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Aspromonte Massiv

Steckbrief

Land

Italien

Re­gi­on

Kalabrien (Calabria), Region / Reggio Calabria, Provinz / Aspromonte Massiv

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https://www.mineralienatlas.de/?l=48691
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Wichtig: Vor dem Betreten dieser wie auch anderer Fundstellen sollte eine Genehmigung des Betreibers bzw. Besitzers eingeholt werden. Ebenso ist darauf zu achten, dass während des Besuches der Fundstelle die erforderlichen Sicherheitsvorkehrungen getroffen und eingehalten werden.

Weitere Funktionen

Mineralien (Anzahl: 27)

Gesteine (Anzahl: 9)

Referenz- und Quellangaben, Literatur

Literatur:

  • Ogniben, L. (1960). Nota illustrativa dello schema geologico della Sicilia nord-orientale. Riv. Min. Sic., 64-65: 183-212.
  • Bonardi, G., Messina, A., Perrone, V., Russo, M., Russo, S. and Zuppetta, A. (1980). La finestra tettonica di Cardeto (Reggio Calabria). Rend. Soc. Geol. It., 3: 3-4.
  • Bonardi, G., Cello, G., Perrone, V., Tortorici, L., Turco, E. and Zuppetta, A., (1982). The evolution of the northern sector of Calabria Peloritani Arc in a semiquantitative palinspastic restoration. Boll. Soc. Geol. Ital., 101, 259-74.
  • Crisci, G.M., Donati, G., Messina, A., Russo, S., Perrone, V. (1982). L’Unità superiore dell’Aspromonte. Studio geologico e petrografica. Rend. S.I.M.P., 38 (3): 989-1014
  • Bonardi, G., Messina, A., Perrone, V., Russo, S., Zuppetta, A. (1984). L’unita di Stilo nel settore meridionale dell’Arco Calabro-Peloritano, Boll. Soc. Geol. It., 103, 279-309.
  • Bonardi, G., Compagnoni, R., Del Moro, A., Messina, A., Perrone, V. (1987). Riequilibrazioni tettonico-metamorfiche Alpine dell'Unità dell'Aspromonte, Calabria Meridionale. Rend. SIMP, 42:301.
  • Cavazza, W. (1988). La Formazione di Stilo-Capo d'Orlando: un possibile strumento per lo studio dell'evoluzione strutturale dell'Arco Calabro-Peloritano. Rend. Soc. Geol. It., 11: 35-38
  • Pezzino, A., Pannucci, S., Puglisi, G., Atzori, P., Ioppolo, S., Lo Giudice, A. (1990). Geometry and metamorphic environment of the contact between the Aspromonte - Peloritani Unit (Upper Unit) and Madonna dei Polsi Unit (Lower Unit) in the central Aspromonte area (Calabria). Boll. Soc. Geol. It., 109: 455-69.
  • Puglisi, G. and Pezzino, A. (1994). Metamorphism in the central Aspromonte area: geological, mineralogical and petrogenetic relationships. Per. Min., 63, 153-68.
  • Cavazza, W., Blenkinsop, J., Decelles, P.G., Patterson, R.T., Reinhardt, E.G. (1997). Stratigrafia e sedimentologia della sequenza sedimentaria oligocenico-quaternaria del bacino calabro-ionico. Boll. Soc.Geol. It., 116: 51-77
  • Graeßner, T. and Schenk, V. (1999). Low-pressure metamorphism of Palaeozoic pelites in the Aspromonte, S Calabria: constraints for the thermal evolution in the Calabrian crustal cross-section during the Hercynian orogeny. J. Metamorphic Geology., 17 (2): 157-72.
  • Ortolano, G., Cirrincione, R., Pezzino, A. (2005). P-T evolution of alpine metamorphism in the S Aspromonte Massif (Calabria - Italy). Schw. Min. und Petrogr.Mitt. vol. 85-1, S.31-56.
  • Fazio, E., Heilbronner, R., Punturo, R. (2007). Microstructural study and petrophysical characterization of naturally deformed leuco-gneisses from the Montalto shear zone (Aspromonte Massif, S Italy). DRT 2007 - 16°Conf, Deformation Mechanisms, Rheology and Tectonics. Milano, 27.9. - 2.10. 2007. In: Rendiconti della Soc. Geol, Ital,, 5, 87-88.
  • Pezzino, A. et al. (2008). Alpine metamorphism in the Aspromonte Massif: implications for a new framework for the southern sector of the Calabria-Peloritani Orogen (Italy). Intern.Geol. Rev., 50, 423-41.
  • Fazio, E., Cirrincione, R., Pezzino, A. (2008). Estimating P-T conditions of Alpine-type metamorphism using multistage garnet in the tectonic windows of the Cardeto area (S Aspromonte Massif, Calabria). Min. Petrol., 93, 111-142.
  • Cirrincione, R., Fazio, E., Fiannacca, P., Ortolano, G., Punturo, R. (2009). Microstructural Investigation Of Naturally Deformed Leucogneiss from an Alpine Shear Zone (S Calabria – Italy). Pure and Applied Geophysics, 166, 995-1010. doi 10.1007/s00024-009-0483.
  • Fazio, E., Cirrincione, R., Pezzino, A. (2009). Garnet crystal growth in sheared metapelites (S Calabria – Italy): relationships between isolated porphyroblasts and coalescing euhedral crystals. Per.Miner., 78, 1, 3-18.
  • Fazio, E., Cirrincione, R., Punturo, R. (2010). Quartz c-axis texture mapping of mylonitic metapelite with rods structures (Calabria, S Italy): clues for hidden shear flow direction. Special Issue "Structural Geology-From Classical to Modern Concepts", J. Geol. Soc. India, 75, 171-82.
  • Cirrincione, R. et al. (2010). Microstructure and elastic anisotropy of naturally deformed leucogneiss from a shear zone in Montalto (S Calabria, Italy). From: SPALLA, M.I., MAROTTA, A.M. & GOSSO, G. (eds). Advances in Interpretation of Geol. Proc. Geol.Soc., London, Special Publications, 332, 49–68. doi: 10.1144/SP332.4.
  • Cirrincione, R., Fazio, E., Ortolano, G., Pezzino, A., Punturo, R. (2011). Fault-related rocks: deciphering the structural–metamorphic evolution of an accretionary wedge in a collisional belt, NE Sicily. Intern.Geol.Rev.,doi:10.1080/00206814.2011.623022.
  • Cirrincione, R. et al. (2013). The Alpine evolution of the Aspromonte Massif: constraints for geodynamic reconstruction of the Calabria–Peloritani Orogen. Geol. Field Trips, 5, 1-73.

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