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Autor:
K. Yu. Sveshnikova, L. D. Tsvetkov, V. A. Krupenik, V. I. Gorbachev, Oleg Petrov, A. M. Akhmedov, A. F. Morozov, B. N. Khakhaev, G. V. Tarkhanov, Yu. M. Erinchek
Publikováno v:
Doklady Earth Sciences. 435:1483-1486
A thick (200 m) rock salt mass covering Late Archean granitoids was exposed for the first time in the Early Proterozoic volcanogenic-sedimentary formations in the Onega trough of the east Baltic Shield by the Onega parametric well. The mineral compos