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http://hdl.handle.net/2122/6482
DC Field | Value | Language |
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dc.contributor.authorall | Callegari, A.M.; Dipartimento di scienze della terra, Università di Pavia, Italy | en |
dc.contributor.authorall | Boiocchi, M.; Centro Grandi Strumenti, Università di Pavia, Italy | en |
dc.contributor.authorall | Bellatreccia, F.; Dipartimento di Scienze Geologiche, Università di Roma Tre, Italy | en |
dc.contributor.authorall | Caprilli, E.; Dipartimento di Scienze Geologiche, Università di Roma Tre, Italy | en |
dc.contributor.authorall | Medenbach, O.; Institute of Geology, Mineralogy and Geophysics, Ruhr-Universitat Bochum, Germany | en |
dc.contributor.authorall | Cavallo, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.date.accessioned | 2010-12-30T11:27:01Z | en |
dc.date.available | 2010-12-30T11:27:01Z | en |
dc.date.issued | 2010-08-21 | en |
dc.identifier.uri | http://hdl.handle.net/2122/6482 | en |
dc.description.abstract | Capranicaite, ideally KCaNaAl4B4Si2O18, is a new mineral recently approved by the IMA CNMNC (case no. 2009-086) found in the Vico volcanic complex at Capranica, Viterbo, Italy. Capranicaite occurs in miarolitic cavities of a feldspathoid-bearing syenite ejectum probably formed during late-stage metasomatic processes related to volcanic activity. Capranicaite forms small, tabular crystals no longer than 0.1 mm. Crystals are colourless, with a white streak and a vitreous lustre; they are not fluorescent and have a good {001} cleavage. Capranicaite is biaxial (-) with α = 1.495(1), β = 1.543(1), γ = 1.544(1); 2V(obs) = 7.3(2)°. Capranicaite is monoclinic, space group P21/n, a = 4.8507(2), b = 16.6156(6), c = 20.5445(7) Å, β = 90.245(1)°, V = 1655.82(17) Å3, Z = 4. Electron microprobe analysis gives: SiO2 20.70, Al2O3 32.91, B2O3 22.90, K2O 5.36, CaO 11.04, Na2O 4.08, Cs2O 2.20, sum 99.19%. Calculated density is 2.41 gcm-3. The formula unit, calculated on the basis of 18 O, is (K0.69Cs0.10)Ʃ0.79(Ca1.19Na0.80)Ʃ1.99Al3.91B3.99Si2.09O18. Capranicaite is a Cs bearing inosilicate with a new topological arrangement of the 2-periodic Si2O6 single chains. The crystal structure of capranicaite consists of three overlapping layers of polyhedra (A, B, and C) normal to c. The A-layer contains the Si2O6 chains that extend along a. Respect than pyroxene, in capranicaite the Si-tetrahedra are rotated and the Si2O6 groups do not have two apical oxygens pointing towards the same direction. The B-layer is built by isolated AlO4 tetrahedra and BO3 triangles connected to form a continuous sheet of six-fold rings (3Al + 3B). Two B-layers are connected to a single sandwiched A-layer to forms a bi-dimensional B-A-B network. The B-A-B networks contain seven fold cavities not completely populated by K and minor Cs. Adjacent B-A-B bi-dimensional networks are linked together via the C-layer, constituted by isolated octahedra with a mixed (Ca,Na) population. Along c the sequence of layer results C-B-A-B-C-B-A-B-C. | en |
dc.language.iso | English | en |
dc.relation.ispartof | IMA 2010 | en |
dc.subject | Capranicaite | en |
dc.subject | Capranica | en |
dc.title | Capranicaite: a new mineral from Capranica, Viterbo, Italy | en |
dc.type | Poster session | en |
dc.description.status | Unpublished | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology | en |
dc.description.ConferenceLocation | Budapest, Hungary | en |
dc.description.obiettivoSpecifico | 2.3. TTC - Laboratori di chimica e fisica delle rocce | en |
dc.description.fulltext | open | en |
dc.contributor.author | Callegari, A.M. | en |
dc.contributor.author | Boiocchi, M. | en |
dc.contributor.author | Bellatreccia, F. | en |
dc.contributor.author | Caprilli, E. | en |
dc.contributor.author | Medenbach, O. | en |
dc.contributor.author | Cavallo, A. | en |
dc.contributor.department | Dipartimento di scienze della terra, Università di Pavia, Italy | en |
dc.contributor.department | Centro Grandi Strumenti, Università di Pavia, Italy | en |
dc.contributor.department | Dipartimento di Scienze Geologiche, Università di Roma Tre, Italy | en |
dc.contributor.department | Dipartimento di Scienze Geologiche, Università di Roma Tre, Italy | en |
dc.contributor.department | Institute of Geology, Mineralogy and Geophysics, Ruhr-Universitat Bochum, Germany | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
item.openairetype | Poster session | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Univ Pavia, Dipartimento Sci Terra, I-27100 Pavia, Italy | - |
crisitem.author.dept | Univ Pavia, Ctr Grandi Strumenti, I-27100 Pavia, Italy | - |
crisitem.author.dept | Università Roma Tre | - |
crisitem.author.dept | Univ Roma Tre, Dipartimento Sci Geol, I-00146 Rome, Italy | - |
crisitem.author.dept | Institute of Geology, Mineralogy and Geophysics, Ruhr-Universitat Bochum, Germany | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Conference materials |
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File | Description | Size | Format | |
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Poster capranicaite FB.pdf | 227.58 kB | Adobe PDF | View/Open |
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