HP-LT metamorphism in Elba Island: Implications for the geodynamic evolution of the inner Northern Apennines (Italy)

The inner Northern Apennines belt (i.e., northern Tyrrhenian Sea and Tuscany) is an Alpine chain affectedby high-P metamorphic conditions during its evolution. Although Elba Island is structurally located closeto the Adria-Europe suture zone, for several authors it represents a sector of the orogen affected bylow-P metamorphism. The involvement of Elba Island tectonic units in high-P metamorphism was onlysuspected for the sparse presence of phengitic white mica in the metasedimentary rocks. This paperpresents the first clear evidence of high-P and low-T metamorphism found in metabasite rocks embed-ded in the Cretaceous calcschist of eastern Elba Island. Mineral composition of metabasite includesGln + Cpx + Ep + Ab + Act + Qtz + Ilm ± Ti-oxide ± Spn and is indicative of a former equilibration in the epi-dote blueschist subfacies and subsequent retrogression in the greenschist facies. Recorded metamorphicconditions are P = 0.9–1.0 GPa and T = 330–350◦C. Tectonic discrimination using immobile elements inthe metabasite does not point to an oceanic setting. As a consequence, the metasedimentary succes-sion containing metabasite is explained as belonging to the Tuscan continental domain and not to theLigurian-Piedmont Ocean, as previously interpreted. Our results have two significant implications: (i)it is confirmed and strengthened that the tectonic stacking of the Elba Island units did not occur in alow-pressure context; (ii) Elba Island is now completely reconciled in the tectonic and metamorphicevolution of the inner Northern Apennines

The lawsonite-glaucophane blueschists of Elba Island (Italy)

Evidence for high-P blueschist-facies metamorphism was found in metabasites embedded in calcschists of Eastern Elba Island (Northern Apennines, Italy). Study of immobile trace elements (REEs and HFSEs) in the metabasites indicates an affinity with T- and E-MORBs, and they are interpreted as sill or dykes intruded in the western margin of the Adria continental plate. The minerals are heterogeneously distributed in the rock, constituting mafic and Ca-Al-rich microdomains inherited respectively from the magmatic pyroxene- and plagioclase-rich zones of the original doleritic rock. The peak pressure paragenesis consisted of lawsonite, aegirine-omphacite, glaucophane and chlorite. Former rhombic prism of lawsonite has been replaced by pseudomorphic clinozoisite (0.1 mm in size) with inclusions of Ms. ± Ab ± Qz. The inclusions are preferentially oriented parallel to one of the diagonals of the basal rhombic sections, indicating that the two diagonals were not crystallographically equivalent. This implies that the protocrystals were orthorhombic prisms with {110} faces, which is the case of lawsonite. The different compositions shown by white mica and epidote in the pseudomorphs (muscovite and Fe3+-poor clinozoisite) and in the matrix (phengite and Fe,sup>3+-rich epidote) also suggest the former presence of Mg- and Fe-poor lawsonite in these rocks. Thermodynamic modelling, using the THERMOCALC software and dataset, suggests that metabasites experienced a clockwise P-T path from the lawsonite-blueschist to epidote-blueschist subfacies, down to greenschist facies. The estimated peak pressure conditions are P ≥ 1.6 GPa and 450 40Ar/39Ar method. This evolution is interpreted in terms: (i) intrusion of basic magmas in carbonatic and pelitic sediments (post-late Cretaceous, pre-Oligocene), (ii) subduction (Oligocene), (iii) collision (early Miocene: 19.8 ± 1.4 Ma), (iv) exhumation and granite intrusion (middle-late Miocene), favored by extensional tectonics. We underline that the eastern part of Elba Island belongs to a blueschist-facies belt that extends from Gorgona Island, in the northwest, to Argentario and Giglio Island in the southeast, so many of the conclusions of this study can be extended to the whole of this belt

