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Fault-blocky structure of the Moho boundary under the central part of the Donets folded structure (along the line of the seismic profile DOBREflection2000)

A possibility to reconstruct the fault-blocky structure of geological objects according to the results of solving the inverse dynamic problem of seismic is under consideration in the paper. The initial are seismic data of the deep section of CDP obtained by SGE «Ukrgeophysics», on the profile DOBRE...

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Autor principal: D.M. Gryn
Formato: Artigo
Lenguaje:Inglês
Publicado: Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine 2020-11-01
Colección:Геофизический журнал
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Acceso en línea:https://journals.uran.ua/geofizicheskiy/article/view/215083
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