Integration of multiple sulfur isotopes with structural analysis unveils the evolution of ore fluids and source of sulfur at the Kanowna Belle Archean orogenic gold deposit, Yilgarn Craton, Western Australia
The Kanowna Belle deposit is a world-class Archean orogenic gold system that witnessed multiple fluid episodes over a protracted deformation history. The hydrothermal fluid circulation episodes at the Kanowna Belle deposit initiated with the precipitation of early gold-bearing carbonate-famatinite-p...
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| Veröffentlicht in: | Mineralium deposita 2021-11, Vol.56 (8), p.1471-1490 |
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| creator | Sugiono, Dennis Thébaud, Nicolas LaFlamme, Crystal Fiorentini, Marco Martin, Laure Rogers, Jamie Lorusso, Giovanna McFarlane, Chris |
| description | The Kanowna Belle deposit is a world-class Archean orogenic gold system that witnessed multiple fluid episodes over a protracted deformation history. The hydrothermal fluid circulation episodes at the Kanowna Belle deposit initiated with the precipitation of early gold-bearing carbonate-famatinite-pyrite-telluride-electrum veins (V1a). These early veins were subsequently folded during a NE-SW shortening event (D1b
KB
) that led to the development of sericite-chlorite-pyrite stringers (V1b) and foliation (S1
KB
) dated at c. 2658 ± 9 Ma (U-Pb, xenotime). D1b
KB
structures are overprinted by quartz-carbonate-sericite-pyrite-gold veins (V2) controlled by the reverse faulting formed as a result of N-S shortening during D2
KB.
A subsequent deformation event (D3a
KB
) is related to sinistral shearing produced under ENE-WSW shortening and associated with the development of the Troy lodes and deposition of quartz-pyrite-sericite-gold veins (V3a) dated at c. 2628 ± 9 Ma (U-Pb, xenotime). The application of multiple sulfur isotope analyses of sulfides related to the different mineralization events resolves the hydrothermal fluid isotopic evolution through time. Despite the ore mineralogy differences of the V1, V2, and V3 vein sets, their associated sulfides yield small positive ∆
33
S (+ 0.1 to + 0.4‰;
n
= 231) values with two outliers (∆
33
S = + 0.5‰ and + 0.6‰) across all lithology types. The constant value of MIF-S through the three temporally different gold mineralization episodes implies that sulfur was derived from a single homogenized source of sulfur distal from the deposition site, irrespective of the Au endowment. The consistent small positive ∆
33
S sulfur isotope signature may support that the Archean orogenic gold system sourced sulfur and possibly hydrothermal fluids from a mantle/magmatic dominated source that homogenized with crustal sulfur at depth prior to gold deposition. |
| doi_str_mv | 10.1007/s00126-020-01032-1 |
| format | Article |
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KB
) that led to the development of sericite-chlorite-pyrite stringers (V1b) and foliation (S1
KB
) dated at c. 2658 ± 9 Ma (U-Pb, xenotime). D1b
KB
structures are overprinted by quartz-carbonate-sericite-pyrite-gold veins (V2) controlled by the reverse faulting formed as a result of N-S shortening during D2
KB.
A subsequent deformation event (D3a
KB
) is related to sinistral shearing produced under ENE-WSW shortening and associated with the development of the Troy lodes and deposition of quartz-pyrite-sericite-gold veins (V3a) dated at c. 2628 ± 9 Ma (U-Pb, xenotime). The application of multiple sulfur isotope analyses of sulfides related to the different mineralization events resolves the hydrothermal fluid isotopic evolution through time. Despite the ore mineralogy differences of the V1, V2, and V3 vein sets, their associated sulfides yield small positive ∆
33
S (+ 0.1 to + 0.4‰;
n
= 231) values with two outliers (∆
33
S = + 0.5‰ and + 0.6‰) across all lithology types. The constant value of MIF-S through the three temporally different gold mineralization episodes implies that sulfur was derived from a single homogenized source of sulfur distal from the deposition site, irrespective of the Au endowment. The consistent small positive ∆
33
