1887

Abstract

The basic features of a structure of the Riphean sedimentary rocks in the edge of Kaltasynsky aulacogene and their oil-and-gas content are considered. The transformants of the gravity field reflecting a density structure of the Riphean sedimentary rocks are constructed. Zones of «decrease of density», presumably bound with areas of sedimentary rocks burial that have good reservoir properties are detected.

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/content/papers/10.3997/2214-4609.20146878
2008-04-07
2020-03-31
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