Diamonds in the Attawapiskat area of the Superior craton (Canada): Evidence for a major diamond-forming event younger than 1.1 Ga

Contributions to Mineralogy and Petrology

Volumn 167, Issue 1, 2014, Pages 1-16

  Smit, K V ^a   Stachel, T ^a   Stern, R A ^a  

^a UNIVERSITY OF ALBERTA   (Canada)

Author keywords

Attawapiskat; Diamond; Lithospheric mantle; Nitrogen aggregation; Superior

Indexed keywords

AGGREGATION; CARBON ISOTOPE; CRATON; DIAMOND; ISOTOPIC COMPOSITION; KIMBERLITE; LITHOSPHERIC STRUCTURE; MANTLE STRUCTURE; NITROGEN;

ARIZONA; ATTAWAPISKAT; CANADA; MIDCONTINENT RIFT; ONTARIO [CANADA]; SUPERIOR; UNITED STATES;

EID: 84891789099     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-013-0962-6     Document Type: Article

References (109)

1. Armstrong JP, Fitzgerald CE, Kjarsgaard BA, Heaman L, Tappe S (2012) Kimberlites of the Coronation Gulf Field, Northern Slave Craton, Nunavut Canada. In: 10th International Kimberlite Conference Extended Abstracts, vol 170.
2. Beakhouse GP (1991) Winnipeg River subprovince. In: Thurston PC, Williams HR, Sutcliffe RH, Stott GM (eds) Geology of Ontario, special volume 4, part 1, pp 279-301. Ontario Geological Survey.
3. Bell K, Blenkinsop J (1987) Nd and Sr isotopic compositions of East African carbonatites: implications for mantle heterogeneity. Geology 15(2): 99-102.
4. Berman RG, Sanborn-Barrie M, Stern RA, Carson CJ (2005) Tectonometamorphism at ca. 2. 35 and 1. 85 Ga in the Rae Domain, Western Churchill Province, Nunavut, Canada: insights from structural, metamorphic and in situ geochronological analysis of the Southwestern Committee Bay Belt. Can Mineral 43: 409-442.
5. Blank JG, Delaney JR, Des Marais DJ (1993) The concentration and isotopic composition of carbon in basaltic glasses from the Juan de Fuca Ridge, Pacific Ocean. Geochim Cosmochim Acta 57: 875.
6. Böhm CO, Heaman LM, Creaser RA, Crockery MT (2000) Discovery of pre-3. 5 Ga exotic crust at the northwestern Superior Province margin, Manitoba. Geology 28(1): 75-78.
7. Boyd SR, Mattey DP, Pillinger CI, Milledge HJ, Mendelssohn M, Seal M (1987) Multiple growth events during diamond genesis: an integrated study of carbon and nitrogen isotopes and nitrogen aggregation state in coated stones. Earth Planet Sci Lett 86: 341-353.
8. Boyd SR, Kiflawi I, Woods GS (1994) The relationship between infrared absorption and the A defect concentration in diamond. Philos Mag B 69(6): 1149-1153.
9. Boyd SR, Kiflawi I, Woods GS (1995) Infrared absorption by the B nitrogen aggregate in diamond. Philos Mag B 72(3): 351-361.
10. Brey GP, Bulatov VK, Girnis AV, Lahaye Y (2008) Experimental melting of carbonated peridotite at 6-10 GPa. J Petrol 49(4): 797-821.
11. Bursill LA, Glaisher RW (1985) Aggregation and dissolution of small and extended defect structures in Type Ia diamond. Am Mineral 70(5-6): 608-618.
12. Cartigny P (2005) Stable isotopes and the origin of diamond. Elements 1: 79-84.
13. 13C-N concentrations in diamonds. Earth Planet Sci Lett 185: 85-98.
14. Coggon RM, Teagle DAH, Cooper MJ, Hayes TEF, Green DRH (2006) Data report: compositions of calcium carbonate veins from superfast spreading rate crust, ODP Leg 206. Proc ODP Sci Results 206: 1-6.
15. Corfu F, Wood J (1986) U-Pb zircon ages in supracrustal and plutonic rocks; North Spirit Lake area, northwestern Ontario. Can J Earth Sci 23: 967-977.
