track ages, Nucl. Tracks Radiat. Meas., 21, 459, 10.1016/1359-0189(93)90185-C · DOI
  42. Gehrels, 2000, Tectonic implications of detrital zircon data from Paleozoic and Triassic strata in western Nevada and Northern California, Paleozoic and Triassic paleogeography and tectonics of western Nevada and Northern California, Geological Society of America, 133
  43. Green, 1988, Crustal structure of the Grenville front and adjacent terranes, Geology, 16, 788, 10.1130/0091-7613(1988)016<0788:CSOTGF>2.3.CO;2 · DOI · Paper page
  44. Griffin, 2000, The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites, Geochim. Cosmochim. Acta, 64, 133, 10.1016/S0016-7037(99)00343-9 · DOI
  45. Griffin, 2002, Zircon chemistry and magma mixing, SE China: in-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes, Lithos, 61, 237, 10.1016/S0024-4937(02)00082-8 · DOI
  46. Haggart, 1993, Last gasp of the Grenville orogeny - thermochronology of the Grenville Front Tectonic Zone near Killarney, Ontario, J. Geol., 101, 575, 10.1086/648250 · DOI · Paper page
  47. Heaman, 1997, Global mafic magmatism at 2.45 Ga: Remnants of an ancient large igneous province?, Geology, 25, 299, 10.1130/0091-7613(1997)025<0299:GMMAGR>2.3.CO;2 · DOI
  48. Hill, 2018, New U-Pb geochronology evidence for 2.3 Ga detrital zircon grains in the youngest Huronian Supergroup formations, Canada. Precambrian Research, 314, 428, 10.1016/j.precamres.2018.07.001 · DOI
  49. Holland, 2020, Geochronologic and Hf-isotope framework of Proterozoic rocks from central New Mexico, USA: Formation of the Mazatzal crustal province in an extended continental margin arc, Precambr. Res., 347, 10.1016/j.precamres.2020.105820 · DOI
  50. Holm, 2007, Reinterpretation of Paleoproterozoic accretionary boundaries of the north-central United States based on a new aeromagnetic-geologic compilation, Precambr. Res., 157, 71, 10.1016/j.precamres.2007.02.023 · DOI
  51. Holmden, 1995, Paleoproterozoic crustal history of the southwestern Grenville Province: evidence from Nd isotopic mapping, Can. J. Earth Sci., 32, 472, 10.1139/e95-040 · DOI
  52. Hynes, 2010, Protracted continental collision - evidence from the Grenville Orogen, Can. J. Earth Sci., 47, 591, 10.1139/E10-003 · DOI · Paper page
  53. Jackson, 2004, The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology, Chem. Geol., 211, 47, 10.1016/j.chemgeo.2004.06.017 · DOI
  54. James, 2002, The East Bull Lake Intrusive Suite: Remnants of a ∼2.48 Ga Large Igneous and Metallogenic Province in the Sudbury Area of the Canadian Shield, Econ. Geol., 97, 1577
  55. Jamieson, 1995, North-west propagation of the Grenville Orogen: Grenvillian structure and metamorphism near Key Harbour, Georgian Bay, Ontario, J. Metam. Geol., 13, 185, 10.1111/j.1525-1314.1995.tb00213.x · DOI · Paper page
  56. Jamieson, 2010, The Grenville Orogen explained? Applications and limitations of integrating numerical models with geological and geophysical data, Can. J. Earth Sci., 47, 517, 10.1139/E09-070 · DOI
  57. Kemp, 2017, Hafnium Isotope Characteristics of Palaeoarchaean Zircon OG1/OGC from the Owens Gully Diorite, Pilbara Craton, Western Australia, Geostand. Geoanal. Res., 41, 659, 10.1111/ggr.12182 · DOI
