Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic

2019/09/03 by Douwe J.J. van Hinsbergen, Trond H. Torsvik, Stefan M. Schmid +5 · 638 citations
Earth and Planetary Sciences · Biochemistry, Genetics and Molecular Biology · #Geological and Geophysical Studies Worldwide #earthquake and tectonic studies #Geomagnetism and Paleomagnetism Studies #Geology #Subduction #Paleontology #Tectonics #Plate tectonics #Paleomagnetism #Earth science #Seismology

paper · doi:10.1016/j.gr.2019.07.009

published in Gondwana Research 81, 79-229 (Elsevier BV)

openalex publication_date 2019/09/03 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/04

Abstract

The basins and orogens of the Mediterranean region ultimately result from the opening of oceans during the early break-up of Pangea since the Triassic, and their subsequent destruction by subduction accommodating convergence between the African and Eurasian Plates since the Jurassic. The region has been the cradle for the development of geodynamic concepts that link crustal evolution to continental break-up, oceanic and continental subduction, and mantle dynamics in general. The development of such concepts requires a first-order understanding of the kinematic evolution of the region for which a multitude of reconstructions have previously been proposed. In this paper, we use advances made in kinematic restoration software in the last decade with a systematic reconstruction protocol for developing a more quantitative restoration of the Mediterranean region for the last 240 million years. This restoration is constructed for the first time with the GPlates plate reconstruction software and uses a systematic reconstruction protocol that limits input data to marine magnetic anomaly reconstructions of ocean basins, structural geological constraints quantifying timing, direction, and magnitude of tectonic motion, and tests and iterations against paleomagnetic data. This approach leads to a reconstruction that is reproducible, and updatable with future constraints. We first review constraints on the opening history of the Atlantic (and Red Sea) oceans and the Bay of Biscay. We then provide a comprehensive overview of the architecture of the Mediterranean orogens, from the Pyrenees and Betic-Rif orogen in the west to the Caucasus in the east and identify structural geological constraints on tectonic motions. We subsequently analyze a newly constructed database of some 2300 published paleomagnetic sites from the Mediterranean region and test the reconstruction against these constraints. We provide the reconstruction in the form of 12 maps being snapshots from 240 to 0 Ma, outline the main features in each time-slice, and identify differences from previous reconstructions, which are discussed in the final section.

Citations

• The southernmost margin of the Tethys realm during the Mesozoic and Cenozoic: Initial geometry and timing of the inversion processes
• Geochronological evidence for the Alpine tectono-thermal evolution of the Veporic Unit (Western Carpathians, Slovakia)
• Iberian plate kinematics: a jumping plate boundary between Eurasia and Africa
• The hercynian chain in Sardinia (Italy)
• India–Eurasia collision chronology has implications for crustal shortening and driving mechanism of plates
• The East Anatolian Fault: geometry, segmentation and jog characteristics
• The arc of the western Alps in the light of geophysical data on deep crustal structure
• Phanerozoic polar wander, palaeogeography and dynamics
• Geochemistry, petrogenesis and tectonic setting of the Samothraki mafic suite, NE Greece: Trace-element, isotopic and zircon age constraints
• Kinematic reconstruction of the Caribbean region since the Early Jurassic
• New evidence and solution to the Maden complex controversy of the Southeast Anatolian orogenic belt (Turkey)
• The structure of the Atlantic–Mediterranean transition zone from the Alboran Sea to the Horseshoe Abyssal Plain (Iberia–Africa plate boundary)
• Tectonic map and overall architecture of the Alpine orogen
• Geophysical‐geological transect and tectonic evolution of the Swiss‐Italian Alps
• Age constraints on the igneous and metamorphic evolution of the Hellenic-Dinaric ophiolites
• Orogenic processes and the Corsica/Apennines geodynamic evolution: insights from Taiwan
• Plate tectonics and net lithosphere rotation over the past 150 My
• Tethyan evolution of Turkey: A plate tectonic approach
• Lateral extrusion in the eastern Alps, PArt 2: Structural analysis
• The North Pacific: an Example of Tectonics on a Sphere
• Subduction and the depth of convection in the Mediterranean mantle
• The architecture of an incipient oceanic basin: a tentative reconstruction of the Jurassic Liguria-Piemonte basin along the Northern Apennines–Alpine Corsica transect
• Late Eocene–Neogene sedimentary geology of the Girne (Kyrenia) Range, northern Cyprus: A case history of sedimentation related to progressive and diachronous continental collision
• Über die tektonisch-mechanischen Folgerungen aus den großen anatolischen Erdbeben des letzten Dezenniums
• Tectonics of the Mediterranean Cimmerides: nature and evolution of the western termination of Palaeo-Tethys
• Post-collisional orogen-parallel large-scale extension in the Eastern Alps
• The interaction between Aegean back-arc extension and Anatolia escape since Middle Miocene
• Tectonics of the Caucasus and adjoining regions: implications for the evolution of the Tethys ocean
• Mesozoic–Tertiary tectonic evolution of Albania in its regional Eastern Mediterranean context
• Tectonics of the Tethysides: Orogenic Collage Development in a Collisional Setting
• The Tauern Window (Eastern Alps, Austria): a new tectonic map, with cross-sections and a tectonometamorphic synthesis
• Dating of the Black Sea Basin: new nannoplankton ages from its inverted margin in the Central Pontides (Turkey)
• Reconstructing the Alps–Carpathians–Dinarides as a key to understanding switches in subduction polarity, slab gaps and surface motion
• Tectonic, magmatic, and metallogenic evolution of the Late Cretaceous arc in the Carpathian‐Balkan orogen
• The evolution of a key segment in the Europe–Adria collision: The Fruška Gora of northern Serbia
• Age, spreading rates, and spreading asymmetry of the world's ocean crust
• Northern Apennine–Corsica orogenic system: an updated overview
• The geological development of the Balkan Peninsula related to the approach, collision and compression of Gondwanan and Eurasian units
• Global continental and ocean basin reconstructions since 200Ma
• Greater India Basin hypothesis and a two-stage Cenozoic collision between India and Asia
• A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons
• THE NORTH ANATOLIAN FAULT: A NEW LOOK
• Evolution of the Calabrian accretionary wedge (central Mediterranean)
• Formation and deformation of the Pannonian Basin: constraints from observational data
• Timing of uplift in the Zagros belt/Iranian plateau and accommodation of late Cenozoic Arabia–Eurasia convergence
• Tectonic evolution of Western Tethys from Jurassic to present day: coupling geological and geophysical data with seismic tomography models
• The Aptian (Early Cretaceous) oceanic anoxic event (OAE1a) in Svalbard, Barents Sea, and the absolute age of the Barremian-Aptian boundary
• Earth History and Palaeogeography
• Understanding fossil fore-arc basins: Inferences from the Cretaceous Adria-Europe convergence in the NE Dinarides

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