Detection of the connection of wave fields with the fine structure of seismic boundaries in magmatic rocks
Abstract
Based on detailed studies of elastic parameters of well cores in the Kafan ore field it is shown that the velocity section of magmatic rocks is represented mainly by layers of small thickness (up to 100 m), among which thin layers with a thickness of 10-20 m predominate ...
Область исследования:
(Archived) Without section
References
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