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Geological,Structural and Mineralogical Approach to Investigate the Evolution of Low-and very Low-Grade Metamorphic Units from the intra-pontide suture zone,Central pontides,Turkey

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Journal of Earth Science 2021年第6期32卷 1512-1527页

作者： Alessandro Ellero Chiara Frassi Mehmet Cemal Göncüoğlu Marco Lezzerini Michele Marroni Giuseppe Ottria Luca Pandolfi Kaan Sayit Marco Tamponi Istituto di Geoscienze e Georisorse-CNR Via G.Moruzzi 156124PisaItaly Dipartimento di Scienze della Terra Universitàdi PisaVia S.Maria 5356126PisaItaly Department of Geological Engineering Middle East Technical University06800AnkaraTurkey

A multidisciplinary approach combining multiscale geological-structural analyses(from field to microscale) and clay mineral transformations(clay mineralogy, illite and chlorite "crystallinity" and b cell dimension(b_(0)) of K-white mica) was adopted to unravel the tectono-metamorphic evolution of low-and very low-grade tectono-metamorphic units from the intra-pontide suture zone in northern Turkey. The mineralogical study allowed to better evaluate the structural stacking outlined during the geological mapping, leading to distinguish three tectono-metamorphic units, two in epizone(Daday and Emirkoy units) and one in anchizone(Cifter Unit) metamorphic conditions. The mesostructural and microstructural analyses suggest a polyphase tectonic-metamorphic evolution. The different macroscopic features observed between the two units characterized by the same epizone metamorphism, can be justified by the evidence that these metamorphic conditions were acquired during the last stages of exhumation in the Daday Unit, while they constrained the metamorphic-peak conditions in the Emirkoy Unit. Contemporary analyses and comparison between structural and mineralogical data have thus proven to be a powerful tool to investigate the low-grade and very low-grade metamorphic environments, allowing at the same time to solve the apparent contradictions deriving from the mineralogical study and to significantly improve the detail of the geological mapping in the field.

关键词： clay minerals structural analyses low-temperature metamorphism epizone anchizone diagenesis intra-pontide suture zone Turkey

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Geological-structural and mineralogical approach to investigate the evolution of low- and very low-grade metamorphic units from the intra-pontide suture zone(Central pontides， Turkey)

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Journal of Earth Science 2021年

作者： Alessandro Ellero Chiara Frassi Mehmet Cemal G?ncüo?lu Marco Lezzerini Michele Marroni Giuseppe Ottria Luca Pandolfi Kaan Sayit Marco Tamponi Istituto di Geoscienze e Georisorse-CNR Dipartimento di Scienze della Terra， Università di Pisa Department of Geological Engineering， Middle East Technical University

A multidisciplinary approach combining multiscale geological-structural analyses （from field to microscale） and clay mineral transformations (clay mineralogy， illite and chlorite “crystallinity” and b cell dimension (b0) of K-white mica) was adopted to unravel the tectono-metamorphic evolution of low- and very low-grade tectono-metamorphic units from the intra-pontide suture zone in northern Turkey. The mineralogical study allowed to better evaluate the structural stacking outlined during the geological mapping， leading to distinguish three tectono-metamorphic units， two in Epizone （Daday and Emirk?y units） and one in Anchizone （?ifter Unit） metamorphic conditions. The mesostructural and microstructural analyses suggest a polyphase tectonic-metamorphic evolution. The different macroscopic features observed between the two units characterized by the same Epizone metamorphism， can be justified by the evidence that these metamorphic conditions were acquired during the last stages of exhumation in the Daday Unit， while they constrained the metamorphic-peak conditions in the Emirk?y Unit. Contemporary analyses and comparison between structural and mineralogical data have thus proven to be a powerful tool to investigate the low-grade and very low-grade metamorphic environments， allowing at the same time to solve the apparent contradictions deriving from the mineralogical study and to significantly improve the detail of the geological mapping in the field.

关键词： Clay minerals Structural analyses Low-temperature metamorphism Epizone Anchizone Diagenesis intra-pontide suture zone Turkey

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The intra-pontide ophiolites in Northern Turkey revisited:From birth to death of a Neotethyan oceanic domain

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Geoscience Frontiers 2020年第1期11卷 129-149页

作者： Michele Marroni M.Cemal Goncüoglu Chiara Frassi Kaan Sayit Luca Pandolfi Alessandro Ellero Giuseppe Ottria Dipartimento di Scienze della Terra Universita di Pisavia S.Maria 5356126PisaItaly Istituto di Geoscienze e Georisorse-CNR Via G.Moruzzi 156124PisaItaly Department of Geological Engineering Middle East Technical University06531 AnkaraTurkey

The Anatolian peninsula is a key location to study the central portion of the Neotethys Ocean(s)and to understand how its western and eastern branches were *** of the lesser known branches of the Mesozoic ocean(s)is preserved in the northern ophiolite suture zone exposed in Turkey,namely,the intra-pontide suture *** is located between the Sakarya terrane and the Eurasian margin(i.e.,Istanbul-Zonguldak terrane)and consists of several metamorphic and non-metamorphic units containing ophiolites produced in supra-subduction settings from the Late Triassic to the Early *** preserved in the metamorphic units recorded pervasive deformations and peak metamorphic conditions ranging from blueschist to eclogite *** the nonmetamorphic units,the complete oceanic crust sequence is preserved in tectonic units or as olistoliths in sedimentary ***,structural,metamorphic and geochronological investigations performed on ophiolite-bearing units allowed the formulation of a new geodynamic model of the entire"life"of the intrapontide oceanic basin(s).The reconstruction starts with the opening of the intra-pontide oceanic basins during the Late Triassic between the Sakarya and Istanbul-Zonguldak continental microplates and ends with its closure caused by two different subductions events that occurred during the upper Early Jurassic and Middle *** continental collision between the Sakarya continental microplate and the Eurasian margin developed from the upper Early Cretaceous to the *** presented reconstruction is an alternative model to explain the complex and articulate geodynamic evolution that characterizes the southern margin of Eurasia during the Mesozoic era.

关键词： intra-pontide suture zone Central pontides Northern Turkey Ophiolites Neotethys Ocean Geodynamics

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