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Relevant bibliographies by topics / San Leucio (Italy)

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Academic literature on the topic 'San Leucio (Italy)'

Author: Grafiati

Published: 27 July 2024

Last updated: 31 July 2025

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Journal articles on the topic "San Leucio (Italy)"

1

Stoppa, F., and A. Cundari. "Origin and multiple crystallization of the kamafugite-carbonatite association: the San Venanzo-Pian di Celle occurrence (Umbria, Italy)." Mineralogical Magazine 62, no. 2 (1998): 273–89. http://dx.doi.org/10.1180/002646198547530.

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AbstractThe Late Pleistocene kamafugite–carbonatite association at San Venanzo-Pian di Celle forms part of the Umbria-Latium Ultra-alkaline District (ULUD) of central Italy and, together with Toro-Ankole, SW Uganda and Mata de Corda, Brazil, represents one of three similar occurrences so far reported worldwide.Excellent field exposure and stratigraphic control prompted a study of the kamafugite–carbonatite suite and related phase interactions to understand the nature of the distinct mineral assemblages of the pyroclasts, compared to that of the lavas, the former containing essential potassium

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2

Innocenzi, Francesca, Isra S. Ezad, Sara Ronca, Samuele Agostini, Michele Lustrino, and Stephen F. Foley. "Experimental petrology constraints on kamafugitic magmas." European Journal of Mineralogy 36, no. 5 (2024): 899–916. http://dx.doi.org/10.5194/ejm-36-899-2024.

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Abstract. Kamafugites are rare volcanic igneous rocks, characterized by the presence of kalsilite and variable amounts of leucite, nepheline, melilite, clinopyroxene, olivine and phlogopite, which may not necessarily be present all together. Kamafugites are silica-poor (moderately ultrabasic to basic), CaO- and alkali-rich (mostly ultrapotassic) lithologies, generated from strongly metasomatized and heterogeneous mantle sources, with abundant phlogopite and little or no orthopyroxene. Melting of phlogopite- and carbonate-bearing veins is often invoked as being responsible for the ultrapotassic

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Pretese, Roberta, Cristina Bonfanti, Martha Caterina Faraguna, et al. "The Impact of Diet on Body Composition in a Cohort of Pediatric and Adult Patients with Maple Syrup Urine Disease." Nutrients 16, no. 18 (2024): 3145. http://dx.doi.org/10.3390/nu16183145.

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The treatment for Maple Syrup Urine Disease (MSUD) consists of a hypoproteic diet with integration therapy to limit leucine intake, ensuring adequate energy, macronutrients, and micronutrients to prevent catabolism and promote anabolism. We conducted a retrospective cross-sectional study at the Metabolic Rare Disease Unit, Fondazione IRCCS San Gerardo dei Tintori, Monza, Italy. Patients with MSUD who were over 3 years old, not treated with liver transplantation, and who provided written consent, were included. The study aimed to describe the dietary treatment of patients with MSUD, evaluate gr

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4

Cringoli, Gerardo, and Andrea Pomella. "San Leucio, the utopian social labor experiment in the pre-unification Southern Italy." Labor History, April 2, 2024, 1–14. http://dx.doi.org/10.1080/0023656x.2024.2338296.

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5

"Preface." Journal of Physics: Conference Series 2439, no. 1 (2023): 011001. http://dx.doi.org/10.1088/1742-6596/2439/1/011001.

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Selected papers from the 25th edition of the International Conference on Spectral Line Shapes (ICSLS 2022) The 25th edition of the International Conference on Spectral Line Shapes (ICSLS 2022) was held inside the wonderful Monumental Complex of Belvedere di San Leucio, in Caserta, south of Italy, from 19 to 24 June 2022. Initially scheduled for June 2020, it was postponed by two years due to the COVID-19 pandemic. ICSLS 2022 has brought together, in person, researchers from universities and institutions to stimulate new activities in those fields in which the analysis of spectral line shapes i

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6

Lustrino, Michele, Sara Ronca, Antonio Caracausi, Bordenca Claudio Ventura, Samuele Agostini, and Davide Benedetto Faraone. "Strongly SiO2-undersaturated, CaO-rich kamafugitic Pleistocene magmatism in Central Italy (San Venanzo volcanic complex) and the role of shallow depth limestone assimilation." June 26, 2020. https://doi.org/10.1016/j.earscirev.2020.103256.

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The Pleistocene (~460–265 ka) San Venanzo volcanic complex belongs to the IAP (Intra-Apennine Province) in central Italy, which comprises at least four small Pleistocene monogenetic volcanoes plus several unrooted pyroclastic deposits with peculiar mineralogical and whole-rock chemical compositions. San Venanzo products are strongly SiO<sub>2</sub>-undersaturated, CaO- and MgO-rich and show ultrapotassic serial character. The relatively common occurrence of calcite in the pyroclastic rocks and the overall high CaO content are interpreted in literature as primary miner

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7

Novembre, Daniela, Domingo Gimeno, Monia Calista, Vania Mancinelli, and Enrico Miccadei. "On the suitability of phillipsite-chabazite zeolitite rock for ammonia uptake in water: a case study from the Pescara River (Italy)." Scientific Reports 12, no. 1 (2022). http://dx.doi.org/10.1038/s41598-022-13367-y.

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AbstractIonic exchange tests have been performed on superficial wastewaters to remove ammonia using a volcanic zeolitized rock from Lazio Region (Central Italy). The zeolitite (natural zeolite) is characterized by chabazite, phillipsite and minor amounts of sanidine, leucite and analcime. After preliminary column experiments in laboratory focused to determine the saturation time of the zeolitite, a pilot plant was built up on a little water course near the area of San Giustino channel (Abruzzo Region, Central Italy). Wastewaters, characterized by starting ammonia value ranging between 5 and 12

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Books on the topic "San Leucio (Italy)"

1

Narciso, Giuseppina. The Belvedere of San Leucio. Colonnese editore, 2019.

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2

Il codice delle leggi leuciane: Atti del convegno, Caserta 27 maggio 2005. Saletta dell'uva, 2006.

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Book chapters on the topic "San Leucio (Italy)"

1

Ciano, Marco, Ebrahim Aminifar, Corrado Chisari, et al. "Structural Features of San Leucio Historical Site in Caserta, Italy." In Lecture Notes in Civil Engineering. Springer Nature Switzerland, 2025. https://doi.org/10.1007/978-3-031-87316-4_71.

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