Skip to main content
Log in

Potassium-fluor-richterite, a new amphibole from San Vito, Monte Somma, Campania, Italy

Potassium-fluor-nchterite, un nuovo anfibolo da San Vito, Monte Somma, Campania, Italia

  • Published:
Rendiconti Lincei Aims and scope Submit manuscript

Abstract

Potassium-fluor-richterite occurs as euhedral crystals, light-grey in colour, in a skarn ejectum from a pyroclastic deposit near S. Vito, Monte Somma, Naples. It is associated with diopside and calcite. The strongest X-ray diffraction lines are (d- spacing in Å): 3.166, 8.49, 3.288, 2.831, 1.918 and 1.633. The cell parameters (in Å, space groupC2/m) are:a = 9.978 (1);b = 17.991(2);c = 5.269 (1); ß(°) = 104.90 (2);V = 914.2 (3). Potassium-fluor-richterite is biaxial negative with (± 0.004) nX = 1.613; nY = 1.623; nZ = 1.630. The crystal-chemical formula is:

(K0.67Na0.34) (Ca1.09Na0.91) (Mg40.976Fe0.017Mn0.002) (Si7.94Al0.04Ti0.007) O22 (F1.35OH0.65).

The FTIR spectrum in the OH-stretching region is discussed.

Riassunto

La potassium-fluor-richterite si rinviene in proietti carbonatici metamorfosati e metasomatizzati contenuti in un deposito piroclastico affiorante vicino al Comune di S. Vito, Monte Somma, Napoli. È associata con diopside e calcite. I riflessi più intensi nello spettro misurato ai raggi X sono (distanze interplanari in Å): 3.166, 8.49, 3.288, 2.831, 1.918 e 1.633. I parametri di cella sono (in Å):a = 9.978 (1);b = 17.991 (2);c = 5.269 (1); ß(°)= 104.90 (2);V = 914.2 (3). La potassium-fluor-richterite è biassica negativa. Gli indici di rifrazione sono (± 0.004): nX = 1.613; nY = 1.623; nZ = 1.630. La formula cristallochimica è: (K0.67Na0.34) (Ca1.09Na0.91) (Mg40.976Fe0.017Mn0.002) (Si7.94Al0.04Ti0.007) O22 (F1.35OH0.65). Lo spettro FTIR nella regione di stiramento dell’OH viene discusso. mis|Nella seduta dell’8 febbraio 1992.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Appleman D. E., Evans H.T., 1963.Job 9214: Indexing and least-square refinement of powder diffraction data. Natl. Technl. Inf. Serv. U.S. Dep. Commerce, Springfield, Virginia, Document PB-216 188.

  • Barberi F., Leoni L., 1980.Metamorphic carbonate ejecta from Vesuvius plinian eruption: Evidence of the occurrence of a shallow magma chamber. Bull. Volcanol., 43: 107–120.

    Article  CAS  Google Scholar 

  • Cameron M., Sueno S., Papyke J. J., Prewitt C.T., 1983.High temperature crystal chemistry of K and Na flùor- richterites. Am. Min., 68: 924–943.

    CAS  Google Scholar 

  • Della Ventura G., Maras A., Parodi G. C., 1983.Potassium-fluorrichterite from Monte Somma (Campania)Italy. Per. Mineral., 52: 617–630.

    Google Scholar 

  • Della Ventura G., Robert J.-L., 1990.Synthesis, XRD and FTIR studies of strontium rich tentes. Eur. Journ. Min., 2: 171–175.

    Google Scholar 

  • Della Ventura G., Robert J.-L., Beny J.-M., 1991.Tetrahedrally coordinated Ti4 +in synthetic Ti-rich potassic nchtente: evidence from XRD, FTIR and Raman studies. Am. Min., 76: 1134–1140.

    Google Scholar 

  • HuebnerJ. S., Papike J.J., 1970.Synthesis and crystal chemistry of sodium-potassium richterite, (Na,K)NaCaMg 5 Si 8 0 22 (OH F) 2 :a model for amphiboles. Am. Min., 55: 1973–1992.

    Google Scholar 

  • Leake B., 1978.Nomenclature of amphiboles. Min. Mag., 42: 533–563.

    Article  CAS  Google Scholar 

  • Mandarino J.A., 1978.The Glandstone-Dale relationship. Part II: Trends among constants. Can. Min., 16: 169–174.

    CAS  Google Scholar 

  • Maresch W., Langer K, 1976.Synthesis, lattice constant and OH-valence vibrations of an orthorombic amphibole with excess OH in the system Li2O—MgO—SiO2—H2O. Contrib. Mineral. Petrol., 56: 27–34.

    Article  CAS  Google Scholar 

  • Mottana A., Griffin W. L., 1986.Crystal chemistry of two coexisting K-richterites from St. Marcel (Val d’Aosta, Italy). Am. Min., 71: 1426–1433.

    CAS  Google Scholar 

  • Oberti R., Ungaretti L., Cannillo E., Hawthorne F. C., 1992.The behaviour of Ti in amphiboles: I. Fourarid six-coordinate Ti in richterite. Eur. Journ. Min., in press.

  • Pieruccini R., 1950.La mica di un blocco pneurnatolitico del Monte Somma ed i minerali che I’accompagnano. Atti Soc. Tosc. Sc. Nat, 57: 145–173.

    CAS  Google Scholar 

  • Robert J.-L., Della Ventura G., Thauvin J.-L, 1989a.The infrared OH-stretching region of synthetic potassium nchterites in the system K2O—Na2O—CaO—MgO—SiO2—H2O—HF. Eur. J. Min., 1: 203–211.

    CAS  Google Scholar 

  • Robert J.-L., Bény J.-M., Bény C., Volfinger M., 1989b.Raman and infrared characterization of hydroxyllepidolites. Part I: Relationships between OH-stretching wavenumbers and composition. Can. Min., 27: 225–235.

    Google Scholar 

  • Rowbotham G., Farmer V.C., 1973.The effect of «A»site occupancy upon the hydroxyl stretching frequency in clinoamphiboles. Contrib. Mineral. Petrol., 38: 147–149.

    Article  Google Scholar 

  • Savelli C., 1968.The problem of rock assimilation by Somma-Vesuvius magma. II. Composition of sedimentary rocks and carbonate ejecta from the Vesuvius area. Contrib. Mineral. Petrol., 18: 43–64.

    Article  CAS  Google Scholar 

  • Washington H.S., 1906.The Roman comagmatic region. Carnegie Inst. Wash. Publ. No, 57: 199 pp.

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Ventura, G.D., Parodi, G.C., Maras, A. et al. Potassium-fluor-richterite, a new amphibole from San Vito, Monte Somma, Campania, Italy. Rend. Fis. Acc. Lincei 3, 239–245 (1992). https://doi.org/10.1007/BF03001570

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF03001570

Key words

Navigation