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Geodynamics and evolution of the Miocene mineralization in the Cycladic - Pelagonian belt, Hellenides

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Γεωδυναμική και εξέλιξη των μειοκαινικών μεταλλοφοριών στο χώρο των Κυκλάδων και της Πελαγονίκης (EL)
Geodynamics and evolution of the Miocene mineralization in the Cycladic - Pelagonian belt, Hellenides (EN)
SKARPELIS, N.
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
2002-01-01
Δεν διατίθεται περίληψη (EL)
The paper aims to provide a sound account of the type of Miocene mineralisations in the Cycladic – Pelagonian belt and their relationship with the geodynamic evolution of the area. Skarn and manto types, epithermal precious and base metals mineralisation, and vein magnesite in ultramafics are associated to distinct stages of the geodynamic evolution of the belt. Extensional tectonics favoured their generation. Late stages of extensional tectonics resulted in the formation of vertical to subvertical NW-SE trending fault zones, which were then used as conduits for ascending hydrothermal fluids. The relationship between the geodynamics and the metallogenetic evolution of the belt is discussed on the basis of available data on the geology of four critical areas: Tinos and Mykonos islands, Laurium and Northern Euboea. (EN)
Cyclades (EN)
skarns (EN)
extension (EN)
Euboea (EN)
granitoids (EN)
manto (EN)
vein magnesite (EN)
epithermal mineralisation (EN)
Laurium (EN)
Late Miocene (EN)
Pelagonian (EN)
precious metals (EN)
Δελτίο της Ελληνικής Γεωλογικής Εταιρίας
English
Geological Society of Greece (EN)
0438-9557
2529-1718
Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Τόμ. 34 Αρ. 6 (2002): 9o διεθνές Συνέδριο της ΕΓΕ; 2191-2206 (EL)
Bulletin of the Geological Society of Greece; Vol. 34 No. 6 (2002): 9th International Conference of the Geological Society of Greece; 2191-2206 (EN)
https://creativecommons.org/licenses/by-nc/4.0
Copyright (c) 2018 N. SKARPELIS (EN)
Geological Society of Greece
Bulletin of the Geological Society of Greece
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