Plio-Quaternary Volcanism in Italy [electronic resource] : Petrology, Geochemistry, Geodynamics / by Angelo Peccerillo.
Material type: TextPublisher: Berlin, Heidelberg : Springer Berlin Heidelberg, 2005Description: XIV, 365 p. online resourceContent type: text Media type: computer Carrier type: online resourceISBN: 9783540290926Subject(s): Earth sciences | Geochemistry | Geology | Mineralogy | Geophysics | Earth Sciences | Geology | Geochemistry | Geophysics and Environmental Physics | Geophysics/Geodesy | MineralogyAdditional physical formats: Printed edition:: No titleDDC classification: 551 LOC classification: QE1-996.5Online resources: Click here to access onlineItem type | Current library | Call number | Status | Date due | Barcode |
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e-Books | Bangalore University Library | Available | BUSP001593 |
Plio-Quaternary Magmatism in Italy: An Introductory Overview -- The Tuscany Province -- The Intra-Apennine Province -- The Roman Province -- The Ernici-Roccamonfina Province -- The Campania Province, Pontine Islands, and Mount Vulture -- The Aeolian arc -- The Sicily Province -- Sardinia and the Southern Tyrrhenian Sea -- Petrogenesis and Geodynamics in Italy.
Central-Southern Italy and the Tyrrhenian Sea are the sites of extensive Plio-Quaternary magmatic activity. The rock compositions include crustal anatectic granites and rhyolites, tholeiitic, calc-alkaline, shoshonitic volcanics, and potassic to ultrapotassic and Na-alkaline volcanics. This very wide compositional variation makes Italian magmatism one of the most complex petrological issues, the understanding� of which is a challenge for modern petrology and geochemistry. This book summarises the petrological, geochemical and volcanological characteristics of�Italian Plio-Quaternary volcanism, and discusses petrogenetic hypotheses and possible geodynamics settings. The book is written for petrologists and geochemists, but�fundamental�geochemical information is�well presented and the use of excessive jargon is avoided,� making the book readable to a wide audience of Earth scientists.
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