vfuzemlВестник Северо-Восточного федерального университета им. М.К. Аммосова. Vestnik of North-Eastern Federal University. Серия «Науки о Земле». Earth SciencesVestnik of North-Eastern Federal University Series "Earth Sciences"2587-8751Северо-Восточный федеральный университет имени М.К.Аммосова10.25587/2587-8751-2026-1-5-33vfuzeml-389Research ArticleГЕОЛОГИЯGEOCOLOGYТипоморфизм породообразующих минералов андезитов Карабуранского комплекса Половинкинской впадины (Алдано-Становой щит)Typomorphism of rock-forming minerals of andesites from the Karaburan Complex of the Polovinkinskaya Depression (Aldan-Stanovoy shield)https://orcid.org/0000-0002-5485-3127ИвановА. И.IvanovA. I.

Иванов Алексей Иванович – кандидат геолого-минералогических наук, старший научный сотрудник

ResearcherID: JBR-7954-2023

Scopus Author ID: 57674640500

г. Якутск

Alexey I. Ivanov – Cand. Sci. (Geology and Mineralogy), senior researcher 

Researcher ID: JBR-7954-2023

Scopus Author ID: 57674640500

Yakutsk

leps_2002@mail.ruhttps://orcid.org/0000-0002-0204-1653ИвановМ. С.IvanovM. S.

Иванов Мичил Спартакович – младший научный сотрудник

ResearcherID: AAL-7447-2021

Scopus Author ID: 57212410522

г. Якутск

 Michil S. Ivanov – junior researcher

ResearcherID: AAL-7447-2021

Scopus Author ID: 57212410522

Yakutsk

ivanov.michil@bk.ruhttps://orcid.org/0000-0003-0115-5146ЖуравлевА. И.ZhuravlevA. I.

Журавлев Анатолий Иванович – ведущий инженер

ResearcherID: AAC-6095-2019

Scopus Author ID: 57200217371

г. Якутск

Anatolii I. Zhuravlev – leading engineer

ResearcherID: AAC-6095-2019

Scopus Author ID: 57200217371

Yakutsk

ai.zhuravlevgeo@gmail.comhttps://orcid.org/0000-0001-7491-1067ЛоскутовЕ. Е.LoskutovE. E.

Лоскутов Евгений Евгеньевич – кандидат геолого-минералогических наук, старший научный сотрудник

ResearcherID: AAO-4823-2021

Scopus Author ID: 57205150102

г. Якутск

Evgeniy E. Loskutov – Cand. Sci. (Geology and Mineralogy), senior researcher

ResearcherID: AAO-4823-2021

Scopus Author ID: 57205150102

Yakutsk

loskutov@diamond.ysn.ruИнститут геологии алмаза и благородных металлов СО РАНРоссияDiamond and Precious Metal Geology Institute SB RASRussian Federation20262709202603533Copyright © Иванов А.И., Иванов М.С., Журавлев А.И., Лоскутов Е.Е., 20262026Иванов А.И., Иванов М.С., Журавлев А.И., Лоскутов Е.Е.Ivanov A.I., Ivanov M.S., Zhuravlev A.I., Loskutov E.E.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.vnzsvfu.ru/jour/article/view/389

Впервые рассмотрены химические составы породообразующих минералов из андези­тов Половинкинской впадины, локализованной в центральной части Алдано-Станового щита, на грани­це Тындинского и Нимнырского террейнов. Полученные в ходе микрозондовых исследований данные по составам минералов рассчитывались по программам MagMin PT, WinPyrox и COMAGMAT, с целью систематики и определения термодинамических параметров кристаллизации минералов вкрапленников, а также возможной металлогенической специализации андезитов. В результате чего, были установле­ны: плагиоклаз (олигоклаз, андезин первой и второй генераций), а также андезин микролитов основной массы, пироксен (авгит, диопсид), Са-амфибол (эденит, паргасит) и Mg-биотит. Показано, что кристал­лизация олигоклаза и андезина двух генераций проходила в условиях, близких таковым для плагиокла­зов андезитов островных дуг и активных континентальных окраин: при высокой активности кислоро­да (logfO2=-5,04…-6,86) и росте температур от1090оС до 1124оС при снижении давления от 12 кбар до 4,5 кбар. Состав и условия кристаллизации плагиоклазов и пироксенов подтверждают мнение предше­ственников об участии субдуцированной океанической коры Монголо-Охотского бассейна в формиро­вании материнских магматических очагов мезозойского алданского комплекса. На основе выделенных интервалов зависимости Р-Т условий кристаллизации минералов от глубины: (I) 36-24 км, (II) 24-12 км, (III) 12-6 км и (IV) 6-2 км, высказана точка зрения о существовании в мезозое промежуточных магматиче­ских камер. В соответствии с результатами анализа типоморфных характеристик амфиболов и биотитов (фугитивности кислорода и активность воды), а также геологических предпосылок эволюции андезитов, было высказано мнение о возможности обнаружения в пределах Половинкинской впадины золоторудных систем эпитермального типа.

This study presents an inaugural analysis of rock-forming mineral chemistry within andesites from the Polovinkinskaya Depression, situated at the junction of the Tynda and Nimnyr terranes in the central Aldan- Stanovoy Shield. Utilizing microprobe data processed through MagMin PT, WinPyrox, and COMAGMAT, we evaluated the systematics, thermodynamic crystallization conditions, and potential metallogenic significance of these rocks. The mineral assemblage includes plagioclase (oligoclase and two generations of andesine), groundmass andesine microlites, pyroxenes (augite and diopside), Ca-amphiboles (edenite and pargasite), and Mg-biotite. Our findings indicate that plagioclase crystallization occurred under conditions analogous to those found in island arcs and active continental margins, characterized by high oxygen fugacity (logfO2=-5.04 to -6.86), temperatures ranging from 1090°C to 1124°C, and pressures decreasing from 12 to 4,5 kbar. These data support the hypothesis that subducted oceanic crust from the Mongol-Okhotsk Basin contributed to the Mesozoic Aldan magmatic sources. Furthermore, the identified P-T depth intervals (36–24, 24–12, 12–6, and 6–2 km) suggest the presence of intermediate Mesozoic magma chambers. Finally, an assessment of amphibole and biotite typomorphism, combined with the geological evolution of the andesites, indicates a high potential for epithermal gold mineralization in the region.

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