High‐P tectono‐metamorphic evolution of mylonites from the Variscan basement of the Northern Apennines, Italy. (19th October 2017)

• Record Type: Journal Article
• Authors: Lo Pò, Deborah; Braga, Roberto; Massonne, Hans‐Joachim; Molli, Giancarlo; Montanini, Alessandra; Bargossi, Giuseppe M.
• Is Part Of: Journal of metamorphic geology. Volume 36:Number 1(2018)
• Page Start: 23
• Page End: 39
• Publication Date: 2017-10-19
• Subjects: High‐P metamorphism -- mylonite -- Northern Apennines -- P–T–D path -- Variscan orogeny; Metamorphism (Geology) -- Periodicals; 552.4
• DOI: 10.1111/jmg.12281
• Languages: English
• ISSNs: 0263-4929

Abstract

Abstract: Strain localization within shear zones may partially erase the rock fabric and the metamorphic assemblage(s) that had developed before the mylonitic event. In poly‐deformed basements, the loss of information on pre‐kinematic phases of mylonites hinders large‐scale correlations based on tectono‐metamorphic data. In this study, devoted to a relict unit of Variscan basement reworked within the nappe stack of the Northern Apennines (Italy), we investigate the possibility to reconstruct a complete pressure ( P ) – temperature ( T )–deformation ( D ) path of mylonitic micaschist and amphibolite by integrating microstructural analysis, mineral chemistry and thermodynamic modelling. The micaschist is characterized by a mylonitic fabric with fine‐grained K‐white mica and chlorite enveloping mica‐fishes, quartz, and garnet pseudomorphs. Potassic white mica shows Mg‐rich cores and Mg‐poor rims. The amphibolite contains green amphibole+plagioclase+garnet+quartz+ilmenite defining S1 with a superposed mylonitic fabric localized in decimetre‐ to centimetre‐scale shear zones. Garnet is surrounded by an amphibole+plagioclase corona. Phase diagram calculations provide P–T constraints that are linked to the reconstructed metamorphic‐deformational stages. For the first time an early high‐ P stage at >11 kbar and 510°C was constrained, followed by a temperature peak at 550–590°C and 9–10 kbar and a retrograde stage (<475°C, <7 kbar), during which ductile shear zones developed. The inferred clockwise P–T–D path was most likely related to crustal thickening by continent‐continent collision during the Variscan orogeny. A comparison of this P–T–D path with those of other Variscan basement occurrences in the Northern Apennines revealed significant differences. Conversely, a correlation between the tectono‐metamorphic evolution of the Variscan basement at Cerreto pass, NE Sardinia and Ligurian Alps was established.