Locality type: | Outcrop |
Classification |
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Species: | Baddeleyite |
Formula: | ZrO2 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Baddeleyite data |
Locality Data: | Click here to view Corigliano, Sessa Aurunca, Roccamonfina Volcanic Complex, Caserta, Campania, Italy |
Data Identifiers |
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Mindat Occurrence Record ID: | 538856 |
Long-form Identifier: | 1:3:538856:1 |
GUID (UUID V4): | 14babe32-78d5-4486-bae3-1e88b4a2f004 |
Nearest other occurrences of Baddeleyite |
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53.7km (33.4 miles) | ⓘTorregaveta, Bacoli, Naples, Campania, Italy |
58.4km (36.3 miles) | ⓘPozzo Vecchio, Procida Island, Naples, Campania, Italy |
62.5km (38.9 miles) | ⓘMontone Quarry, Ercolano, Mount Somma, Somma-Vesuvius Complex, Naples, Campania, Italy |
63.2km (39.3 miles) | ⓘSan Vito Quarry, San Vito, Ercolano, Mount Somma, Somma-Vesuvius Complex, Naples, Campania, Italy |
64.4km (40.0 miles) | ⓘTrapolino Quarry (Cava Nuova), Somma Vesuviana, Mount Somma, Somma-Vesuvius Complex, Naples, Campania, Italy |
64.5km (40.1 miles) | ⓘMount Somma, Somma-Vesuvius Complex, Naples, Campania, Italy |
64.6km (40.1 miles) | ⓘLagno Macedonia, Somma Vesuviana, Mount Somma, Somma-Vesuvius Complex, Naples, Campania, Italy |
93.1km (57.8 miles) | ⓘPunta della Guardia, Ponza Island, Ponza, Latina Province, Lazio, Italy |
References |
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Della Ventura, G., Williams, T. C., Raudsepp, M., Bellatreccia, F., Caprilli, E., Giordano, G. (2001) Perrierite-(Ce) and zirconolite from a syenitic ejectum of the Roccamonfina volcano (Latium, Italy): implications for the mobility of Zr, Ti and REE in volcanic environments. Neues Jahrbuch für Mineralogie - Monatshefte, 2001 (9) Schweizerbart. 385-402 |
Reference Search (possible matching items) |
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| | Journal (article/letter/editorial) | existence ofa dipositive mononuclear Ti hydroxyl complex in this pH range, as discussed below. Other experiments...noted significant Ti mobility. Under high T-low P (volcanic) conditions, in which the fluid phase has low...is probably present as a dipositive mononuclear complex, either TiO 2÷ or Ti (OH)2+, a conclusion supported...Lukachina, 1964) supports the presence of a neutral complex. Baes and Mesmer (1986) accepted this evidence...proposed that above pH 5.6 a negatively charged complex HTiO~becomes dominant; if true this would enhance | | | Book (volume) | Spain by F. Vazquez Guzman Portugal by D. Thadeu Italy by P. Zuffardi European part of the U.S.S.R. by...Southwest Europe embraces France, Spain, Portugal and Italy. Each volume has an introductory chapter of the...deposits Hercynian deposits Volcanogenic-sedimentary complex sulphide deposits . Volcanogenic-sedimentary manganese...Baixo Tejo and Sado Basins Silica sand deposits Italy by P. Zuffardi Introduction Geological setting Stratigraphy...province Alpidic plutonic sub-province . Alpidic volcanic sub-province . Alpidic tectonized, non-Alpidic |
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