Spatial distribution and compositional variation of APS minerals related to uranium deposits in the Kiggavik-Andrew Lake structural trend, Nunavut, Canada
详细信息    查看全文
  • 作者:Thomas Riegler ; Dave Quirt ; Daniel Beaufort
  • 关键词:APS minerals ; Thelon ; Hydrothermal alteration ; Paleo ; laterite
  • 刊名:Mineralium Deposita
  • 出版年:2016
  • 出版时间:February 2016
  • 年:2016
  • 卷:51
  • 期:2
  • 页码:219-236
  • 全文大小:2,767 KB
  • 参考文献:Aoki M, Comsti EC, Lazo FB (1993) Advanced argillic alteration and geochemistry of alunite in an evolving hydrothermal system at Baguio, Northern Luzon, Philippines. Resource Geol 43:155–164
    Beaufort D, Patrier P, Laverret E, Bruneton P, Mondy J (2005) Clay alteration associated with Proterozoic unconformity-type uranium deposits in the East Alligator Rivers Uranium Field, Northern Territory, Australia. Econ Geol 100:515–536CrossRef
    Braun J-J, Pagel M, Muller J-P, Bilong P, Michard A, Guillet B (1990) Cerium anomalies in lateritic profiles. Geochim Cosmichim Acta 54:781–795CrossRef
    Carignan J, Hild P, Mevelle G, Morel J, Yeghicheyan D (2001) Routine analyses of trace elements in geological samples using flow injection and low pressure on-line liquid chromatography coupled to ICP-MS: a study of geochemical reference materials BR, DR-N, UB-N, AN-G and GH. Geostand Geoanal Res 25:187–198CrossRef
    Cloutier J, Kyser K, Olivo GR, Alexandre P (2010) Contrasting patterns of alteration at the Wheeler River area, Athabasca Basin, Saskatchewan, Canada: insights into the apparently uranium-barren zone K alteration system. Econ Geol 105:303–324CrossRef
    Cuney M, Mathieu R (2000) Extreme light rare earth element mobilization by diagenetic fluids in the geological environment of the Oklo natural reactor zones, Franceville basin, Gabon. Geology 28:743–746CrossRef
    Cuney M (2005) World-class unconformity uranium deposits: key factors for their genesis In: Mao J, Bierlein FP (eds) 8th Biennal SGA Meeting. Beijing, China, pp 245-246
    Davis WJ, Zaleski E (1998) Geochronological investigations of the Woodburn Lake group, western Churchill Province: preliminary results Current Research 1998-F. Geological Survey of Canada, pp 89-97
    Derome D, Cathelineau M, Cuney M, Fabre C, Lhomme T, Banks DA (2005) Mixing of sodic and calcic brines and uranium deposition at McArthur River, Saskatchewan, Canada: a Raman and laser-induced breakdown spectroscopic study of fluid Inclusions. Econ Geol 100:1529–1545CrossRef
    Dill HG (2001) The geology of aluminium phosphates and sulphates of the alunite group minerals: a review. Earth Sci Rev 53:35–93CrossRef
    Fayek M, Kyser K (1997) Characterization of multiple fluid events and rare-earth-element mobility associated with formation of unconformity-type uranium deposits in the Athabasca Basin, Saskatchewan. Can Mineralog 35:627–658
    Gaboreau S, Beaufort D, Vieillard P, Patrier P, Bruneton P (2005) Aluminum phosphate-sulfate minerals associated with Proterozoic unconformity-type uranium deposits in the East Alligator River uranium field, Northern Territories, Australia. Can Mineralog 43:813–827CrossRef
    Gaboreau S, Cuney M, Quirt D, Beaufort D, Patrier P, Mathieu R (2007) Significance of aluminum phosphate-sulfate minerals associated with U unconformity-type deposits: the Athabasca basin, Canada. Am Mineralog 92:267–280CrossRef
    Gall Q, Peterson T, Donaldson JA (1992) A proposed revision of Early Proterozoic stratigraphy of the Thelon and Baker Lake basins, Northwest Territories In: GSC (ed) Current research, part c. Geological Survey of Canada, pp 129-137
