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U–Pb Age and Geochemistry of Detrital Zircons from Quartzites of the Daldyn Group, Anabar Shield, Northern Central Siberia, Russia
— The paper presents U–Pb zircon dates (SHRIMP-II) and isotopic-geochemical data (SIMS and Sm–Nd method) on detrital zircon and its sedimentary host rocks of the Daldyn Group at the Anabar Shield. The rocks were metamorphosed to the granulite facies. The oldest Eoarchean (3.7 Ga) source of terrigeno...
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Published in: | Geochemistry international 2020-06, Vol.58 (6), p.737-745 |
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The paper presents U–Pb zircon dates (SHRIMP-II) and isotopic-geochemical data (SIMS and Sm–Nd method) on detrital zircon and its sedimentary host rocks of the Daldyn Group at the Anabar Shield. The rocks were metamorphosed to the granulite facies. The oldest Eoarchean (3.7 Ga) source of terrigenous material (determined based on single zircon grains) is confirmed by the Nd model age of the protolith: T
Nd
(DM)
2
= 3.69–3.71 Ga. The rocks are dominated by zircon dated at 3.5 Ga, which reflects that the area from which the terrigenous material was brought consisted mostly of Paleoarchean magmatic rocks. |
doi_str_mv | 10.1134/S0016702920060117 |
format | article |
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The paper presents U–Pb zircon dates (SHRIMP-II) and isotopic-geochemical data (SIMS and Sm–Nd method) on detrital zircon and its sedimentary host rocks of the Daldyn Group at the Anabar Shield. The rocks were metamorphosed to the granulite facies. The oldest Eoarchean (3.7 Ga) source of terrigenous material (determined based on single zircon grains) is confirmed by the Nd model age of the protolith: T
Nd
(DM)
2
= 3.69–3.71 Ga. The rocks are dominated by zircon dated at 3.5 Ga, which reflects that the area from which the terrigenous material was brought consisted mostly of Paleoarchean magmatic rocks.</description><identifier>ISSN: 0016-7029</identifier><identifier>EISSN: 1556-1968</identifier><identifier>DOI: 10.1134/S0016702920060117</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Geochronology ; Isotopes ; Lead ; Magma ; Quartzite ; Radiometric dating ; Rock ; Rocks ; Rocks, Metamorphic ; Sedimentary facies ; Short Communications ; Zircon</subject><ispartof>Geochemistry international, 2020-06, Vol.58 (6), p.737-745</ispartof><rights>Pleiades Publishing, Ltd. 2020</rights><rights>COPYRIGHT 2020 Springer</rights><rights>Pleiades Publishing, Ltd. 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a330t-f843052fff517985f150ac20f5d37f42c90b3dd0e4509e1c34ea74ae95c205b73</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Sergeeva, L. Yu</creatorcontrib><creatorcontrib>Gusev, N. I.</creatorcontrib><creatorcontrib>Skublov, S. G.</creatorcontrib><title>U–Pb Age and Geochemistry of Detrital Zircons from Quartzites of the Daldyn Group, Anabar Shield, Northern Central Siberia, Russia</title><title>Geochemistry international</title><addtitle>Geochem. Int</addtitle><description>—
The paper presents U–Pb zircon dates (SHRIMP-II) and isotopic-geochemical data (SIMS and Sm–Nd method) on detrital zircon and its sedimentary host rocks of the Daldyn Group at the Anabar Shield. The rocks were metamorphosed to the granulite facies. The oldest Eoarchean (3.7 Ga) source of terrigenous material (determined based on single zircon grains) is confirmed by the Nd model age of the protolith: T
Nd
(DM)
2