16. David J, Parent M, Stevenson R, Nadeau P, Godin L (2002) The Porpoise Cove supracrustal sequence, Inukjuak area: a unique example of Paleoarchean crust (ca. 3. 8 Ga) in the Superior Province. Ministère des Resources Naturelles de Québec, DV, 2002-10.
17. Day HW (2012) A revised diamond-graphite transition curve. Am Mineral 97: 52-62.
18. de Stefano A, Kopylova MG, Cartigny P, Afanasiev V (2009) Diamonds and eclogites of the Jericho kimberlite (Northern Canada). Contrib Miner Petrol 158(3): 295-315.
19. Deines P (1980) The carbon isotopic composition of diamonds: relationship to diamond shape, colour, occurrence and vapour deposition. Geochim Cosmochim Acta 44: 943-961.
20. Deines P, Gold DP (1973) The isotopic composition of carbonatite and kimberlite carbonate and their bearing on the isotopic composition of deep-seated carbon. Geochim Cosmochim Acta 37: 1709-1733.
21. 13C content of Finsch and Premier diamonds and their implications. Geochim Cosmochim Acta 53: 1367-1378.
22. Deines P, Viljoen F, Harris JW (2001) Implications of the carbon isotope and mineral inclusion record for the formation of diamonds in the mantle underlying a mobile belt: Venetia, South Africa. Geochim Cosmochim Acta 65: 813-838.
23. Des Marais DJ, Moore JG (1984) Carbon and its isotopes in mid-oceanic basaltic glasses. Earth and Planetary Science Letters 62: 43-57.
24. Doig R (1970) An alkaline rock province linking Europe and North America. Can J Earth Sci 7(1): 22-26.
25. Eaton DW, Darbyshire F (2010) Lithospheric architecture and tectonic evolution of the Hudson Bay region. Tectonophysics 480: 1-22.
26. 2 system. Am J Sci 278: 305-343.
27. Evans T, Qi Z (1982) The kinetics of aggregation of nitrogen in diamond. Proc R Soc Lond Ser A 361: 109-127.
28. Evans T, Kiflawi I, Luyten W, van Tendeloo G, Woods GS (1995) Conversion of platelets into dislocation loops and voidite formation in Type IaB diamonds. Proc R Soc Lond Ser A 449: 295-313.
29. Exley RA, Mattey DP, Clague DA, Pillinger CT (1986) Carbon isotope systematics of a mantle "hot spot": a comparison of Loihi Seamount and MORB glasses. Earth Planet Sci Lett 78: 189-199.
30. Graham S, Lambert DD, Shee SR, Smith CB, Reeves S (1999) Re-Os isotopic evidence for Archean lithospheric mantle beneath the Kimberley block, Western Australia. Geology 27(5): 431-434.
31. Grütter HS (2009) Pyroxene xenocryst geotherms: techniques and application. Lithos 112S: 1167-1178.
32. Haggerty SE (1999) A diamond trilogy: superplumes, supercontinents, and supernovae. Science 285: 851-860.
33. Halls HC (1978) The late Precambrian Central North American Rift System-a survey of recent geological and geophysical investigations. In: Ramberg IB, Neumann ER (eds) Tectonics and geophysics of continental rifts. Reidel, Dordrecht, pp 111-123.
34. Harte B, Fitzsimons ICW, Harris JW, Otter ML (1999) Carbon isotope ratios and nitrogen abundances in relation to cathodoluminescence characteristics for some diamonds from the Kaapvaal Province, S. Africa. Mineral Mag 63(6): 829-856.
35. Hasterok D, Chapman DS (2011) Heat production and geotherms for the continental lithosphere. Earth Planet Sci Lett 307: 59-70.
36. Hattori K, Hamilton S (2008) Geochemistry of peat over kimberlites in the Attawapiskat area, James Bay Lowlands, northern Canada. Appl Geochem 23: 3767-3782.
37. Heaman LM, Kjarsgaard BA (2000) Timing of eastern North American kimberlite magmatism: continental extension of the Great Meteor hotspot track? Earth Planet Sci Lett 178: 253-268.
