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Lucia Civetta

Researcher at University of Naples Federico II

Publications -  99
Citations -  5872

Lucia Civetta is an academic researcher from University of Naples Federico II. The author has contributed to research in topics: Volcanic rock & Volcano. The author has an hindex of 44, co-authored 97 publications receiving 5345 citations. Previous affiliations of Lucia Civetta include National Institute of Geophysics and Volcanology.

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Chemical and Sr-isotopical evolution of the Phlegraean magmatic system before the Campanian Ignimbrite and the Neapolitan Yellow Tuff eruptions

TL;DR: In this article, geochronological, geochemical, and Sr-isotope data on volcanics erupted before the Campanian Ignimbrite (CI, 37 ka) and the Neapolitan Yellow Tuff (NYT, 12 ka) caldera-forming eruptions at Campi Flegrei (CF) have allowed us to investigate the behavior and temporal evolution of the Phlegraean magmatic system.
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Short-term ground deformations and seismicity in the resurgent Campi Flegrei caldera (Italy): an example of active block-resurgence in a densely populated area

TL;DR: In this article, the authors performed an analysis of the ground deformation and seismic data collected since 1970 and showed that the detected deformation can be accounted for by an overpressure of 75 MPa in a source with a radius of 1 km, located at 5 km depth.
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Source contamination and mantle heterogeneity in the genesis of Italian potassic and ultrapotassic volcanic rocks: Sr–Nd–Pb isotope data from Roman Province and Southern Tuscany

TL;DR: In this article, the Tyrrhenian border of the Italian peninsula has been the site of intense magmatism from Pliocene to recent times, and a decrease of alkaline character in time and space (southward) is observed.
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The Geochemistry of Volcanic Rocks from Pantelleria Island, Sicily Channel: Petrogenesis and Characteristics of the Mantle Source Region

TL;DR: In this paper, a data set for mafic and felsic volcanic rocks from the island of Pantelleria is presented, where the major and trace element, Sr-Nd-Pb isotope and mineral chemical at least two distinct geochemical components: a mid-ocean ridge basalt (MORB) source, relatively depleted component, and a data are presented for MAFic and Felsic volcano.