  58. Ketchum, 2002, Anatomy and orogenic history of a Paleoproterozoic accretionary belt: the Makkovik Province, Labrador, Canada, Can. J. Earth Sci., 39, 711, 10.1139/e01-099 · DOI
  59. Ketchum, 2000, Crustal architecture and tectonic assembly of the Central Gneiss Belt, southwestern Grenville Province, Canada: A new interpretation, Can. J. Earth Sci., 37, 217, 10.1139/e98-099 · DOI · Paper page
  60. Ketchum, 2013, Age, petrogenesis and tectonic setting of the Thessalon volcanic rocks, Huronian Supergroup, Canada, Precambr. Res., 233, 144, 10.1016/j.precamres.2013.04.009 · DOI
  61. Ketchum, 1994, 1.45 Ga granulites in the southwestern Grenville province: Geologic setting, P-T conditions, and U-Pb geochronology, Geology, 22, 215, 10.1130/0091-7613(1994)022<0215:GGITSG>2.3.CO;2 · DOI
  62. Krogh, 1994, Precise U-Pb ages for Grenvillian and pre-Grenvillian thrusting of Proterozoic and Archean metamorphic assemblages in the Grenville Front Tectonic Zone, Canada, Tectonics, 13, 963, 10.1029/94TC00801 · DOI · Paper page
  63. Krogh, 1984, Precise U-Pb zircon and baddeleyite ages for the Sudbury area, Ontario Geological Survey Special, 1, 431
  64. Long, 2004, The tectonostatigraphic evolution of the Huronian basement and the subsequent basin fill: geological constraints on impact models of the Sudbury event, Precambr. Res., 129, 203, 10.1016/j.precamres.2003.10.003 · DOI
  65. Lumbers, 1975, Geology of the Burwash area, districts of Nipissing, Parry Sound and Ontario, Ontario Division of Mines Geological Report, 116, 158
  66. Lumbers, 1991, Petrology and age of the A-type Mulock batholith, northern Grenville Province, Ontario, Precambr. Res., 53, 199, 10.1016/0301-9268(91)90072-I · DOI
  67. Mako, 2015, Polyphase Proterozoic deformation in the Four Peaks area, central Arizona, and relevance for the Mazatzal orogeny, Geosphere, 11, 1975, 10.1130/GES01196.1 · DOI
  68. Martin, 2020, The core of Rodinia formed by the juxtaposition of opposed retreating and advancing accretionary orogens, Earth Sci. Rev., 211, 10.1016/j.earscirev.2020.103413 · DOI · Paper page
  69. McEachern, 1993, Age of deformation within the Central Metasedimentary Belt boundary thrust zone, southwest Grenville orogen: Constraints on the collision of the Mid-Proterozoic Elzevir terrane, Can. J. Earth Sci., 30, 1155, 10.1139/e93-098 · DOI · Paper page
  70. Mole, 2021, The formation of Neoarchean continental crust in the south-east Superior Craton by two distinct geodynamic processes, Precambr. Res., 356, 10.1016/j.precamres.2021.106104 · DOI
  71. Mortensen, 1993, U-Pb age constraints for the magmatic and tectonic evolution of the Pontiac Subprovince, Quebec, Can. J. Earth Sci., 30, 1970, 10.1139/e93-173 · DOI
  72. Mulder, 2018, Rodinian devil in disguise: Correlation of 1.25–1.10 Ga strata between Tasmania and Grand Canyon, Geology, 46, 991, 10.1130/G45225.1 · DOI
  73. Nowell, 1998, High precision Hf isotope measurements of MORB and OIB by thermal ionisation mass spectrometry: insights into the depleted mantle, Chem. Geol., 149, 211, 10.1016/S0009-2541(98)00036-9 · DOI
  74. Papapavlou, 2021, The Pre-Grenvillian assembly of the southeastern Laurentian margin through the U-Pb–Hf detrital zircon record of Mesoproterozoic supracrustal sequences (Central Grenville Province, Quebec, Canada), Geol. Mag., 1
