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Ventruti, G., Caggianelli, A., Festa, V., and Langone, A. (2020) Crystal chemistry of barian titanian phlogopite from a lamprophyre of the Gargano Promontory (Apulia, Southern Italy). Minerals, 10(9), 766.
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Avanzinelli, R., Sapienza, G. T., & Conticelli, S. (2012). The Cretaceous to Paleogene within-plate magmatism of Pachino-Capo Passero (southeastern Sicily) and Adria (La Queglia and Pietre Nere, southern Italy): geochemical and isotopic evidence against a plume-related origin of circum-Mediterranean magmas. European Journal of Mineralogy, 24(1), 73-96.
Russo, M. (2008): I minerali delle Vulcaniti di Punta delle Pietre Nere nel Gargano (Lesina, Foggia, Italy). MICRO (località). Periodico dell'Associazione Micro-mineralogica Italiana, 2008(2). 227-244.
De Astis, G., Kempton, P. D., Peccerillo, A., & Wu, T. W. (2006). Trace element and isotopic variations from Mt. Vulture to Campanian volcanoes: constraints for slab detachment and mantle inflow beneath southern Italy. Contributions to Mineralogy and Petrology, 151(3), 331-351.
Bigazzi, G., Laurenzi, M. A., Principe, C., & Brocchini, D. (1996). New geochronological data on igneous rocks and evaporites of the Pietre Nere Point (Gargano Peninsula, southern Italy). Bollettino della Societa Geologica Italiana, 115(2), 439-448.
De Fino, M., La Volpe, L., & Piccarreta, G. (1983). Mafic minerals from Punta delle Pietre Nere subvolcanites (Gargano, Southern Italy): their petrological significance. Tschermaks mineralogische und petrographische Mitteilungen, 32(1), 69-78.
De Fino, M., La Volpe, L., & Piccarreta, G. (1982). Crystallization trends of pyroxenes from alkaline subvolcanites of Punta delle Pietre Nere (Gargano, Southern Italy). Tschermaks mineralogische und petrographische Mitteilungen, 29(3), 177-192.
de Fino, M., La Volpe, L., & Piccarreta, G. (1981). Geochemistry and petrogenesis of the Paleocene platform magmatism at Punta delle Pietre Nere (Southeastern Italy). Neues Jahrbuch für Mineralogie. Abhandlungen, 142(2), 161-177.
Hawkesworth, C. J., & Vollmer, R. (1979). Crustal contamination versus enriched mantle: 143 Nd/144 Nd and 87 Sr/86 Sr evidence from the Italian volcanics. Contributions to Mineralogy and Petrology, 69(2), 151-165.
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