gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2023-14-2-0691gtcrust-1662Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSПЕТРОХИМИЧЕСКИЕ И СТРУКТУРНЫЕ ХАРАКТЕРИСТИКИ МЕДНО-ПОРФИРОВОГО ОРУДЕНЕНИЯ В РУДОПРОЯВЛЕНИИ АСТАНЕ СРЕДНЕЙ ЧАСТИ МАГМАТИЧЕСКОЙ ДУГИ УРУМИЕ-ДОХТАР (ИРАН)PETROCHEMICAL AND STRUCTURAL CHARACTERISTICS OF PORPHYRY COPPER MINERALIZATION IN THE ASTANEH ORE DEPOSIT, MIDDLE PART OF THE URUMIEH-DOKHTAR MAGMATIC ARC (IRAN)https://orcid.org/0000-0002-0391-3863БейгиС.BeygiS.

199106, Санкт-Петербург, Васильевский остров, 21 линия, 2

2 21st Line, Saint Petersburg 199106

https://orcid.org/0000-0001-7944-8366ТадаёнМ.TadayonM.

8174673441, Исфахан, площадь Азади

Azadi Sq, Isfahan 817467341

https://orcid.org/0000-0003-2241-3239ИлаловаР. К.IlalovaR. K.

199106, Санкт-Петербург, Васильевский остров, 21 линия, 2

2 21st Line, Saint Petersburg 199106

https://orcid.org/0000-0003-4132-7010ТаловинаИ. В.TalovinaI. V.

199106, Санкт-Петербург, Васильевский остров, 21 линия, 2

2 21st Line, Saint Petersburg 199106

https://orcid.org/0000-0001-5572-3212МейшелТ. С.MeiseT. C.

A-8700, Леобен, Франц-Йозеф-Штрассе 18

18 Franz-Josef-Straße, Leoben A-8700

Санкт-Петербургский горный университетРоссияSaint Petersburg Mining UniversityRussian FederationИсфаханский университетИранUniversity of IsfahanIslamic Republic of IranЛеобенский горный университетАвстрияMontanuniversität LeobenAustria202319042023142691691Copyright © Бейги С., Тадаён М., Илалова Р.К., Таловина И.В., Мейшел Т.С., 20232023Бейги С., Тадаён М., Илалова Р.К., Таловина И.В., Мейшел Т.С.Beygi S., Tadayon M., Ilalova R.K., Talovina I.V., Meise T.C.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/1662

В пределах магматической дуги Уромие-Дохтар в центральной части Ирана, образование которой связано с закрытием Неотетиса, расположено множество медно-порфировых месторождений и рудопроявлений. Одно из них – медно-порфировое рудопроявление Астане, которое находится в центральной части рудного района Саве-Ардестан, расположенного юго-западнее г. Ардестан. Целью данного исследования является изучение петрохимических характеристик горных пород и определение взаимосвязи между распределением меднопорфирового оруденения и положением тектонических разломов в пределах изучаемой территории. Для достижения цели были использованы структурно-геологические и минералого-геохимические данные, полученные как в ходе проведения полевых работ, так и по результатам лабораторных исследований. Результаты исследования доказывают, что разнообразные по составу горные породы рудопроявления Астане (андезит, андезибазальт, базальт, трахибазальт) сформировались в надсубдукционной зоне и, вероятно, в обстановке, предшествовавшей столкновению континентальных плит. Парагенетические связи и минералогический анализ показали, что эволюция минерализации рудопроявления Астане может быть разделена на три этапа: дорудный, рудный и гипергенный. Геохимические исследования, основанные на изучении содержания главных химических элементов в породах района, определяют, что магматические породы относятся к известково-щелочным базальтам и со стороны геодинамической обстановки могут быть отнесены к продуктам магматизма континентальной островной дуги энсиалического типа. В результате изучения был сделан вывод о том, что основные этапы формирования медно-порфирового рудопроявления на исследуемой территории демонстрируют максимальное временное и пространственное сходство с тектономагматическими фазами развития океана Неотетис. Кроме того, разлом Южный Ардестан, проходящий через изучаемую территорию и секущий структуры фундамента, образует широкие проницаемые зоны, благоприятные для формирования медно-порфировых рудопроявлений.

Within the Urumieh-Dokhtar Magmatic Arc in the central part of Iran, the formation of which is associated with the Neotethys closure, there are many porphyry copper deposits and ore occurrences. One of them is the Astaneh porphyry copper ore deposit, located in the central part of the Saveh-Ardestan ore region southeast of Ardestan city. The purpose of this study is to investigate the petrochemical characteristics of rocks and to determine the relationship between the distribution of porphyry copper mineralization and tectonic position of faults within the study area. To achieve the goal, there were used the structural and geological data obtained in the fieldwork, as well as the results of mineralogical and geochemical analyses. The obtained results show that rocks of different composition of the Astaneh ore deposit (andesite, andesite-basalt, basalt, trachybasalt) were formed in the suprasubduction zone, and probably in the environment prior to the collision of the of continental plates. Paragenetic relationships and mineralogical analysis show that the evolution of mineralization of the Astaneh ore deposit can be divided into three stages: pre-ore, hypogene and supergene mineralization. Geochemical research based on the study of the content of the major chemical elements in the rocks of the region shows that igneous rocks belong to calc-alkaline basalts and geodynamically can be attributed to the products of magmatism of the ensial island arc. The results concluded that the main stages of the formation of a porphyry copper ore deposit in the study area attain maximum spatio-temporal similarity with the tectonomagmatic phases of the development of the Neotethys Ocean. In addition, the Southern Ardestan fault, running through the study area and intersecting the basement structures, forms wide permeable zones favorable for the formation of porphyry copper deposits therein.

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