gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2021-12-4-0560gtcrust-1371Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSДИСБАЛАНС Pd/Pt В ЛАВАХ И ИНТРУЗИЯХ НОРИЛЬСКО-ТАЛНАХСКОГО РУДНОГО РАЙОНАPd/Pt IMBALANCE IN LAVAS AND INTRUSIONS OF THE NORILSK-TALNAKH ORE REGIONДудкинТ. В.DudkinT. V.

664033, Иркутск, ул. Лермонтова, 128,

663300, Норильск, Промзона, 1

128 Lermontov St, Irkutsk 664033,

1 Promzona, Norilsk, 663300

МарфинА. Е.MarfinA. E.

664033, Иркутск, ул. Лермонтова, 128

Alexander E. Marfin

128 Lermontov St, Irkutsk 664033

marfin1309@gmail.comИвановА. В.IvanovA. V.

664033, Иркутск, ул. Лермонтова, 128

128 Lermontov St, Irkutsk 664033

КаменецкийВ. С.KamenetskyV. S.

664033, Иркутск, ул. Лермонтова, 128

128 Lermontov St, Irkutsk 664033

Институт земной коры СО РАН; ООО «Норильскгеология»РоссияInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences; Norilskgeologiya LLCRussian FederationИнститут земной коры СО РАНРоссияInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of SciencesRussian Federation202114122021124883890Copyright © Дудкин Т.В., Марфин А.Е., Иванов А.В., Каменецкий В.С., 20212021Дудкин Т.В., Марфин А.Е., Иванов А.В., Каменецкий В.С.Dudkin T.V., Marfin A.E., Ivanov A.V., Kamenetsky V.S.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/1371

В работе рассмотрены значения Pd/Pt отношения в рудах месторождений Норильск-1 и Талнахское, связанных с пермско-триасовыми интрузиями норильского типа, а также проведено сравнение с таковым отношением в одновозрастных лавах Норильского района. Показано, что в лавах Pd/Pt отношение составляет в среднем 1, а в рудах и безрудных горизонтах интрузий Норильск-1 и Талнах превышает это значение в 2–4 раза. Наиболее вероятно, такое увеличение указывает на заимствование магмой этих элементов из существовавших в коре малых и средних месторождений, связанных с предшествующим этапом пермского островодужного вулканизма.

The paper considers the Pd/Pt ratio in the ores of the Norilsk-1 and Talnakh deposits associated with the Permian-Triassic intrusions of the Norilsk type in comparison with that in the lavas of the same age in the Norilsk region. The Pd/Pt mean ratio is 1 in lavas and 2–4 times higher than that in ores and barren horizons of the Norilsk-1 and Talnakh intrusions. Such an increase implies that these elements were borrowed by magma from small and medium-sized crust deposits associated with the previous stage of Permian island-arc volcanism.

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The authors declare that there are no conflicts of interest present.