Interaction between Mid‐Ocean Ridge and Subduction Magmatism in Albanian Ophiolites

Albanian ophiolites are represented by two different coeval belts, each displaying well‐exposed, complete ophiolitic sequences that originated in the same oceanic basin and each showing distinct geochemical characteristics. The eastern belt is characterized by suprasubduction zone (SSZ) ophiolitic s...

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Veröffentlicht in:	The Journal of geology 2002-09, Vol.110 (5), p.561-576
Hauptverfasser:	Bortolotti, V., Marroni, M., Pandolfi, L., Principi, G., Saccani, E.
Format:	Artikel
Sprache:	eng
Schlagworte:	Andesite Basalt Chemical composition Geochemistry Geology Magma Magmatism Marine Melting Oceanography Plate tectonics Subduction Volcanology
Online-Zugang:	Volltext
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