= 3.69–3.71 Ga. The rocks are dominated by zircon dated at 3.5 Ga, which reflects that the area from which the terrigenous material was brought consisted mostly of Paleoarchean magmatic rocks.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Geochronology</subject><subject>Isotopes</subject><subject>Lead</subject><subject>Magma</subject><subject>Quartzite</subject><subject>Radiometric dating</subject><subject>Rock</subject><subject>Rocks</subject><subject>Rocks, Metamorphic</subject><subject>Sedimentary facies</subject><subject>Short Communications</subject><subject>Zircon</subject><issn>0016-7029</issn><issn>1556-1968</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1kb9u2zAQxomiBeqkeYBuBLJaKSmSojQaTuoWCPrPydJFoKSjzUAmnSM1uFOHvkHfsE9SGg6QoSg4HMD7fd8dviPkLWdXnAv5bs0YrzQrm5KxinGuX5AZV6oqeFPVL8ns2C6O_dfkLMYHxqQUjZ6RX_d_fv7-0tHFBqjxA11B6LewczHhgQZLryGhS2ak3x32wUdqMezo18lg-uESxCOTtkCvzTgcPF1hmPZzuvCmM0jXWwfjMKefAmYGPV2CT5jN1q4DdGZOv00xOvOGvLJmjHDxVM_J_fubu-WH4vbz6uNycVsYIVgqbC0FU6W1VnHd1MpyxUxfMqsGoa0s-4Z1YhgYSMUa4L2QYLQ00KgMqU6Lc3J58t1jeJwgpvYhTOjzyLaUXKg6ZyczdXWiNmaE1nkb8s59fkPOJWcA1uX_hc6eVa0bkQX8JOgxxIhg2z26ncFDy1l7vE77z3WypjxpYmb9BvB5lf-L_gLkwJD7</recordid><startdate>20200601</startdate><enddate>20200601</enddate><creator>Sergeeva, L. Yu</creator><creator>Gusev, N. I.</creator><creator>Skublov, S. G.</creator><general>Pleiades Publishing</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20200601</creationdate><title>U–Pb Age and Geochemistry of Detrital Zircons from Quartzites of the Daldyn Group, Anabar Shield, Northern Central Siberia, Russia</title><author>Sergeeva, L. Yu ; Gusev, N. I. ; Skublov, S. G.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a330t-f843052fff517985f150ac20f5d37f42c90b3dd0e4509e1c34ea74ae95c205b73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geochemistry</topic><topic>Geochronology</topic><topic>Isotopes</topic><topic>Lead</topic><topic>Magma</topic><topic>Quartzite</topic><topic>Radiometric dating</topic><topic>Rock</topic><topic>Rocks</topic><topic>Rocks, Metamorphic</topic><topic>Sedimentary facies</topic><topic>Short Communications</topic><topic>Zircon</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sergeeva, L. Yu</creatorcontrib><creatorcontrib>Gusev, N. I.</creatorcontrib><creatorcontrib>Skublov, S. G.</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geochemistry international</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sergeeva, L. Yu</au><au>Gusev, N. I.</au><au>Skublov, S. G.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>U–Pb Age and Geochemistry of Detrital Zircons from Quartzites of the Daldyn Group, Anabar Shield, Northern Central Siberia, Russia</atitle><jtitle>Geochemistry international</jtitle><stitle>Geochem. Int</stitle><date>2020-06-01</date><risdate>2020</risdate><volume>58</volume><issue>6</issue><spage>737</spage><epage>745</epage><pages>737-745</pages><issn>0016-7029</issn><eissn>1556-1968</eissn><abstract>—
The paper presents U–Pb zircon dates (SHRIMP-II) and isotopic-geochemical data (SIMS and Sm–Nd method) on detrital zircon and its sedimentary host rocks of the Daldyn Group at the Anabar Shield. The rocks were metamorphosed to the granulite facies. The oldest Eoarchean (3.7 Ga) source of terrigenous material (determined based on single zircon grains) is confirmed by the Nd model age of the protolith: T
Nd
(DM)
2
= 3.69–3.71 Ga. The rocks are dominated by zircon dated at 3.5 Ga, which reflects that the area from which the terrigenous material was brought consisted mostly of Paleoarchean magmatic rocks.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0016702920060117</doi><tpages>9</tpages></addata></record> |
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subjects | Earth and Environmental Science Earth Sciences Geochemistry Geochronology Isotopes Lead Magma Quartzite Radiometric dating Rock Rocks Rocks, Metamorphic Sedimentary facies Short Communications Zircon |
title | U–Pb Age and Geochemistry of Detrital Zircons from Quartzites of the Daldyn Group, Anabar Shield, Northern Central Siberia, Russia |
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