S sulfur isotope signature may support that the Archean orogenic gold system sourced sulfur and possibly hydrothermal fluids from a mantle/magmatic dominated source that homogenized with crustal sulfur at depth prior to gold deposition.</description><identifier>ISSN: 0026-4598</identifier><identifier>EISSN: 1432-1866</identifier><identifier>DOI: 10.1007/s00126-020-01032-1</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Carbonates ; Chlorite ; Cratons ; Deformation ; Deposition ; Earth and Environmental Science ; Earth Sciences ; Evolution ; Fluids ; Geology ; Gold ; Isotopes ; Lead ; Lithology ; Mineral Resources ; Mineralization ; Mineralogy ; Orogeny ; Outliers (statistics) ; Pipe stringers ; Pyrite ; Quartz ; Shearing ; Stringers ; Structural analysis ; Sulfides ; Sulfur ; Sulfur isotopes ; Sulphur ; Tellurides ; Veins (geology) ; Xenotime</subject><ispartof>Mineralium deposita, 2021-11, Vol.56 (8), p.1471-1490</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH, DE part of Springer Nature 2021</rights><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH, DE part of Springer Nature 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a342t-cf87a58c737c0eda75c1be76b2bb3fa81456a85565aa55d161b2983c9b24db223</citedby><cites>FETCH-LOGICAL-a342t-cf87a58c737c0eda75c1be76b2bb3fa81456a85565aa55d161b2983c9b24db223</cites><orcidid>0000-0002-4417-0621</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00126-020-01032-1$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00126-020-01032-1$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Sugiono, Dennis</creatorcontrib><creatorcontrib>Thébaud, Nicolas</creatorcontrib><creatorcontrib>LaFlamme, Crystal</creatorcontrib><creatorcontrib>Fiorentini, Marco</creatorcontrib><creatorcontrib>Martin, Laure</creatorcontrib><creatorcontrib>Rogers, Jamie</creatorcontrib><creatorcontrib>Lorusso, Giovanna</creatorcontrib><creatorcontrib>McFarlane, Chris</creatorcontrib><title>Integration of multiple sulfur isotopes with structural analysis unveils the evolution of ore fluids and source of sulfur at the Kanowna Belle Archean orogenic gold deposit, Yilgarn Craton, Western Australia</title><title>Mineralium deposita</title><addtitle>Miner Deposita</addtitle><description>The Kanowna Belle deposit is a world-class Archean orogenic gold system that witnessed multiple fluid episodes over a protracted deformation history. The hydrothermal fluid circulation episodes at the Kanowna Belle deposit initiated with the precipitation of early gold-bearing carbonate-famatinite-pyrite-telluride-electrum veins (V1a). These early veins were subsequently folded during a NE-SW shortening event (D1b
KB
) that led to the development of sericite-chlorite-pyrite stringers (V1b) and foliation (S1
KB
) dated at c. 2658 ± 9 Ma (U-Pb, xenotime). D1b
KB
structures are overprinted by quartz-carbonate-sericite-pyrite-gold veins (V2) controlled by the reverse faulting formed as a result of N-S shortening during D2
KB.
A subsequent deformation event (D3a
KB
) is related to sinistral shearing produced under ENE-WSW shortening and associated with the development of the Troy lodes and deposition of quartz-pyrite-sericite-gold veins (V3a) dated at c. 2628 ± 9 Ma (U-Pb, xenotime). The application of multiple sulfur isotope analyses of sulfides related to the different mineralization events resolves the hydrothermal fluid isotopic evolution through time. Despite the ore mineralogy differences of the V1, V2, and V3 vein sets, their associated sulfides yield small positive ∆
33
S (+ 0.1 to + 0.4‰;
n
= 231) values with two outliers (∆
33
S = + 0.5‰ and + 0.6‰) across all lithology types. The constant value of MIF-S through the three temporally different gold mineralization episodes implies that sulfur was derived from a single homogenized source of sulfur distal from the deposition site, irrespective of the Au endowment. The consistent small positive ∆
33
S sulfur isotope signature may support that the Archean orogenic gold system sourced sulfur and possibly hydrothermal fluids from a mantle/magmatic dominated source that homogenized with crustal sulfur at depth prior to gold deposition.