- Код статьи
- S30345073S0016777025030053-1
- DOI
- 10.7868/S3034507325030053
- Тип публикации
- Статья
- Статус публикации
- Опубликовано
- Авторы
- Том/ Выпуск
- Том 67 / Номер выпуска 3
- Страницы
- 337-375
- Аннотация
- Sn(-Cu) район Там Дао расположен на южном окончании Южно-Китайского блока в пределах структуры Ло Гам северо-восточного Вьетнама. Генетически рудная минерализация района Там Дао ассоциирована с одноименным массивом биотитовых гранитов среднетриасового возраста комплекса Пиа Биок и объединяет большое количество месторождений и рудопроявлений. Одним из наиболее крупных и изученных является месторождение Нгой Лем (4700 т Sn и 300 т Cu). Несмотря на широкое распространение гранитоидного магматизма ранне-среднетриасового возраста в структуре Ло Гам, оловорудная минерализация выявлена только в ореоле массива Там Дао и практически не проявляется в связи с другими массивами комплекса. Анализ геохимических характеристик цирконов (содержание РЗЭ, Ti, U) из биотитовых гранитов различных массивов свидетельствует о близости величины фугитивности кислорода и степени фракционирования родоначальных расплавов. Установленные характеристики в полной мере согласуются с генетическими моделями формирования оловорудных месторождений в связи с восстановленными интрузиями. Дискретность металлогенического потенциала одновозрастных и геохимически близких гранитоидов объясняется условиями частичного плавления метаосадочного субстрата. Рудоносные биотитовые граниты массива Там Дао характеризуются более высокими температурами кристаллизации циркона (~>780-800°C), предполагающими формирование значительного объема выплавок в условиях безводного плавления с разложением биотита и вовлечением в область магмогенерации внешнего мантийного источника тепла. Взаимодействие базитовых и гранитоидных магм привело к обогащению кислых расплавов медью. Низкая фугитивность кислорода обуславливала доминирование сульфидной формы нахождения серы в расплавах, что, в свою очередь, определило низкую ее концентрацию. Низкое отношение S/Cu в гранитном расплаве препятствовало сульфидной сегрегации и удалению меди из расплава в виде сульфидов. Предложенный сценарий насыщения гранитного расплава медью и отсутствия значительного ее фракционирования в сульфидную фазу объясняет противоречивую Sn-Cu металлогению рудного района Там Дао. Обобщая полученные новые данные о геохимических характеристиках циркона из раннеи среднетриасовых гранитов комплекса Пиа Биок, представляется возможным сформулировать ключевые индикаторные характеристики цирконов, указывающие на потенциальную оловоносность восстановленных гранитов: (1) T~>780-800°C, (2) ΔFMQ
- Ключевые слова
- гранит оловорудное месторождение U-Pb-датирование циркон геохимия индикаторы фертильности Там Дао Северо-Восточный Вьетнам
- Дата публикации
- 21.12.2025
- Год выхода
- 2025
- Всего подписок
- 0
- Всего просмотров
- 62
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