Vai ai contenuti. | Spostati sulla navigazione | Spostati sulla ricerca | Vai al menu | Contatti | Accessibilità

logo del sistema bibliotecario dell'ateneo di padova

Carluccio, Roberta (2013) Studio sull'orientazione preferenziale degli assi c del reticolo cristallino del quarzo in una milonite granulitica della Calabria. = Study of the quartz c-axis preferred orientation in a granulite facies mylonite of the Calabria basament. [Laurea triennale]

Full text disponibile come:

[img]PDF (Tesi)


This study will focus on a granulite mylonite from the Amaroni Shear Zone in the Serre Massif within the Calabria-Peloritani-terrain arc. The mylonite appears to be structurally and geometrically linked to the mean Alpine thrust contact: the Curinga-Girifalco Line, which separates the basement units from those that underwent an Alpine overprint. The researcher’s aim is to identify the mylonitic shear zone. In particular, to understand if the mylonite was subject to high temperature conditions during granulite facies metamorphism in the Varisican orogeny, or whether it formed at lower temperatures associated with amphibolite to greenschist facies metamorphism during the Alpine orogeny.These uncertainties regarding emplacement conditions can be deduced quickly and effectively by studying the rock’s microstructures, specifically the crystallographic preferred orientation of the minerals (CPO). The analysis of the quartz microlattice structure, using the EBSD technique and analysis of kinematic indicators, will allow us to deduce the correct P-T-t conditions operating during the mylonite’s formation. From the experimental data, we assert that the mylonite formed during high temperature conditions pertaining to granulite facies metamorphism. The conditions necessary for the development and evolution of a high grade metamorphic environment were active during the extension and isothermal uplift phase, which is characteristic of the Calabria-Peloritani-terrain arc earlier than 300 Ma, but not after 252 Ma. After this time, it is known that temperatures were below the conditions necessary for granulite facies metamorphism.

Item Type:Laurea triennale
Corsi di Laurea Triennale:Scuola di Scienze > Scienze geologiche
Subjects:Area 04 - Scienze della terra > GEO/07 Petrologia e petrografia
Codice ID:45301
Relatore:Spiess, Richard
Data della tesi:20 September 2013
Biblioteca:Polo di Scienze > Dip. Geoscienze - Biblioteca
Tipo di fruizione per il documento:on-line per i full-text
Tesi sperimentale (Si) o compilativa (No)?:Yes

Solo per lo Staff dell Archivio: Modifica questo record