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Age, Composition, and Metallogeny of the Pyrkataghin Granitoid Massif, Chukotka Arctic Coast, Northeastern Russia
Аbstract The first U–Th–Pb zircon data on granitoids of the Pyrkataghin massif located in the central part of the Kuul Rise of the Anyui–Chukotka fold system on the coast of the East Siberian Sea are provided. They are indicative of the granitoid intrusion in the Albian (106–104 Ma) corresponding to...
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Published in: | Doklady earth sciences 2024, Vol.519 (2), p.2049-2062 |
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creator | Luchitskaya, M. V. Vatrushkina, E. V. Mazurkevich, K. N. Sokolov, S. D. |
description | Аbstract
The first U–Th–Pb zircon data on granitoids of the Pyrkataghin massif located in the central part of the Kuul Rise of the Anyui–Chukotka fold system on the coast of the East Siberian Sea are provided. They are indicative of the granitoid intrusion in the Albian (106–104 Ma) corresponding to the Albian granitoid magmatism of Chauna province in the Chukotka region (110–100 Ma [1]) and to the Aptian–Albian postcollision extension after termination of collision between the Chukotka–Arctic Alaska microcontinent and the Siberian continent with the earlier accreted Kolyma–Omolon microcontinent. The increased alkalinity and geochemical features of Pyrkatagin massif granitoids, such as enrichment in LIL and LREEs and depletion in Ta, Nb, Ba, and Sr, make them similar to other postcollision granitoids of the Chauna province. Granitoids of the massif and granitoids with different types of mineralization are compared. |
doi_str_mv | 10.1134/S1028334X24604061 |
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The first U–Th–Pb zircon data on granitoids of the Pyrkataghin massif located in the central part of the Kuul Rise of the Anyui–Chukotka fold system on the coast of the East Siberian Sea are provided. They are indicative of the granitoid intrusion in the Albian (106–104 Ma) corresponding to the Albian granitoid magmatism of Chauna province in the Chukotka region (110–100 Ma [1]) and to the Aptian–Albian postcollision extension after termination of collision between the Chukotka–Arctic Alaska microcontinent and the Siberian continent with the earlier accreted Kolyma–Omolon microcontinent. The increased alkalinity and geochemical features of Pyrkatagin massif granitoids, such as enrichment in LIL and LREEs and depletion in Ta, Nb, Ba, and Sr, make them similar to other postcollision granitoids of the Chauna province. Granitoids of the massif and granitoids with different types of mineralization are compared.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X24604061</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Alkalinity ; Chauna ; Earth and Environmental Science ; Earth Sciences ; Geology ; Magma ; Massifs ; Metallogenesis ; Mineralization ; Zircon</subject><ispartof>Doklady earth sciences, 2024, Vol.519 (2), p.2049-2062</ispartof><rights>Pleiades Publishing, Ltd. 2024 ISSN 1028-334X, Doklady Earth Sciences, 2024, Vol. 519, Part 2, pp. 2049–2062. © Pleiades Publishing, Ltd., 2024.ISSN 1028-334X, Doklady Earth Sciences, 2024. © Pleiades Publishing, Ltd., 2024.</rights><rights>Copyright Springer Nature B.V. 2024</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c198t-4ae5b0a8e4c45bd60e8f40576c95dfa55de59d045efa09061d10ff2c51822a073</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,27905,27906</link.rule.ids></links><search><creatorcontrib>Luchitskaya, M. V.</creatorcontrib><creatorcontrib>Vatrushkina, E. V.</creatorcontrib><creatorcontrib>Mazurkevich, K. N.</creatorcontrib><creatorcontrib>Sokolov, S. D.</creatorcontrib><title>Age, Composition, and Metallogeny of the Pyrkataghin Granitoid Massif, Chukotka Arctic Coast, Northeastern Russia</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><description>Аbstract