  75. Percival, 2007, Chapter 8.4 Eo- to Mesoarchean Terranes of the Superior Province and Their Tectonic Context, 1065, 10.1016/S0166-2635(07)15084-2 · DOI
  76. Percival, 2003, Archean adakites from the Ashuanipi complex, eastern Superior Province, Canada: geochemistry, geochronology and tectonic significance, Contrib. Miner. Petrol., 145, 265, 10.1007/s00410-003-0450-5 · DOI
  77. Prevec, 1992, U-Pb constraints on early Proterozoic mafic magmatism from the southern Superior and western Grenville provinces, Ontario. Radiogenic Age and Isotopic Studies: Report 6, Geol. Surv. Can. Pap., 92–2, 97
  78. Prevec, 1995, Sm–Nd isotopic evidence for crustal contamination in the ca. 1750 Ma Wanapitei Complex, western Grenville Province, Ontario. Canadian Journal of Earth Sciences, 32, 486, 10.1139/e95-041 · DOI
  79. Prevec, 2004, Basement tracing using Mid-Proterozoic anorthosites straddling a palaeoterrane boundary, Ontario, Canada, Precambr. Res., 129, 169, 10.1016/j.precamres.2003.10.009 · DOI
  80. Rivers, 1997, Lithotectonic elements of the Grenville Province: Review and tectonic implications, Precambr. Res., 86, 117, 10.1016/S0301-9268(97)00038-7 · DOI · Paper page
  81. Rivers, 2012, Upper-crustal orogenic lid and mid-crustal core complexes: signature of a collapsed orogenic plateau in the hinterland of the Grenville Province, Can. J. Earth Sci., 49, 1, 10.1139/e11-014 · DOI · Paper page
  82. Rivers, 2015, Tectonic setting and evolution of the Grenville Orogen: an assessment of progress over the last 40 years, Geosci. Can., 42
  83. Rivers, 2002, The high-pressure belt in the Grenville Province: Architecture, timing and exhumation models, Can. J. Earth Sci.
  84. Schellart, 2006, A Late Cretaceous and Cenozoic reconstruction of the Southwest Pacific region: Tectonics controlled by subduction and slab rollback processes, Earth Sci. Rev., 76, 191, 10.1016/j.earscirev.2006.01.002 · DOI
  85. Schulz, 2007, The Penokean orogeny in the Lake Superior region, Precambr. Res., 157, 4, 10.1016/j.precamres.2007.02.022 · DOI
  86. Shulman, 2017, Timing and anatomy of granitic strain gradients in the Grenville Front tectonic zone, Ontario, Canada, Geosphere, 13, 1949, 10.1130/GES01413.1 · DOI
  87. Skår, 2002, U-Pb geochronology and geochemistry of early Proterozoic rocks of the tectonic basement windows in central Nordland, Caledonides of north-central Norway, Precambr. Res., 116, 265, 10.1016/S0301-9268(02)00026-8 · DOI
  88. Slagstad, 2009, Western Grenville Province holds key to midcontinental Granite-Rhyolite Province enigma, Terra Nova, 21, 181, 10.1111/j.1365-3121.2009.00871.x · DOI · Paper page
  89. Slagstad, T., Culshaw, N.G., Jamieson, R.A., Ketchum, J.W.F., 2004. Early Mesoproterozoic tectonic history of the southwestern Grenville Province, Ontario: Constraints from geochemistry and geochronology of high-grade gneisses, in: Tollo, R.P., Corriveau, L., McLelland, J., Bartholomew, M.J. (Eds.), Proterozoic tectonic evolution of the Grenville orogen in North America, pp. 209-241. · DOI
  90. Söderlund, 2004, The 176Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Precambrian mafic intrusions, Earth Planet. Sci. Lett., 219, 311, 10.1016/S0012-821X(04)00012-3 · DOI
