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VDM Verlag Geologie des Betancuria Massivs auf Fuerteventura, Kanarische Inseln: Eine geologische Geländeuntersuchung des plutonischen Basalkomplexes und basaltischen Gangschwarms nördlich von Pájara

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Description

Die Kanarischen Inseln gehören zusammen mit den Azoren, Madeira, Selvagens und Kapverden zu den mittelatlantischen Vulkaninseln. Der vorwiegend vulkanische Aufbau der Kanaren erfolgte im Wesentlichen in drei Phasen: der sogenannten Prä-Schild-Phase, gefolgt von der Schild-Phase und abschließend der Post-Schild-Phase. Während auf den meisten Inseln jüngerer Magmatismus bis heute dominiert (rezent submarin nahe El Hierro), zeichent sich Fuerteventura zusätzlich durch die geologische Archivierung des ältesten aktiven Vulkanismus vor mehr als 65 Millionen Jahren aus. Dies formte den um die Ortschaft Pájara aufgeschlossenen Basalkomplex. Die hier vorgelegte Arbeit umfasst eine detaillierte geologische Geländeuntersuchung einschließlich geologischer Kartierung innerhalb dieses Basalkomplexes. Sie eignet sich als Basis für weitere geologische Untersuchungen, aber auch als geologischer Führer für den interessierten Laien. About the Author Paul R. Eizenhöfer graduierte 2010 als Diplom Geologe an der Ruprecht-Karls-Universität Heidelberg. Seitdem promoviert er an der Universität Hong Kong. Sein derzeitiger Forschungsschwerpunkt liegt in der Rekonstruktion der geologischen Entwicklung Nordchinas.

Product Specifications

Format
paperback
Domain
Amazon UK
Release Date
07 December 2011
Listed Since
12 December 2011

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