38. Heaman LM, Kjarsgaard BA, Creaser RA (2004) The temporal evolution of North American kimberlites. Lithos 76: 377-397.
39. Hoefs J, Frey M (1976) The isotopic composition of carbonaceous matter in a metamorphic profile from the Swiss Alps. Geochim Cosmochim Acta 40: 945.
40. Howell D, O'Neill CJ, Grant KJ, Griffin WL, O'Reilly SY, Pearson NJ, Stern RA, Stachel T (2012) Platelet development in cuboid diamonds: insights from micro-FTIR mapping. Contrib Miner Petrol 164: 1011-1025.
41. Huizenga JM, Crossingham A, Viljoen F (2012) Diamond precipitation from ascending reduced fluids in the Kaapvaal lithosphere: thermodynamic constraints. CR Geosci 344: 67-76.
42. Humble P (1982) The structure and mechanism of formation of platelets in natural type Ia diamond. Proc R Soc Lond Ser A 381: 65-81.
43. Hunt LC, Stachel T, McCandless TE, Armstrong J, Muehlenbachs K (2012) Diamonds and their mineral inclusions from the Renard kimberlites in Quebec. Lithos 142-143: 267-284.
44. Januszczak N, Seller MH, Kurszlaukis S, Murphy C, Delgaty J, Tappe S, Ali K, Zhu J, Ellemers P (2013) A multidisciplinary approach to the Attawapiskat kimberlite field, Canada: accelerating the discovery-to-production pipeline. In: Proceedings of the 10th International Kimberlite Conference.
45. Javoy M, Pineau F, Delorme H (1986) Carbon and nitrogen isotopes in the mantle. Chem Geol 57(1-2): 41-62.
46. Kiflawi I, Bruley J (2000) The nitrogen aggregation sequence and the formation of voidites in diamond. Diam Relat Mater 9: 87-93.
47. Kirkley MB, Gurney JJ, Otter ML, Hill SJ, Daniels LR (1991) The application of C isotope measurements to the identification of the sources of C in diamonds: a review. Appl Geochem 6: 477-494.
48. Klewin KW, Berg JH (1991) Geochemistry of the Mamainse Point volcanics, Ontario: petrogenesis and continental rift evolution. J Geophys Res 96: 457-474.
49. Kong JM., Boucher DR, Scott-Smith BH (1999) Exploration and geology of the Attawapiskat kimberlites, James Bay Lowlands, Northern Ontario, Canada. In: Extended abstracts of the 7th International Kimberlite Conference, pp 446-448.
50. 2 pressures on alkalic rock and its bearing on the formation of alkalic ultrabasic rocks and the associated carbonatites. Am J Sci 275: 163-185.
51. Langford FF, Morin JA (1976) The development of the Superior Province of Northwestern Ontario by merging Island Arcs. Am J Sci 270: 1023-1034.
52. Leahy K, Taylor WR (1997) The influence of the Glennie domain deep structure on the diamonds in Saskatchewan kimberlites. Russ Geol Geophys 38(2): 481-491.
53. LeCheminant AN, Heaman LM (1989) Mackenzie igneous events, Canada: Middle Proterozoic hotspot magmatism associated with ocean opening. Earth Planet Sci Lett 96: 38-48.
54. Luguet A, Jaques AL, Pearson DG, Smith CB, Bulanova GP, Roffey SL, Rayner MJ, Lorand J-P (2009) An integrated petrological, geochemical and Re-Os isotope study of peridotite xenoliths from the Argyle lamproite, Western Australia and implications for cratonic diamond occurrences. In: Lithos, 112S-proceedings of the 9th International Kimberlite Conference, pp 1096-1108.
55. Marty B, Zimmermann L (1999) Volatiles (He, C, N, Ar) in mid-ocean ridge basalts: assessment of shallow-level fractionation and characterization of source composition. Geochim Cosmochim Acta 63(21): 3619-3633.
