1,721,182 research outputs found
Metamorphic evolution of the Saka Unit (Central Pontides, Northern Turkey): new implications for the Mesozoic convergence-related processes in the Intra-Pontide suture zone
Full text linkIn Northern Turkey, the Intra-Pontide suture (IPS) zone represents an east-west trending belt of deformed and/or metamorphic rocks bounded by the Istanbul-Zonguldak Terrane (IZ) to the north and the Sakarya Composite Terrane (SK) to the south (e.g. Göncüoğlu et al., 1997). Despite its importance for the geodynamics reconstructions of the Black Sea and Eastern Mediterranean areas during the Mesozoic, the IPS zone has been poorly investigated; only recently the role of its metamorphic units during the syn-collisional evolution was explored (Marroni et al., 2014; Frassi et al., 2016; 2017)
In order to provide new insights on the Mesozoic-Tertiary geodynamic reconstruction of the southern margin of the Laurasia, we present new data from the Saka Unit from the eastern portion of the IPS. Using a multidisciplinary approach that includes lithological, structural, metamorphic and petrographic investigations, we constrained the P-T-t path during the Mesozoic subduction and consequent exhumation and accretion to Laurasia. Following the determination of mesostructures, we analysed a series of samples of metabasite and metapelite. Mineral chemistry of phases at equilibrium in the pervasive S2 foliation was determined, and PT determinations were performed through pseudosection calculation of three samples. PT conditions are within the epidote-amphibolite facies, with pressures of 1.2 ± 0.15 GPa and Temperatures 600 ± 50 °C, thus higher than those determined previously, suggesting that S2 could be a composite foliation where a progressive evolution acquired during onset of exhumation was recorded. A comparison with the PT evolutions of the nearby Daday and Domuz-Dag units, shows that they record lower T at D2 at different ages, and that the pre-D2 conditions, when they are preserved, are different in the three units.
References
Frassi C., Göncüoğlu M.C., Marroni M., Pandolfi L., Ruffini L. Ellero A., Ottria G. & Sayit K. 2016. The Intra-Pontide Suture Zone in the Tosya-Kastamonu area, Northern Turkey. J. of Maps. 12, 211-219
Frassi, C, Marroni, M., Pandolfi, L., Göncüoğlu, M. C., Ellero, A., Ottria, G., Sayit, K., McDonald, C.S., Balestrieri, M.L. & Malasoma, A. 2018. Burial and exhumation history of the Daday Unit (Central Pontides, Turkey): implications for the closure of the Intra-Pontide oceanic basin. Geol. Mag., 155, 356-376.
Göncüoğlu, M. C., Marroni, M., Sayit, K., Tekin, U. K., Ottria, G., Pandolfi, L. & Ellero, A., 2012. The Ayli Dag ophiolite sequence (central-northern Turkey): A fragment of middle Jurassic oceanic lithosphere within the Intra-Pontide suture zone. Ofioliti, 37, 77–91.
Marroni, M., Frassi, C., Göncüoğlu, C. M., Di Vincenzo, G., Pandolfi, L., Rebay, G., Ellero, A. & Ottria, G. 2014. Late Jurassic amphibolite-facies metamorphism in the Intra-Pontide Suture Zone (Turkey): an eastward extension of the Vardar Ocean from the Balkans into Anatolia? J. Geol. Soc., 171, 605–608
Carta geologico-strutturale dell'alta Val di Vara (Appennino ligure-emiliano), scala 1:25.000, con sezioni
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Detrimental effects of high-dose dexamethasone in severe, refractory, HIV-related thrombocytopenia.
No full textGabbro-derived granulites from External Liguride units (northern Apennine, Italy): Implications for the rifting processes in the western Tethys
No full textDinamiche nei complessi in subduzione: trasferimento di massa in sistemi fossili e confronti con esempi attuali. (Progetto nazionale PRIN, coordinatore nazionale M. Marroni) Il prisma di accrezione Cretaceo-Eocenico dell’Appennino settentrionale: informazioni dall’assetto strutturale delle unità Liguri e dalla distribuzione delle paleotemperature. (Progetto dell'Unità di Bologna, responsabile G.A. Pini)
No full textNell'ambito delle tematiche del programma di ricerca nazionale, l'Unità operativa di Bologna, da me cooordinata, si occuperà dello studio delle unità Liguri dell'Appennino Settentrionale, anche in comparazione con le unità a forte deformazione (melanges) del Giappone e della Nuova Zelanda.
L'UO di Bologna si dedicherà alla ricostruzione delle paleotemperature e paleopressioni di carico nelle unità Liguri dell'Appennino settentrionale. Tale studio sarà integrato dallo studio dell'assetto strutturale interno e generale delle unità Liguri, con particolare riguardo per le unità a forte deformazione interna e stratal disruption (mlanges).
Finalità del programma è definire un quadro cinematico per il prisma di accrezione cretaceo-eocenico dell’Appennino settentrionale
Calcareous nannofossils dating of the S. Martino Formation, from the balagne ophiolites sequence (Alpine Corsica): comparison with the palombini shale of the Northern Apennines, Ofioliti, v. 25, n. 2, 147-157
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Geological Constraints for the Geodynamic evolution of the Southern Margin of the Caribbean Plate
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