Пенолиты – новый тип эндогенных горных пород (о. Бельковский, Россия)

V. I. Silaev, V. F. Proskurnin, I. I. Golubeva, D. N. Remizov, V. N. Filippov, V. P. Lyutoev, Yu. S. Simakova

Аннотация


Обобщены результаты комплексного изучения шлакоподобного сидеритолита – представителя ранее неизвестного генетического типа горных пород. Исследованы наномикроструктурные особенности, химический состав, микроэлементы, конституция и спектроскопические свойства породообразующих и акцессорных минералов. С использованием минералого-онтогенического метода расшифрована история образования породы, сделан вывод о том, что шлакоподобный сидеритолит может быть определен как представитель нового генетического типа эндогенных горных пород – пенолитов, образующихся непосредственно в пузыристой пене.

Ключевые слова


архипелаг Анжу; о. Бельковский; палеогеновая пачка туффитов; шлакоподобный сидеритолит; наномикроструктурные; минералого-геохимические; спектрскопические и минералого-онтогенические свойства; пенолиты

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Литература


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DOI: http://dx.doi.org/10.17072/psu.geol.18.2.125

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