56. Mather KA, Pearson DG, McKenzie D, Kjarsgaard BA, Priestley K (2011) Constraints on the depth and thermal history of cratonic lithosphere from peridotite xenoliths, xenocrysts and seismology. Lithos 125: 729-742.
57. Mattey DP, Carr RH, Wright IP, Pillinger CT (1984) Carbon isotopes in submarine basalts. Earth Planet Sci Lett 70: 196-206.
58. McCandless TE, Gurney JJ (1997) Diamond eclogites: comparison with carbonaceous chondrites, carbonaecous shales, and microbial carbon-enriched MORB. Russian geology and geophysics, special issue: proceedings of the 6th International Kimberlite Conference, vol 2, pp 394-404.
59. Miller CE, Kopylova MG, Ryder J (2012) Vanished diamondiferous cratonic root beneath the Southern Superior province: evidence from diamond inclusions in the Wawa metaconglomerate. Contrib Miner Petrol 164(4): 697-714.
60. Nickel KG, Green DH (1985) Empirical geothermobarometry for garnet peridotites and implications for the nature of the lithosphere, kimberlites and diamonds. Earth Planet Sci Lett 73: 158-170.
61. Nimis P, Grütter H (2009) Internally consistent geothermometers for garnet peridotites and pyroxenites. Contrib Miner Petrol 159(3): 411-427.
62. Nimis P, Taylor WR (2000) Single clinopyroxene thermobarometry for garnet peridotites. Part I. Calibration and testing of a Cr-in-Cpx barometer and an enstatite-in-Cpx thermometer. Contrib Miner Petrol 139: 541-554.
63. Nisbet EG, Mattey DP, Lowry D (1994) Can diamonds be dead bacteria? Nature 367: 694.
64. Ojakangas RW, Morey GB, Green JC (2001) The Mesoproterozoic Midcontinent Rift system, Lake Superior Region, USA. Sed Geol 141-142: 421-442.
65. Paces JB, Bell K (1989) Non-depleted sub-continental mantle beneath the Superior Province of the Canadian Shield: Nd-Sr isotopic and trace element evidence from Midcontinent Rift basalts. Geochim Cosmochim Acta 53: 2023-2035.
66. Palot M, Pearson DG, Stern RA, Stachel T, Harris JW (2013) Multiple growth events, processes and fluid sources involved in diamond genesis: a micro-analytical study of sulphide-bearing diamonds from the Finsch mine, RSA. Geochim Cosmochim Acta 106: 51-70.
67. Pearson DG, Meyer HOA, Boyd FR, Shirey SB, Carlson RW (1997) Re-Os isotope evidence for late Archaean stabilisation of a thick lithospheric mantle keel beneath the Kirkland Lake area, Superior Province, Canada. Further evidence for long-term crust-mantle coupling. Russian geology and geophysics, special issue: proceedings of the 6th International Kimberlite Conference, vol 2, pp 427-429.
68. Pearson DG, Shirey SB, Harris JW, Carlson RW (1998) Sulphide inclusions in diamonds from the Koffiefontein kimberlite, S Africa: constraints on diamond ages and mantle Re-Os systematics. Earth Planet Sci Lett 160: 311-326.
69. Percival JA, Sanborn-Barrie M, Skulski T, Stott GM, Helmstaedt H, White DJ (2006) Tectonic evolution of the western Superior Province from NATMAP and Lithoprobe studies. Can J Earth Sci 43: 1085-1117.
70. Pineau F, Javoy M, Allègre CJ (1973) Etude systématique des isotopes de l'oxygène, du carbone et du strontium dans les carbonatites. Geochim Cosmochim Acta 37: 2363-2377.
71. Richardson SH (1986) Latter-day origin of diamonds of eclogitic paragenesis. Nature 322: 623-626.
72. Richardson SH, Harris JW, Gurney JJ (1993) Three generations of diamond from old continental mantle. Nature 366: 256-258.
