Thermodynamic modeling assisted by multivariate statistical image analysis as a tool for unraveling metamorphic P-T-d evolution: an example from ilmenite-garnet-bearing metapelite of the Peloritan
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- 作者：Patrizia Fiannacca (1)
Deborah Lo Pò (2)
Gaetano Ortolano (1)
Rosolino Cirrincione (1)
Antonino Pezzino (1) - 刊名：Mineralogy and Petrology
- 出版年：2012
- 出版时间：4 - November 2012
- 年：2012
- 卷：106
- 期：3
- 页码：151-171
- 全文大小：2377KB
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Deborah Lo Pò (2)
Gaetano Ortolano (1)
Rosolino Cirrincione (1)
Antonino Pezzino (1)
1. Department of Biological, Geological and Environmental Sciences, University of Catania, Corso Italia 57, 95129, Catania, Italy
2. Department of Earth and Geoenvironmental Sciences, University of Bologna, Piazza di Porta San Donato 1, 40126, Bologna, Italy - ISSN：1438-1168
文摘
An ilmenite-garnet-bearing schist from the medium-grade metapelite complex of the Mandanici Unit in the Peloritani Mountains has been investigated to constrain the P-T conditions attained in this sector of the southern European Hercynian chain. Microprobe investigations assisted by statistical handling of X-ray maps via principal component analysis allowed us to better elucidate the porphyroblast-matrix relationships, the geometry of the elemental distribution in garnet porphyroblasts and the average volume percentage of the reactant garnet during retrograde metamorphic evolution. Selected microprobe data were then used to constrain, by means of P-T pseudosections, the main P-T stages of the metamorphic evolution, using the XRF bulk-rock chemistry as the equilibrium chemical composition for the prograde and peak stages and an effective bulk-rock composition for the retrograde one. Peak metamorphic P-T estimates (~530?°C; 0.9?GPa) are consistent with a Hercynian crustal thickening stage at middle-lower crustal conditions, while subsequent evolution, constrained at 420-60?°C; 0.30-.60?GPa, depicts a retrograde clockwise P-T trajectory linked to exhumation under likely extensional shearing conditions. The results obtained in this paper lead to envisage a new scenario for the crustal evolution of the Peloritani Mountains and stimulate a revision of previous interpretations in the light of the new investigation techniques.