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Lateral extrusion of a thermally weakened pluton overburden (Campiglia Marittima, Tuscany)

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Abstract

The ascent and emplacement of magmas in the upper crust modify the local pre-existing thermal and rheological settings. Such changes have important effects in producing anomalous structures, mass extrusion, rock fracturing, and in some conditions, hydrothermal mineralizations. In the Campiglia Marittima area, detailed field mapping led to the reconstruction of a local deformation history that overlaps, chronologically and spatially, with regional extension. This local deformation was triggered at the Miocene–Pliocene boundary by the intrusion of a monzogranitic pluton beneath a carbonate sedimentary sequence. The emplacement of the pluton produced a perturbation in the rheological behaviour of the carbonate host rocks, producing transient ductile conditions in the very shallow crust. The carbonate rocks were thermally weakened and flowed laterally, accumulating downslope of the pluton roof, mainly toward the east. As the thermal anomaly was decaying, the brittle–ductile boundary moved progressively back towards the pluton, and large tension gash-shaped volumes of fractured marble were generated. These fractured volumes were exploited by rising hydrothermal fluids generating sigmoidal skarn bodies and ore shoots. This work presents the Campiglia Marittima case study as a prime example of structural interference between regional extensional structures and local, lateral mass extrusion in a transient ductile rheological regime triggered by pluton emplacement.

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Acknowledgements

This work has been partly carried out as part of the Ph.D of SV, in the framework of the Ph.D program of the Galileo Galilei School, University of Pisa, with the support of the Project PRA_2016_33, P.I. SR. Thanks to Luca Tinagli, Marco Pistolesi and Angiolo Fedeli for their help during field surveys. We also thank the Parchi Val di Cornia S.p.A. for granting access and sampling in the mining park area. The paper greatly benefited from the constructive criticism of the two reviewers Andrea Brogi and David Westerman.

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Vezzoni, S., Rocchi, S. & Dini, A. Lateral extrusion of a thermally weakened pluton overburden (Campiglia Marittima, Tuscany). Int J Earth Sci (Geol Rundsch) 107, 1343–1355 (2018). https://doi.org/10.1007/s00531-017-1539-9

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