Всероссийский научно-исследовательский геологический институт им. А. П. Карпинского, Санкт-Петербург, Россия¹ ; Санкт-Петербургский горный университет императрицы Екатерины II, Санкт-Петербург, Россия² ; Северо-Восточный комплексный научно-исследовательский институт им. Н. А. Шило ДВО РАН, Магадан, Россия³

Касаткин Н. С., ведущий инженер¹, аспирант², младший научный сотрудник³, kasatikg@gmail.com

Всероссийский научно-исследовательский геологический институт им. А. П. Карпинского, Санкт-Петербург, Россия
Аленичева А. А., старший научный сотрудник

Юрченко Ю. Ю., начальник отдела, канд. геол.-минерал. наук

Санкт-Петербургский горный университет императрицы Екатерины II, Санкт-Петербург, Россия
Таловина И. В., зав. кафедрой, проф., д-р геол.-минерал. наук

Приведены новые данные о минеральном составе и геохимических особенностях молибден-медно-порфировой минерализации рудного поля Павловича (Северное Приохотье, Магаданская обл.). Оруденение рудного поля Павловича приурочено к одноименному плутону альб-сеноманских гранитоидов Приохотского плутонического пояса и выражено широко развитыми зонами вторичных кварцитов, ортоклазитов, окварцевания, кварц-сульфидного прожилкования с молибденитом, с вкрапленностью молибденита и гипергенными минералами меди. Авторы считают проявление Павловича перспективным для выявления среднего молибден-медно-порфирового месторождения и рекомендуют проведение поисковых работ.

Исследования выполнены в рамках Государственных заданий Федерального агентства по недропользованию от 14.01.2022 г. № 049–00018–22–01 по объекту «Создание и подготовка к изданию государственной геологической карты масштаба 1:1 000 000 третьего поколения по группе листов территории Российской Федерации в 2021–2023 годах (листы О-55, 56)» и СВКНИИ ДВО РАН «Разработка критериев рудоносности магматических комплексов» № 124051600003–4.

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