73. Richardson SH, Pöml PF, Shirey SB, Harris JW (2009) Age and origin of peridotitic diamonds from Venetia, Limpopo Belt, Kaapvaal-Zimbabwe Craton. In: Lithos, 112S-proceedings of the 9th International Kimberlite Conference, pp 785-792.
74. Rukhlov AS, Bell K (2010) Geochronology of carbonatites from the Canadian and Baltic Shields, and the Canadian Cordillera: clues to mantle evolution. Mineral Petrol 98(1-4): 11-54.
75. Sage RP (2000) Kimberlites of the Attawapiskat area, James Bay Lowlands, northern Ontario. Ont Geol Surv Open File Rep 6019(341): 341.
76. Schaeffer AJ, Lebedev S (2013) Global shear speed structure of the upper mantle. Geophys J Int 194(1): 417-449.
77. Schidlowski M (2001) Carbon isotopes as biogeochemical recorders of life over 3. 8 Ga of Earth history: evolution of a concept. Precambr Res 106: 117-134.
78. Sheppard SMF, Dawson JB (1975) Hydrogen, carbon and oxygen isotope studies of megacryst and matrix minerals from Lesothan and South African kimberlites. In: Ahrens L, Urey HC, Runcorn SK (eds) Physics and chemistry of the Earth, vol 6. Pergamon Press, Oxford, pp 747-763.
79. Shirey SB, Richardson SH (2011) Start of the Wilson cycle at 3 Ga shown by diamonds from subcontinental mantle. Science 333: 434-436.
80. Shirey SB, Klewin KW, Berg JH, Carlson RW (1994) Temporal changes in the sources of flood basalts: isotopic and trace element evidence from the 1100 Ma old Keweenawan Mamainse Point Formation, Ontario, Canada. Geochim Cosmochim Acta 58(20): 4475-4490.
81. Skulski T, Corkery MT, Stone D, Whalen JB, Stern RA (2000) Geological and geochronological investigations in the Stull Lake-Edmund Lake greenstone belt and granitoid rocks of the northwestern Superior Province. Report of activities 2000, Manitoba Industry, Trade and Mines, pp 117-128. Manitoba Geological Survey.
82. 13C-N study of eclogite-hosted diamonds from the Jericho kimberlite. Geochim Cosmochim Acta 75: 6027-6047.
83. Smit KV, Shirey SB, Richardson SH, le Roex AP, Gurney JJ (2010) Re-Os isotopic composition of peridotitic sulphide inclusions in diamonds from Ellendale, Australia: age constraints on Kimberley cratonic lithosphere. Geochim Cosmochim Acta 74(11): 3292-3306.
84. Smit KV, Pearson GP, Stachel T, Seller M. Peridotite xenoliths from Attawapiskat, Canada: Mesoproterozoic reworking of Palaeoarchaean lithospheric mantle beneath the Northern Superior Superterrane (in preparation).
85. Snyder GA, Taylor LA, Jerde EA, Clayton RN, Mayeda TK, Deines P, Rossman GR, Sobolev NV (1995) Archean mantle heterogeneity and origin of diamondiferous eclogites, Siberia: evidence from stable isotopes and hydroxyl in garnet. Am Mineral 80: 799.
86. Sobolev VS, Sobolev NV (1980) New proof on very deep subsidence of eclogitised crustal rocks. Dokl Akad Nauk SSSR 250: 683-685.
87. Sobolev VN, Taylor LA, Snyder GA (1994) Diamondiferous eclogites from the Udachnaya kimberlite pipe, Yakutia. Int Geol Rev 36: 42.
88. Stachel T, Harris JW (2008) The origin of cratonic diamonds-constraints from mineral inclusions. Ore Geol Rev 34(1-2): 5-32.
89. Stachel T, Aulbach S, Brey GP, Harris JW, Leost I, Tappert R, Viljoen KS (2004) The trace element composition of silicate inclusions in diamonds: a review. Lithos 77: 1-20.
90. Stachel T, Banas A, Muehlenbachs K, Kurszlaukis S, Walker EC (2006) Archean diamonds from Wawa (Canada): samples from deep cratonic roots predating cratonization of the Superior Province. Contrib Miner Petrol 151: 737-750.