PETROLOGY OF BASIC AND INTERMEDIATE OROGENIC GRANITOIDS FROM THE SILA MASSIF (CALABRIA, SOUTHERN ITALY) RID A-1229-2011

Hercynian gabbroic, dioritic and tonalitic rocks crop out in the neighbourhood of Rovale (Sila Grande, Calabria). They make up a crude rectangular outcrop with the western part consisting of gabbroic rocks and the eastern of dioritic and tonalitic rocks. They come into contact with medium to high grade metapelites on the western side and with heterogeneous granodiorites on the other sides. In the gabbroic body both opx +/- ol bearing cumulates and amphibole differentiates occur and are characterized by the widespread presence of brown pargasite. Sporadic magmatic to subsolidus corona textures between olivine and plagioclase or orthopyroxene and plagioclase can be observed and their preservation clearly suggests a post-tectonic emplacement for the gabbroic magma. Diorites and tonalites display hypidiomorphic textures free of olivine and orthopyroxene and bearing green Mg-hornblende. The granitoids, on the basis of chemical data, display orogenic features of the continent-continent collision type. The gabbroic rocks have high Al tholeiitic composition and fractionation of orthopyroxene and plagioclase played an important part in their evolution. The Rb/Sr isochron method did not give a precise emplacement age for the granitoids as a whole. Initial Sr-87/Sr-86 ratios (at 290 Ma) are higher in the gabbroic body (0.7091-0.7095) than in diorites and tonalites (0.7083-0.7092). Thus gabbroic rocks appear more displaced than diorites and tonalites towards crustal isotopic composition. The epsilonNd data seem to confirm this feature, thus suggesting that the gabbroic rocks and diorites derived from distinct mantle magma batches. Interestingly, small isotropic gabbroic masses occur within the diorites and show general features that allow them to be considered as possibly parental with respect to the host diorites. The evolution to the dioritic composition might have occurred through fractionation and minor mixing with a more acidic component such as the northern granodiorites. Geochemical, Sr and Nd isotopic data indicate a scenario of a composite plutonic body formed by distinct magma batches of mixed crust and mantle origin

LATE MAGMATIC TO SUBSOLIDUS CORONAS IN GABBROIC ROCKS FROM THE SILA MASSIF (CALABRIA, ITALY) RID A-1229-2011

Corona textures between olivine and plagioclase or orthopyroxene and plagioclase are present in Hercynian gabbroic rocks from the Calabrian Sila Massif They have been studied through optical and SEM investigations together with EDS and WDS analyses. Textural features indicate the existence of two extreme corona types formed during late magmatic stages or during subsolidus cooling. Magmatic coronas are characterized by an inner orthopyroxene layer and an outer orange-brown amphibole layer that might be in optical continuity with orthopyroxene and amphibole poikilites respectively. Subsolidus coronas consist of an inner layer of colourless amphibole and an outer layer of amphibole +/- spinel. They sometimes form a collar also around plagioclase enclosed in olivine. A large spectrum in the composition of corona amphiboles from Ti-bearing pargasite to Mg-hornblende was observed. The variation in Ti content of amphibole was interpreted as a consequence of the different conditions of crystallization from late magmatic to subsolidus with temperatures ranging from 880-degrees-C to 580-degrees-C. The significant gahnite component in spinel possibly indicates that subsolidus reactions occurred in an open system. The pressure of formation constrained by the mineral assemblage of metamorphic basement rocks and by the neighbouring diorites has been estimated at 4 kbar

Quantification of Flow Patterns in Sheared Tonalite Crystal-melt Mush: Application of Fractal-geometry Methods

Fractal-geometry-based analysis techniques offer simple and efficient ways for analyzing magmatic fabrics that are otherwise difficult to describe quantitatively. This study shows an application of two different methods on flow patterns observed in a syntectonic magmatic body injected into the lower crust. XZ and YZ rock cuts are scanned, and the scans are automatically transferred to binary patterns of mafic and felsic minerals. These are analyzed by box-counting as well as the modified Cantor-dust method. Box-counting leads to characterization of the entire patterns, proves their fractality in two different scale ranges, and yields information about magma mingling and grain-aggregate forming processes. The modified Cantor-dust method quantifies the anisotropy of pattern complexity and represents a potentially powerful method for determination of shear sense during magmatic flow. Both methods represent useful tools specifically for analyzing diffuse magmatic fabrics and for connecting field-related studies with analyses on the microscale