Аннотация
The paper describes indicator minerals of kimberlites found on the southern side of the Vilyui syneclise in the Markha River basin, a tributary of the Lena River. It is shown that indicator minerals—pyrope and picroilmenite—derive from Middle Paleozoic kimberlites, very likely diamondiferous. Methods are proposed for further studies on determining the prospects for the diamond content of the southern side of the Vilyui syneclise and the northern slope of the Aldan anteclise.
Язык оригинала | английский |
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Страницы (с-по) | 535-541 |
Число страниц | 7 |
Журнал | Geology of Ore Deposits |
Том | 62 |
Номер выпуска | 6 |
DOI | |
Состояние | Опубликовано - ноя 2020 |