    Gall Q, Donaldson JA (2006) Diagenetic fluorapatite and aluminum phosphate-sulphate in the Paleoproterozoic Thelon Formation and Hornby Bay Group, northwestern Canadian Shield. Can J Earth Sci 43:617–629CrossRef
    Hartlaub RP, Heaman LM, Ashton KE, Chacko T (2004) The Archean Murmac Bay Group: evidence for a giant Archean rift in the Rae Province, Canada. Precambrian Res 131:345–372CrossRef
    Hasegawa K, Davidson GI, Wollenberg P, Yoshimasa I (1990) Geophysical exploration for unconformity-related uranium deposits in the northeastern part of the Thelon Basin, Northwest Territories, Canada. Mining Geol 40:83–95
    Hedenquist JW, Matsuhisa Y, Izawa E, White NC, Giggenbach WF, Aoki M (1994) Geology, geochemistry, and origin of high sulfidation Cu-Au mineralization in the Nansatsu District, Japan. Econ Geol 89:1–30CrossRef
    Herold H (1987) Zur Kristallchemie und Thermodynamik der Phosphate und Arsenate vom Crandallit-Typ. Erlangen University, pp 109 pp
    Hoffman PF (1990) Subdivision of the Churchill Province and extent of the Trans-Hudson orogen In: Lewry JF, Stauffer MR (eds) The Early Proterozoic Trans-Hudson Orogen of North America. Geological Survey of Canada Special Paper, pp 15-39
    Jefferson CW, Thomas DJ, Gandhi SS, Ramaekers P, Delaney G, Brisbin D, Cutts C, Portella P, Olson RA (2007) Unconformity-associated uranium deposits of the Athabasca Basin, Saskatchewan and Alberta EXTECH IV. pp 23-67
    Jefferson CW, Pehrsson S, Peterson T, Chorlton L, Davis DW, Keating P, Gandhi SS, Fortin R, Buckle JL, Miles W, Rainbird RH, LeCheminant AN, Tschirhart V, Tschirhart P, Morris W, Scott J, Cousens B, McEwan B, Bethune K, Riemer W, Calhoun L, White J, MacIssac D, Leblon B, Lentz D, laRocque A, Shelat Y, Patterson J, Enright A, Stieber C, Riegler T (2011) Northeast Thelon region geoscience framework—new maps and data for uranium in Nunavut In: Canada NR (ed). Geological Survey of Canada
    Jefferson CW, Pehrsson S, Peterson T, Tschirhart V, Anand A, Wollenberg P, Riegler T, Bethune K, Chorlton L, McEwan B, LeCheminant AN, Tschirhart P, Scott J, Davis DW, McNicoll VJ, Riemer W, White J, Patterson J, Morris CL, Keating P, Stieber C (2014) Bedrock geology of the western Marjorie-Tehek supracrustal belt and Aberdeen Sub-basin margin in parts of NTS 66A and 66B, Nunavut-context of the Kiggavik uranium camp Open File7241. Geological Survey of Canada
    Kolitsch U, Ping A (2001) Crystal chemistry of the crandallite, beudantite and alunite groups: a review and evaluation of the suitability as storage materials for toxic metals. J Miner Petrol Sci:67-78
    Kotzer TG, Kyser TK (1995) Petrogenesis of the Proterozoic Athabasca Basin, northern Saskatchewan, Canada, and its relation to diagenesis, hydrothermal uranium mineralization and paleohydrogeology. Chem Geol 120:45–89CrossRef
    Kyser K, Hiatt EE, Renac C, Durocher K, Holk G, Deckart K (2000) Diagenetic fluids in Paleo and Meso-proterozoic sedimentary basins and their implications for long protracted fluid histories In: Kyser K (ed) Fluids and basin evolution. Mineralogical Association of Canada, pp 225-258
    Laverret E, Patrier P, Beaufort D, Kister P, Quirt D, Bruneton P, Clauer N (2006) Mineralogy and geochemistry of the host-rock alterations associated with the Shea Creek unconformity-type uranium deposits (Athabasca basin, Saskatchewan, Canada) Part 1. Spatial variation of illite properties. Clay Clay Miner 54:275–294CrossRef
    LeCheminant AN, Leatherbarrow RW, Miller AR (1979) Thirty Mile Lake (65P, W1/2) map area, District of Keewatin. Current Research GSC Part B:319-327
    MacDonald R (1980) Mineralogy and geochemistry of a Precambrian regolith in the Athabasca Basin. University of Saskatchewan, Saskatoon, p 151
