Abstract
Elba Island intrusive complex: multisheet laccoliths, sheeted pluton, mafic dyke swarm. Laccolith magma fed from dykes and emplaced in crustal discontinuities (traps). Pluton growth by downward stacking of three magma pulses. Laccoliths and plutons: different outcomes of similar processes in different conditions. Emplacement of excess magma in a short time led to massive gravity slide.
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Westerman, D.S., Rocchi, S., Dini, A., Farina, F., Roni, E. (2015). Rise and Fall of a Multi-sheet Intrusive Complex, Elba Island, Italy. In: Breitkreuz, C., Rocchi, S. (eds) Physical Geology of Shallow Magmatic Systems. Advances in Volcanology. Springer, Cham. https://doi.org/10.1007/11157_2014_5
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DOI: https://doi.org/10.1007/11157_2014_5
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