91. Stachel T, Harris JW, Muehlenbachs K (2009) Sources of carbon in inclusion-bearing diamonds. In: Lithos, 112S-proceedings of the 9th International Kimberlite Conference, pp 625-637.
92. Stevenson RK (1995) Crust and mantle evolution in the late Archaean: evidence from a Sm-Nd isotopic study of the North Spirit Lake greenstone belt, northwestern Ontario. Geol Soc Am Bull 107: 1458-1467.
93. Strauss H (1986) Carbon and sulphur isotopes in Precambrian sediments from the Canadian Shield. Geochim Cosmochim Acta 50: 2653-2662.
94. Taylor WR (1998) An experimental test of some geothermometer and geobarometer formulations for upper mantle peridotites with application to the thermobarometry of fertile lherzolite and garnet websterite. Neues Jahrbuch Mineralogie Abhandlungen 172: 381-408.
95. Taylor WR, Jaques AL, Ridd M (1990) Nitrogen-defect aggregation characteristics of some Australasian diamonds: time-temperature constraints on the source regions of pipe and alluvial diamonds. Am Mineral 75: 1290-1310.
96. Thomas RD (2004) Spider #1 and #3 projects (James Bay Joint Venture), James Bay, Ontario. Technical report prepared for Spider Resources and KWG Resources, p 76.
97. Thomassot E, Cartigny P, Harris JW, Viljoen KS (2007) Methane-related diamond crystallisation in the Earth's mantle: stable isotope evidences from a single diamond-bearing xenolith. Earth Planet Sci Lett 257: 362-371.
98. Thurston PC, Osmani IA, Stone D (1991) Northwestern Superior Province: review and terrane analysis. In: Thurston PC, Williams HR, Sutcliffe RH, Stott GM (eds) Geology of Ontario, special volume 4, part 1, pp 81-144. Ontario Geological Survey.
99. Tomlinson KY, Stott GM, Percival JA, Stone D (2004) Basement terrane correlations and crustal recycling in the western Superior Province: Nd isotopic character of granitoid and felsic volcanic rocks in the Wabigoon subprovince, N. Ontario, Canada. Precambr Res 132: 245-274.
100. Tyler I, Page R (1996) Palaeoproterozoic deformation, metamorphism and igneous intrusion in the central zone of the Lamboo Complex, Halls Creek Orogen. Geol Soc Aust Abstr 41: 450.
101. van Schmus WR, Hinze WJ (1985) The Midcontinent Rift system. Annu Rev Earth Planet Sci 13: 345-383.
102. Webb KJ, Smith BHS, Paul JL, Hetman CM (2004) Geology of the Victor Kimberlite, Attawapiskat, Northern Ontario, Canada: cross-cutting and nested craters. Lithos 76: 29-50.
103. 2 as a function of degree of partial melting at 15 and 30 kbar. Am Mineral 65: 37-44.
104. Westerlund K, Shirey S, Richardson S, Carlson R, Gurney J, Harris J (2006) A subduction wedge origin for Paleoarchean peridotitic diamonds and harzburgites from the Panda kimberlite, Slave craton: evidence from Re-Os isotope systematics. Contrib Miner Petrol 152: 275-294.
105. White WS (1972) Keweenawan flood basalts and continental rifting. Geol Assoc Am Abstr Programs 4: 732-734.
106. Wiggers de Vries DF, Bulanova GP, de Corte K, Pearson DG, Craven JA, Davies GR (2013) Micron-scale couple carbon isotope and nitrogen abundance variations in diamonds: evidence for episodic diamond formation beneath the Siberian Craton. Geochim Cosmochim Acta 100: 176-199.
107. Wold RJ, Hinze WJ (1982) Geology and tectonics of the Lake Superior basin. Geol Assoc Am Mem 156: 280.
108. Woods G (1986) Platelets and the infrared absorption of type Ia diamonds. Proc R Soc A407: 219-238.
109. 2 at mantle pressures with geophysical and petrological applications. Contrib Miner Petrol 54: 79-107.