    Mercadier J, Lach P, Brouand M (2010) Note concernant les premiers résultatsd‛Ablation Laser ICP-MS obtenus sur les oxydes d‛uranium de l‛échantillon 9809 du gisement de Kiggavik(Canada): implications sur le mode deformation des minéralisations. CREGU
    Miller AR (1983) A progress report: uranium phosphorus association in the Helikian Thelon Formation and sub-Thelon saprolite, central district of Keewatin, NWT. Current Research GSC 83-1A:449-456
    Miller AR, LeCheminant AN (1985) Geology and uranium metallogeny of Proterozoic supracrustal successions, central District of Keewatin, N.W.T with comparisons to northern Saskatchewan Geology of uranium deposits. Canadian Institute of Mining and Metalurgy, pp 167-185
    Miller AR, Cumming GL, Krstic D (1989) U-Pb, Pb-Pb, and K-Ar isotopic study and petrography of uraniferous phosphate-bearing rocks in the Thelon Formation, Dubawnt Group, Northwest Territories, Canada. Can J Earth Sci 26:867–880CrossRef
    Pagel M (1975) Détermination des conditions physico-chimique de la silicification diagénétique des grès Athabasca (Canada) au moyen des inclusions fluides. CR Acad Sci Paris 280:2301–2304
    Pagel M, Jaffrezic H (1977) Analyses chimiques des saumures des inclusionsdu quartz et de la dolomite du gisement d’uranium de Rabbit Lake(Canada). Aspect méthodologique et importance génétique. CR Acad Sci Paris 284:113–116
    Pehrsson S, Jefferson CW, Peterson TD, Scott J, Chorlton L, Hillary B, Patterson J, Lentz D, Shelat Y, Bethune K (2010) Basement to the Thelon Basin, Nunavut- Revisited Geo Canada 2010. Calgary
    Percival JB, Kodama H (1989) Sudoite from Cigar Lake, Saskatchewan. Can Mineralog 27:633–641
    Peterson TD, Van Breemen O, Sandeman H, Cousens B (2002) Proterozoic (1.85-1.75 Ga) igneous suites of the Western Churchill Province: granitoid and ultrapotassic magmatism in a reworked Archean hinterland. Precambrian Res 119:73–100CrossRef
    Rainbird RH, Hadlari T (2000) Revised stratigraphy and sedimentology of the Paleoproterozoic Dubawnt Supergroup and the Northern Margin of Baker Lake Basin, Nuanvut Current Research. Geological Survey of Canada, pp 9
    Rainbird RH, Hadlari T, Aspler LB, Donaldson JA, LeCheminant AN, Peterson TD (2003) Sequence stratigraphy and evolution of the Paleoproterozoic intracontinental Baker Lake and Thelon basins, western Churchill Province, Nunavut, Canada. Precambrian Res 125:21–53CrossRef
    Ramaekers P (1980) Stratigraphy and tectonic history of the Athabasca Group (Helikian) of Northern Saskatchewan Summary of investigations 80-4. Saskatchewan Geological Survey, pp 99-106
    Ramaekers P (1981) Hudsonian and Helikian Basins of the Athabasca Region, northern Saskatchewan Proterozoic Basins of Canada; Geological Survey of Canada, Paper 81-10. Geological Survey of Canada, pp 233
    Rasmussen B (1996) Early-diagenetic REE-phosphate minerals (florencite, gorceixite, crandallite, and xenotime) in marine sandstones; a major sink for oceanic phosphorus. Am J Sci 296:601–632. doi:10.​2475/​ajs.​296.​6.​601 CrossRef
    Riegler T, Wollenberg P, Lescuyer J-L, Quirt D, Beaufort D (2014) Alteration related to uranium deposits in the Kiggavik-Andrew Lake structural trend, Nunavut, Canada: new insights from petrography and clay mineralogy. Can Mineralog 52:27–45CrossRef
    Schau M (1983) Baker Lake map sheet (56D) Open File 883. Geological Survey of Canada
    Seghal J (1998) Red and lateritic soils. Rotterdam
    Sehnke E (1993) Refractory-grade bauxite: an overview Unitecr’93 Congress Refractories for the New World Economy. Sao Paulo pp 658-670
