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Basin formation followed an interval of felsic volcanism and weathering of underlying bedrock.The diagenetic evolution of theThelon lasted about one billion years and was punctuated by £uid movement in£uenced by tectonic events. Early quartz cements formed in well-sorted, quartz-rich facies during diagenetic stage 1; £uids in which these overgrowths formed had d 18 O values near 0% (Vienna Standard Mean Ocean Water). Uranium-rich apatite cement (P1) also formed during diagenetic stage 1 indicating that oxygenated, uraniumbearing pore water was present in the basin early in its diagenetic history. Syntaxial quartz cement (Q1) formed in water with d 18 O from À 4 to À 0.8% in diagenetic stage 2. Diagenetic stage 3 occurred when theThelon Formation was at ca. 5 km depth, and was marked by extensive illitization, alteration of detrital grains, and uranium mineralization. Basin-wide, illite crystallized at $200 1C by £uids with d 18 O values of 5^9% and dD values of À 60 to À 31%, consistent with evolved basinal brines. Tectonism caused by the accretion of Nena at ca.1600 Ma may have provided the mechanism for brine movement during deep burial. Diagenetic stage 4 is associated with fracturing and emplacement of ma¢c dikes at ca. 1300 Ma, quartz cement (Q3) in fractures and vugs, further illitization, and recrystallization of uraninite (U2). Q3 cements have £uid inclusions that suggest variable salinities, d 18 O values of1.5^9%, and dD values of À 97 to À 83% for stage 4 brines. K-feldspar and Mg-chlorite formed during diagenetic stage 5 at ca. 1000 Ma in upper stratigraphic sequences, and in the west. These phases precipitated from low-temperature, isotopically distinct £uids.Their distribution indicates that the basin hydrostratigraphy remained partitioned for 4600 Ma.","grobid_abstract_attachment_id":"33916492"},"document_type":"paper","pre_hit_view_count_baseline":null,"quality":"high","language":"en","title":"Basin evolution, diagenesis and uranium mineralization in the PaleoproterozicThelon Basin, Nunavut, Canada","broadcastable":true,"draft":null,"has_indexable_attachment":true,"indexable":true}}["work"]; window.loswp.workCoauthors = [12813960,23971819]; window.loswp.locale = "en"; window.loswp.countryCode = "SG"; window.loswp.cwvAbTestBucket = ""; window.loswp.designVariant = "ds_vanilla"; window.loswp.fullPageMobileSutdModalVariant = "control"; window.loswp.useOptimizedScribd4genScript = false; window.loswp.appleClientId = 'edu.academia.applesignon';</script><script defer="" src="https://accounts.google.com/gsi/client"></script><div class="ds-loswp-container"><div 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href="https://www.academia.edu/26196637/Comparison_of_diagenetic_fluids_in_the_Proterozoic_Thelon_and_Athabasca_Basins_Canada_implications_for_protracted_fluid_histories_in_stable_intracratonic_basins">Comparison of diagenetic fluids in the Proterozoic Thelon and Athabasca Basins, Canada: implications for protracted fluid histories in stable intracratonic basins</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="50098757" href="https://independent.academia.edu/KyleDurocher">Kyle Durocher</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Canadian Journal of Earth Sciences, 2002</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Comparison of diagenetic fluids in the Proterozoic Thelon and Athabasca Basins, Canada: implications for protracted fluid histories in 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data-collection-position="4" data-entity-id="7309810" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/7309810/Hydrogeology_sequence_stratigraphy_and_diagenesis_in_the_Paleoproterozoic_western_Thelon_Basin_Influences_on_unconformity_related_uranium_mineralization">Hydrogeology, sequence stratigraphy and diagenesis in the Paleoproterozoic western Thelon Basin: Influences on unconformity-related uranium mineralization</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="12813960" href="https://uwosh.academia.edu/EricHiatt">Eric E Hiatt</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="50060238" href="https://independent.academia.edu/CPettman">Chris Pettman</a></div><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" 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PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="5" data-entity-id="50964305" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/50964305/Fault_Zone_Evolution_and_Development_of_a_Structural_and_Hydrological_Barrier_The_Quartz_Breccia_in_the_Kiggavik_Area_Nunavut_Canada_and_Its_Control_on_Uranium_Mineralization">Fault Zone Evolution and Development of a Structural and Hydrological Barrier: The Quartz Breccia in the Kiggavik Area (Nunavut, Canada) and Its Control on Uranium Mineralization</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="5708074" href="https://independent.academia.edu/AntonioBenedicto">Antonio Benedicto</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Minerals</p><p class="ds-related-work--abstract ds2-5-body-sm">In the Kiggavik area (Nunavut, Canada), major fault zones along, or close to, where uranium deposits are found are often associated with occurrence of thick quartz breccia (QB) bodies. These bodies formed in an early stage (~1750 Ma) of the long-lasting tectonic history of the Archean basement, and of the Proterozoic Thelon basin. The main characteristics of the QB are addressed in this study; through field work, macro and microscopic observations, cathodoluminescence microscopy, trace elements, and oxygen isotopic signatures of the quartz forming the QB. Faults formed earlier during syn- to post-orogenic rifting (1850–1750 Ma) were subsequently reactivated, and underwent cycles of cataclasis, pervasive silicification, hydraulic brecciation, and quartz recrystallization. This was synchronous with the circulation of meteoric fluids mixing with Si-rich magmatic-derived fluids at depth, and were coeval with the emplacement of the Kivalliq igneous suite at 1750 Ma. These processes led t...</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Fault Zone Evolution and Development of a Structural and Hydrological Barrier: The Quartz Breccia in the Kiggavik Area (Nunavut, Canada) and Its Control on Uranium Mineralization","attachmentId":68839742,"attachmentType":"pdf","work_url":"https://www.academia.edu/50964305/Fault_Zone_Evolution_and_Development_of_a_Structural_and_Hydrological_Barrier_The_Quartz_Breccia_in_the_Kiggavik_Area_Nunavut_Canada_and_Its_Control_on_Uranium_Mineralization","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" 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