
doi: 10.1007/bf01824906
Die Banater Erzprovinz ist eine der altberuhmten und auserst interessanten Erzzonen Europas. Die vorliegende Arbeit stellt einen ersten Versuch einer »seismo-tektonomagmatischen« Klassifizierung nach Bewegungszonen und den daran gebundenen Magmatismus der Banater Erzlagerstatten dar. Dabei werden auch plattentektonische Prozesse berucksichtigt, welche diesen karpatischen Raum gepragt haben.
550.geology, Article
550.geology, Article
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