</description><subject>Carbonates</subject><subject>Chlorite</subject><subject>Cratons</subject><subject>Deformation</subject><subject>Deposition</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Evolution</subject><subject>Fluids</subject><subject>Geology</subject><subject>Gold</subject><subject>Isotopes</subject><subject>Lead</subject><subject>Lithology</subject><subject>Mineral Resources</subject><subject>Mineralization</subject><subject>Mineralogy</subject><subject>Orogeny</subject><subject>Outliers (statistics)</subject><subject>Pipe stringers</subject><subject>Pyrite</subject><subject>Quartz</subject><subject>Shearing</subject><subject>Stringers</subject><subject>Structural analysis</subject><subject>Sulfides</subject><subject>Sulfur</subject><subject>Sulfur isotopes</subject><subject>Sulphur</subject><subject>Tellurides</subject><subject>Veins (geology)</subject><subject>Xenotime</subject><issn>0026-4598</issn><issn>1432-1866</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9UU1v1DAQjRBILIU_wMkS14baTpyP47ICWrUSFxDiFE2cSdaVaweP3aq_sn8Jb7dVb5zGo3nvzfO8ovgo-GfBeXtGnAvZlFzykgteyVK8KjaiPjy6pnldbDjP41r13dviHdE157wXNd8UDxcu4hIgGu-Yn9lNstGsFhklO6fADPnoVyR2Z-KeUQxJxxTAMnBg78kQS-4WjSUW98jw1tv0LOUDstkmM1EGT4x8ChoPgydpiI-cS3D-zgH7gjav3Qa9R8j84Bd0RrPF24lNuHoy8ZT9MXaB4NguO_bulP1Gipj7bcrWwBp4X7yZwRJ-eKonxa9vX3_uzsurH98vdturEqpaxlLPXQuq023Vao4TtEqLEdtmlONYzdCJWjXQKdUoAKUm0YhR9l2l-1HW0yhldVJ8Ouquwf9N2cVwnf-Xb0KDVB0Xfb53nVHyiNLBEwWchzWYGwj3g-DDIbjhGNyQgxsegxtEJlVHEmWwWzC8SP-H9Q9tPKDK</recordid><startdate>20211101</startdate><enddate>20211101</enddate><creator>Sugiono, Dennis</creator><creator>Thébaud, Nicolas</creator><creator>LaFlamme, Crystal</creator><creator>Fiorentini, Marco</creator><creator>Martin, Laure</creator><creator>Rogers, Jamie</creator><creator>Lorusso, Giovanna</creator><creator>McFarlane, Chris</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0002-4417-0621</orcidid></search><sort><creationdate>20211101</creationdate><title>Integration of multiple sulfur isotopes with structural analysis unveils the evolution of ore fluids and source of sulfur at the Kanowna Belle Archean orogenic gold deposit, Yilgarn Craton, Western Australia</title><author>Sugiono, Dennis ; 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The hydrothermal fluid circulation episodes at the Kanowna Belle deposit initiated with the precipitation of early gold-bearing carbonate-famatinite-pyrite-telluride-electrum veins (V1a). These early veins were subsequently folded during a NE-SW shortening event (D1b
KB
) that led to the development of sericite-chlorite-pyrite stringers (V1b) and foliation (S1
KB
) dated at c. 2658 ± 9 Ma (U-Pb, xenotime). D1b
KB
structures are overprinted by quartz-carbonate-sericite-pyrite-gold veins (V2) controlled by the reverse faulting formed as a result of N-S shortening during D2
KB.
A subsequent deformation event (D3a
KB
) is related to sinistral shearing produced under ENE-WSW shortening and associated with the development of the Troy lodes and deposition of quartz-pyrite-sericite-gold veins (V3a) dated at c. 2628 ± 9 Ma (U-Pb, xenotime). The application of multiple sulfur isotope analyses of sulfides related to the different mineralization events resolves the hydrothermal fluid isotopic evolution through time. Despite the ore mineralogy differences of the V1, V2, and V3 vein sets, their associated sulfides yield small positive ∆
33
S (+ 0.1 to + 0.4‰;
n
= 231) values with two outliers (∆
33
S = + 0.5‰ and + 0.6‰) across all lithology types. The constant value of MIF-S through the three temporally different gold mineralization episodes implies that sulfur was derived from a single homogenized source of sulfur distal from the deposition site, irrespective of the Au endowment. The consistent small positive ∆
33
S sulfur isotope signature may support that the Archean orogenic gold system sourced sulfur and possibly hydrothermal fluids from a mantle/magmatic dominated source that homogenized with crustal sulfur at depth prior to gold deposition.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00126-020-01032-1</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0002-4417-0621</orcidid></addata></record> |
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| ispartof | Mineralium deposita, 2021-11, Vol.56 (8), p.1471-1490 |
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| language | eng |
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| source | SpringerNature Journals |
| subjects | Carbonates Chlorite Cratons Deformation Deposition Earth and Environmental Science Earth Sciences Evolution Fluids Geology Gold Isotopes Lead Lithology Mineral Resources Mineralization Mineralogy Orogeny Outliers (statistics) Pipe stringers Pyrite Quartz Shearing Stringers Structural analysis Sulfides Sulfur Sulfur isotopes Sulphur Tellurides Veins (geology) Xenotime |
| title | Integration of multiple sulfur isotopes with structural analysis unveils the evolution of ore fluids and source of sulfur at the Kanowna Belle Archean orogenic gold deposit, Yilgarn Craton, Western Australia |
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