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Geochemical and isotopic (Sr-Nd-Pb) signature of crustal contamination in Na-alkali basaltic magmas of South-East Turkey
Volume 141 (2022) f.3
Samuele Agostini1, Paolo Di Giuseppe1, Piero Manetti1,2, Mehmet Yılmaz Savaşçın3 & Sandro Conticelli2,4
Pages: 363-384
DOI: https://doi.org/10.3301/IJG.2022.21
Geochemical characterisation of the alkaline and hyperalkaline groundwater in the Othrys Ophiolite Massif, central Greece
Volume 140 (2021) f.1
Lorenza Li Vigni (1), Kyriaki DaskaLopoulou (2), Sergio Calabrese (1,3), Francesco Parello (1) & Walter D’Alessandro (3)
Pages: 42-56
DOI: https://doi.org/10.3301/IJG.2020.20
Late Cretaceous black shales from the Tuscan Sedimentary Succession (northern Tuscany, Italy): geochemistry and ore mineralogy
Volume 140 (2021) f.2
Massimo D’Orazio (1), Cristian Biagioni (1) & Daniele Mantovani (1)
Pages: 221-236
DOI: https://doi.org/10.3301/IJG.2020.30
Geochemical approach to the genesis of the Buyukkizilcik (Afsin) barite deposit, SE Turkey
Volume 140 (2021) f.3
Nevin Konakci (1) & Ahmet Sasmaz (1)
Pages: 422-437
DOI: https://doi.org/10.3301/IJG.2021.04
U-Pb ages on detrital zircons and geochemistry of Lula paragneiss from Variscan belt, NE Sardinia, Italy: implications for source rocks and early Paleozoic paleogeography
Volume 139 (2020) f.1
Gabriele Cruciani (1), Marcello Franceschelli (1), Valeria Caironi (2) & Giovanni Musumeci (3)
Pages: 131-148
DOI: https://doi.org/10.3301/IJG.2019.24
The Carboniferous-mid Permian successions of the Northern Apennines: new data from the Pisani Mts. inlier (Tuscany, Italy)
Volume 139 (2020) f.2
Federico Marini (1), Enrico Pandeli (1,2), Marco Tongiorgi (3), Elena Pecchioni (1) & Letizia Orti (1)
Pages: 212-232
DOI: https://doi.org/10.3301/IJG.2019.27
Geochemical survey of the Colpitas-Taapaca volcanic-hydrothermal system, northern Chile
Volume 139 (2020) f.3
Manuel Inostroza (1,2), Franco Tassi (3,4), José Sepúlveda (3), Francesco Capecchiacci (3), Andrea L. Rizzo (5) & Felipe Aguilera (2,6,7)
Pages: 359-373
DOI: https://doi.org/10.3301/IJG.2020.09