    Stoffregen RE, Alpers CN (1987) Woodhouseite and svanbergite in hydrothermal ore deposits: products of apatite destruction during advanced argilic alteration. Can Mineralog 25:201–211
    Stoffregen RE (1993) Stability relations of jarosite and natroalunite at 100–250°C. Geochim Cosmichim Acta 58:903–916CrossRef
    Wilson JA (1985a) Crandallite group minerals in the Helikian Athabasca Group in Alberta, Canada. Can J Earth Sci 22:637–641. doi:10.​1139/​e85-065 CrossRef
    Wilson JA (1985b) Geology of the Athabasca Group in Alberta. Alberta Geology Survey
    Zaleski E, Duke N, L’Heureux R, Davis WJ, Wilkinson L (1999) Clastic and chemical sedimentary sequences, Woodburn Lake group, Amarulik Lake to Tehek Lake, western Churchill Province, Northwest Territories (Nunavut) In: Canada GSo (ed) Canadian Shield current research Natural Resources Canada, pp 19-28
  • 作者单位:Thomas Riegler (1)
    Dave Quirt (2)
    Daniel Beaufort (1)

    1. Laboratoire IC2MP, CNRS-UMR 7285, Université de Poitiers, Bâtiment B35, 4 Rue Michel Brunet, TSA 51106, 86079, Poitiers Cedex, France
    2. AREVA Resources Canada Inc., P.O. Box 9204, Saskatoon, SK, S7K 3X5, Canada
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geology
    Mineral Resources
    Mineralogy
  • 出版者:Springer Berlin / Heidelberg
  • ISSN:1432-1866
文摘
The Kiggavik-Andrew Lake structural trend consists of four mineralized zones, partially outcropping, lying 2 km south of the erosional contact with the unmetamorphosed sandstone and basal conglomerates of the Paleoproterozoic Thelon Formation. The mineralization is controlled by a major E-W fault system associated with illite and sudoite alteration halos developed in the Archean metagraywackes of the Woodburn Lake Group. Aluminum phosphate sulfate (APS) minerals from the alunite group crystallized in association with the clay minerals in the basement alteration halo as well as in the overlying sandstones, which underwent mostly diagenesis. APS minerals are Sr- and S-rich (svanbergite end-member) in the sedimentary cover overlying the unconformity, whereas they are light rare earth elements (LREE)-rich (florencite end-member) in the altered basement rocks below the unconformity. The geochemical signature of each group of APS minerals together with the petrography indicates three distinct generations of APS minerals related to the following: (1) paleoweathering of continental surfaces prior to the basin occurrence, (2) diagenetic processes during the burial history of the lower unit of the Thelon sandstones, and (3) hydrothermal alteration processes which accompanied the uranium deposition in the basement rocks and partially overlap the sedimentary-diagenetic mineral parageneses. In addition, the association of a first generation of APS minerals with both detrital cerium oxide and aluminum oxy-hydroxide highlights the fact that a part of the detrital material of the basal Thelon Formation originated from eroded paleolaterite (allochthonous regolith). The primary rare earth element (REE)-bearing minerals (e.g., monazite, REE carbonates, and allanite) of the host rocks were characterized to identify the potential sources of REE. The REE chemical composition highlights a local re-incorporation of the REE released from the alteration processes in the APS minerals of hydrothermal origin. The distinctive geochemical signatures between diagenetic (or sedimentary) and hydrothermal APS minerals suggest a different source material in the Thelon basin than in the Athabasca basin. Keywords APS minerals Thelon Hydrothermal alteration Paleo-laterite

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700