The first U–Th–Pb zircon data on granitoids of the Pyrkataghin massif located in the central part of the Kuul Rise of the Anyui–Chukotka fold system on the coast of the East Siberian Sea are provided. They are indicative of the granitoid intrusion in the Albian (106–104 Ma) corresponding to the Albian granitoid magmatism of Chauna province in the Chukotka region (110–100 Ma [1]) and to the Aptian–Albian postcollision extension after termination of collision between the Chukotka–Arctic Alaska microcontinent and the Siberian continent with the earlier accreted Kolyma–Omolon microcontinent. The increased alkalinity and geochemical features of Pyrkatagin massif granitoids, such as enrichment in LIL and LREEs and depletion in Ta, Nb, Ba, and Sr, make them similar to other postcollision granitoids of the Chauna province. Granitoids of the massif and granitoids with different types of mineralization are compared.</description><subject>Alkalinity</subject><subject>Chauna</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geology</subject><subject>Magma</subject><subject>Massifs</subject><subject>Metallogenesis</subject><subject>Mineralization</subject><subject>Zircon</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp1kEtLAzEUhYMoWKs_wF3AbUeTSTKdWZairVAf-AB3w20mmaaPpE0yi_57Uyq4EFf3wP3OudyD0DUlt5QyfvdOSV4yxr9yXhBOCnqCelQwmpVM8NOk0zo77M_RRQhLQjjnouqh3ahVAzx2m60LJhpnBxhsg59UhPXatcrusdM4LhR-3fsVRGgXxuKJB2uiMwmEEIxOCYtu5eIK8MjLaGRKhBAH-Nn55E1SeYvfusTCJTrTsA7q6mf20efD_cd4ms1eJo_j0SyTtCpjxkGJOYFSccnFvCmIKjUnYljISjQahGiUqBrChdJAqvRwQ4nWuRS0zHMgQ9ZHN8fcrXe7ToVYL13nbTpZs0MzeSUKnih6pKR3IXil6603G_D7mpL60Gz9p9nkyY-ekFjbKv-b_L_pGy3Tew0</recordid><startdate>2024</startdate><enddate>2024</enddate><creator>Luchitskaya, M. V.</creator><creator>Vatrushkina, E. V.</creator><creator>Mazurkevich, K. N.</creator><creator>Sokolov, S. D.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>2024</creationdate><title>Age, Composition, and Metallogeny of the Pyrkataghin Granitoid Massif, Chukotka Arctic Coast, Northeastern Russia</title><author>Luchitskaya, M. V. ; Vatrushkina, E. V. ; Mazurkevich, K. N. ; Sokolov, S. D.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c198t-4ae5b0a8e4c45bd60e8f40576c95dfa55de59d045efa09061d10ff2c51822a073</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Alkalinity</topic><topic>Chauna</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geology</topic><topic>Magma</topic><topic>Massifs</topic><topic>Metallogenesis</topic><topic>Mineralization</topic><topic>Zircon</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Luchitskaya, M. V.</creatorcontrib><creatorcontrib>Vatrushkina, E. V.</creatorcontrib><creatorcontrib>Mazurkevich, K. N.</creatorcontrib><creatorcontrib>Sokolov, S. D.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</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>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Doklady earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Luchitskaya, M. V.</au><au>Vatrushkina, E. V.</au><au>Mazurkevich, K. N.</au><au>Sokolov, S. D.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Age, Composition, and Metallogeny of the Pyrkataghin Granitoid Massif, Chukotka Arctic Coast, Northeastern Russia</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2024</date><risdate>2024</risdate><volume>519</volume><issue>2</issue><spage>2049</spage><epage>2062</epage><pages>2049-2062</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>Аbstract
The first U–Th–Pb zircon data on granitoids of the Pyrkataghin massif located in the central part of the Kuul Rise of the Anyui–Chukotka fold system on the coast of the East Siberian Sea are provided. They are indicative of the granitoid intrusion in the Albian (106–104 Ma) corresponding to the Albian granitoid magmatism of Chauna province in the Chukotka region (110–100 Ma [1]) and to the Aptian–Albian postcollision extension after termination of collision between the Chukotka–Arctic Alaska microcontinent and the Siberian continent with the earlier accreted Kolyma–Omolon microcontinent. The increased alkalinity and geochemical features of Pyrkatagin massif granitoids, such as enrichment in LIL and LREEs and depletion in Ta, Nb, Ba, and Sr, make them similar to other postcollision granitoids of the Chauna province. Granitoids of the massif and granitoids with different types of mineralization are compared.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1028334X24604061</doi><tpages>14</tpages></addata></record> |
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subjects | Alkalinity Chauna Earth and Environmental Science Earth Sciences Geology Magma Massifs Metallogenesis Mineralization Zircon |
title | Age, Composition, and Metallogeny of the Pyrkataghin Granitoid Massif, Chukotka Arctic Coast, Northeastern Russia |
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