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Magmatic geochemistry and geochronology in relation to the geodynamic and metallogenic evolution of the Banat Region and the Apuseni Mountains of Romania [thesis]

Daniela Gallhofer, Christoph A. Heinrich, Albrecht Hans-Otto Franz Constanz Quadt Wykradt-Hüchtenbruck
2015

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The Apuseni-Banat-Timok-Srednogorie (ABTS) magmatic arc in southeastern Europe formed as a result of NE-dipping subduction of the Neotethys ocean beneath the European continental margin during the Late Cretaceous. This magmatic arc is associated with some of Europe's largest porphyry Cu-Au and epithermal Cu-Au deposits. However, the ore deposits
doi:10.3929/ethz-a-010579453 fatcat:k63cqpvrcvhsnnbd6agiy7mnty
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Daniela Gallhofer, Christoph A. Heinrich, Albrecht Hans-Otto Franz Constanz Quadt Wykradt-Hüchtenbruck. "Magmatic geochemistry and geochronology in relation to the geodynamic and metallogenic evolution of the Banat Region and the Apuseni Mountains of Romania." (2015)