Abstract
A new interpretation of the geological and seismic data demonstratd a correlation between the surface structures of endogenic ore regions of the Baltic Shield, the Moho surface relief, and local heterogeneities in the Earth’s crust. As a result, based on consistent analysis of the geological and seismic data, models of the deep structure of the Pechenga and Onega ore regions were constructed and compared.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
