Abstract
Summary The Yenisei-Khatanga trough, framing the structure of Gorny Taimyr from the south and separating Taimyr from the Siberian platform, is made by the Mesozoic-Cenozoic (plate) complex. On the sides, the complex lies subhorizontal with structural unconformity on the Paleozoic underlying rocks. And in the most submerged zones, a Permian-Triassic volcanic complex appears, which is also comparable to the trap fields of the Putorana and Taimyr, but sharply increased in thickness and indicates a possible major stage in the rift development of the Yenisei-Khatanga trough.
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