Other Mafic-Ultramafic Intrusions of the Chiney Intrusive Complex

Авторы: Bronislav Gongalsky, Nadezhda Krivolutskaya
Сборник: World-Class Mineral Deposits of Northeastern Transbaikalia, Siberia, Russia
Серия: Modern Approaches in Solid Earth Sciences
Том: 17
Глава в коллективной монографии
Год издания: 2019
Место издания: Springer Nature Switzerland AG
Первая страница: 243
Последняя страница: 256
DOI: 10.1007/978-3-030-03559-4_9
Аннотация: The mafic-ultramafic rocks occur on the periphery of the Kodar-Udokan basin. They belong to the Chiney Intrusive Complex. The largest bodies are the Chiney and Luktur plutons, as well as the Upper Sakukan and Mylovskiy layered mafic-ultramafic intrusions. Gabbronorite dikes also belong to the Chiney Complex, with the Main Udokan Dike (up to 200 m thick) being the largest. The geochemical and geophysical data indicate that outcrops of mafic and ultramafic rocks at the margins of the Lurbun granite-granodiorite pluton, which cuts through the Chiney pluton, also belong to the Chiney Complex.
Добавил в систему: Гонгальский Бронислав Иосифович

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