  91. Spencer, 2012, Constraining the timing and provenance of the Neoproterozoic Little Willow and Big Cottonwood Formations, Utah: Expanding the sedimentary record for early rifting of Rodinia, Precambr. Res., 204–205, 57, 10.1016/j.precamres.2012.02.009 · DOI
  92. Spencer, 2015, Generation and preservation of continental crust in the Grenville Orogeny, Geosci. Front., 6, 357, 10.1016/j.gsf.2014.12.001 · DOI
  93. Steiger, 1969, Comparative U-Th-Pb systematics in 2.7x109 yr. plutons of different geologic histories, Geochim. Cosmochim. Acta, 33, 1212, 10.1016/0016-7037(69)90043-X · DOI
  94. Thomson, 2011, Nd isotope mapping of Grenvillian crustal terranes in the vicinity of the Manicouagan Impact Structure, Precambr. Res., 191, 184, 10.1016/j.precamres.2011.08.006 · DOI
  95. Tuccillo, 1992, Thermobarometry, geochronology and the interpretation of P-T-t data in the Britt domain, Ontario, Grenville orogen, Canada, J. Petrol., 33, 1225, 10.1093/petrology/33.6.1225 · DOI · Paper page
  96. van Breemen, 1988, Northeast extension of Proterozoic terranes of mid-continental North America, Geol. Soc. Am. Bull., 100, 630, 10.1130/0016-7606(1988)100<0630:NEOPTO>2.3.CO;2 · DOI
  97. van Breemen, O., Davidson, A., Loveridge, W.D., Sullivan, R.W., 1986. U-Pb zircon geochronology of Grenville tectonites, granulites and igneous precursors, Parry Sound, Ontario, in: Moore, J.M., Davidson, A., Baer, A.J. (Eds.), The Grenville Province, pp. 192-207.
  98. Vermeesch, 2021, Maximum depositional age estimation revisited, Geosci. Front., 12, 843, 10.1016/j.gsf.2020.08.008 · DOI
  99. Whitmeyer, 2007, Tectonic model for the Proterozoic growth of North America, Geosphere, 3, 220, 10.1130/GES00055.1 · DOI
  100. Wiedenbeck, 1995, Three natural zircon standards for U-Th-Pb.Lu-Hf, trace element and REE analyses, Geostand. Newslett., 19, 1, 10.1111/j.1751-908X.1995.tb00147.x · DOI
  101. Wodicka, 1996, The Parry Sound domain: A far-travelled allochthon? New evidence from U-Pb zircon geochronology, Can. J. Earth Sci., 33, 1087, 10.1139/e96-083 · DOI · Paper page
  102. Wodicka, 2000, Grenvillian metamorphism of monocyclic rocks, Georgian Bay, Ontario, Canada: Implications for convergence history, Can. Mineral., 38, 471, 10.2113/gscanmin.38.2.471 · DOI · Paper page
  103. Wooden, J.L., Barth, A.P., Mueller, P.A., 2013. Crustal growth and tectonic evolution of the Mojave crustal province: Insights from hafnium isotope systematics in zircons. Lithosphere 5, 17-28. · DOI
  104. Woodhead, 2005, A preliminary appraisal of seven natural zircon reference materials for in situ Hf isotope determination, Geostand. Geoanal. Res., 29, 183, 10.1111/j.1751-908X.2005.tb00891.x · DOI
  105. Young, 2004, New evidence favouring an endogenic origin for supposed impact breccias in Huronian (Paleoproterozoic) sedimentary rocks, Precambr. Res., 133, 63, 10.1016/j.precamres.2004.03.013 · DOI

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Metadata

Authors
Culshaw, N., Van De Kerckhove, S., Slagstad, T., Marsh, J., & Easton, R. M.
ORCID
Slagstad, Trond
Venue
Precambrian Research
Publisher
Elsevier BV
Published
2023-03
Volume
386
Pages
106963
ISSN
0301-9268
DOI
10.1016/j.precamres.2023.106963
Cited by
16
References
1
Language
en
Licence

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

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