Standard
Harvard
Курапов, МЮ, Конопелько, ДЛ, Ершова, ВБ, Проскурнин, ВФ
, Петров, СВ & Берзин , СВ 2024, '
ТРИАСОВЫЙ АДАКИТОВЫЙ МАГМАТИЗМ СЕВЕРО-ВОСТОКА ПОЛУОСТРОВА ТАЙМЫР', Работа представлена на XIV Международная научно-практическая конференция «Геология и минерально-сырьевые ресурсы северо-востока России», Якутск, Российская Федерация,
26/03/24 -
29/03/24 стр. 340-341. <
https://diamond.ysn.ru/wp-content/uploads/2024/12/%D0%93%D0%B5%D0%BE%D0%BB%D0%BE%D0%B3%D0%B8%D1%8F-%D0%B8-%D0%BC%D0%B8%D0%BD%D0%B5%D1%80%D0%B0%D0%BB%D1%8C%D0%BD%D0%BE-%D1%81%D1%8B%D1%80%D1%8C%D0%B5%D0%B2%D1%8B%D0%B5-%D1%80%D0%B5%D1%81%D1%83%D1%80%D1%81%D1%8B-%D0%A1%D0%B5%D0%B2%D0%B5%D1%80%D0%BE-%D0%92%D0%BE%D1%81%D1%82%D0%BE%D0%BA%D0%B0-%D0%A0%D0%BE%D1%81%D1%81%D0%B8%D0%B8-2024-%D1%81-%D0%BD%D0%B0%D0%B2%D0%B8%D0%B3%D0%B0%D1%86%D0%B8%D0%B5%D0%B9.pdf>
APA
Курапов, М. Ю., Конопелько, Д. Л., Ершова, В. Б., Проскурнин, В. Ф.
, Петров, С. В., & Берзин , С. В. (2024).
ТРИАСОВЫЙ АДАКИТОВЫЙ МАГМАТИЗМ СЕВЕРО-ВОСТОКА ПОЛУОСТРОВА ТАЙМЫР. 340-341. Работа представлена на XIV Международная научно-практическая конференция «Геология и минерально-сырьевые ресурсы северо-востока России», Якутск, Российская Федерация.
https://diamond.ysn.ru/wp-content/uploads/2024/12/%D0%93%D0%B5%D0%BE%D0%BB%D0%BE%D0%B3%D0%B8%D1%8F-%D0%B8-%D0%BC%D0%B8%D0%BD%D0%B5%D1%80%D0%B0%D0%BB%D1%8C%D0%BD%D0%BE-%D1%81%D1%8B%D1%80%D1%8C%D0%B5%D0%B2%D1%8B%D0%B5-%D1%80%D0%B5%D1%81%D1%83%D1%80%D1%81%D1%8B-%D0%A1%D0%B5%D0%B2%D0%B5%D1%80%D0%BE-%D0%92%D0%BE%D1%81%D1%82%D0%BE%D0%BA%D0%B0-%D0%A0%D0%BE%D1%81%D1%81%D0%B8%D0%B8-2024-%D1%81-%D0%BD%D0%B0%D0%B2%D0%B8%D0%B3%D0%B0%D1%86%D0%B8%D0%B5%D0%B9.pdf
Vancouver
Author
BibTeX
@conference{0017dc560b984460a166a6579f3faee9,
title = "ТРИАСОВЫЙ АДАКИТОВЫЙ МАГМАТИЗМ СЕВЕРО-ВОСТОКА ПОЛУОСТРОВА ТАЙМЫР",
abstract = "The studied plume-related intrusions of the NE Taimyr are generally classified as evolved high-K I type granites with adakitic affinity. The latter is a regional feature because majority of the analyzed plume-related granitoids are geochemically similar to high potassium continental adakites. It is suggested that adakitic geochemical characteristics of the plume-related granitoids resulted from melting of hydrated mafic lower crustal protoliths and were controlled by the source lithology.",
author = "Курапов, {Михаил Юрьевич} and Конопелько, {Дмитрий Леонидович} and Ершова, {Виктория Бэртовна} and Проскурнин, {Василий Федорович} and Петров, {Сергей Викторович} and Берзин, {Степан Васильевич}",
year = "2024",
language = "русский",
pages = "340--341",
note = "XIV Международная научно-практическая конференция «Геология и минерально-сырьевые ресурсы северо-востока России» : посвященная 300-летию Российской Академии наук и 100-летию золотодобывающей промышленности РС (Я), МНПК ; Conference date: 26-03-2024 Through 29-03-2024",
url = "https://geo.ysn.ru/",
}
RIS
TY - CONF
T1 - ТРИАСОВЫЙ АДАКИТОВЫЙ МАГМАТИЗМ СЕВЕРО-ВОСТОКА ПОЛУОСТРОВА ТАЙМЫР
AU - Курапов, Михаил Юрьевич
AU - Конопелько, Дмитрий Леонидович
AU - Ершова, Виктория Бэртовна
AU - Проскурнин, Василий Федорович
AU - Петров, Сергей Викторович
AU - Берзин , Степан Васильевич
N1 - Conference code: 14
PY - 2024
Y1 - 2024
N2 - The studied plume-related intrusions of the NE Taimyr are generally classified as evolved high-K I type granites with adakitic affinity. The latter is a regional feature because majority of the analyzed plume-related granitoids are geochemically similar to high potassium continental adakites. It is suggested that adakitic geochemical characteristics of the plume-related granitoids resulted from melting of hydrated mafic lower crustal protoliths and were controlled by the source lithology.
AB - The studied plume-related intrusions of the NE Taimyr are generally classified as evolved high-K I type granites with adakitic affinity. The latter is a regional feature because majority of the analyzed plume-related granitoids are geochemically similar to high potassium continental adakites. It is suggested that adakitic geochemical characteristics of the plume-related granitoids resulted from melting of hydrated mafic lower crustal protoliths and were controlled by the source lithology.
M3 - материалы
SP - 340
EP - 341
T2 - XIV Международная научно-практическая конференция «Геология и минерально-сырьевые ресурсы северо-востока России»
Y2 - 26 March 2024 through 29 March 2024
ER -
