Abstract

Emphasizes the role of interrupted ascent of mineralizing solutions (as a result of filling or reopening of fissures) in determining the zonal distribution of ore deposits, citing results of an investigation of vertical changes in ore veins of the Pribram district, Czechoslovakia.

Full Text
Published version (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