Study of fine velocity structure of seismic boundaries in magmatic rocks of ore districts
Abstract
Despite the large volume of seismic exploration in ore areas is still poorly covered the question of the properties of seismic boundaries in igneous rocks. The information about them is based mainly on the results of interpretation of kinematic characteristics of wave fields, which give an opportunity to get a fairly complete idea about the morphology of boundaries, but very little - about their detailed velocity structure ...
Область исследования:
(Archived) Without section
Funding:
None
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