Articles | Volume 9, issue 1
https://doi.org/10.5194/se-9-91-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-9-91-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Multiphase boudinage: a case study of amphibolites in marble in the Naxos migmatite core
Simon Virgo
CORRESPONDING AUTHOR
Structural Geology, Tectonics and Geomechanics, RWTH Aachen University,
Lochnerstrasse 4–20, 52056 Aachen, Germany
Christoph von Hagke
Structural Geology, Tectonics and Geomechanics, RWTH Aachen University,
Lochnerstrasse 4–20, 52056 Aachen, Germany
Janos L. Urai
Structural Geology, Tectonics and Geomechanics, RWTH Aachen University,
Lochnerstrasse 4–20, 52056 Aachen, Germany
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Cited
15 citations as recorded by crossref.
- Quo vadis Zeus : is there a Zas shear zone on Naxos Island, Aegean Sea, Greece? A review of metamorphic history and new kinematic data A. Peillod et al. 10.1144/jgs2020-217
- Ductile Versus Brittle Tectonics in the Anatolian–Aegean–Balkan System E. Mantovani et al. 10.3390/geosciences14100277
- Spacing and strain during multiphase boudinage in 3D B. Bamberg et al. 10.1016/j.jsg.2022.104636
- Rheological behaviour of mafic dykes deformed in a granite host, Wanna, Eyre Peninsula, South Australia C. Wilson et al. 10.1016/j.jsg.2020.104164
- Geodynamics of the Mediterranean Region: Primary Role of Extrusion Processes E. Mantovani et al. 10.3390/encyclopedia5030097
- The 3D geometry of the Naxos detachment fault and the three-dimensional tectonic architecture of the Naxos metamorphic core complex, Aegean Sea, Greece H. Linnros et al. 10.1007/s00531-018-1654-2
- The Cycladic Blueschist Unit on Tinos, Greece: Cold NE Subduction and SW Directed Extrusion of the Cycladic Continental Margin Under the Tsiknias Ophiolite T. Lamont et al. 10.1029/2019TC005890
- Kinematic analyses of the asymmetric boudins in the Tutak area within the Zagros hinterland fold-and-thrust belt, Iran S. Derikvand et al. 10.1016/j.jseaes.2023.105597
- Failure mode transition in brittle boudinage: Effects of cohesion, confining pressure, and layer thickness S. Abe et al. 10.1016/j.jsg.2025.105427
- Outcrop-scale tomography: Insights into the 3D structure of multiphase boudins C. von Hagke et al. 10.1016/j.jsg.2018.02.014
- Polyphase development of chocolate-tablet boudins in the SAT zone, Kumaun Lesser Himalaya, India A. Ojha et al. 10.1016/j.jsg.2019.103863
- Numerical modelling of boudinage under pure shear: Implications for estimating viscosity ratios and finite strain from natural examples M. Dabrowski & B. Grasemann 10.1016/j.jsg.2019.05.009
- Paleostress, deformation mechanisms and finite strain related to chocolate-tablet boudinage and folding of a Permian rock salt/anhydrite sequence (Morsleben site, Germany) M. Mertineit et al. 10.1016/j.tecto.2023.229703
- Compressional origin of the Naxos metamorphic core complex, Greece: Structure, petrography, and thermobarometry T. Lamont et al. 10.1130/B31978.1
- Coeval boudinage and folding of oblique single layers under coaxial plane strain: Layer rotation around the principal stretching axis (X) J. Zulauf et al. 10.1016/j.jsg.2020.104217
15 citations as recorded by crossref.
- Quo vadis Zeus : is there a Zas shear zone on Naxos Island, Aegean Sea, Greece? A review of metamorphic history and new kinematic data A. Peillod et al. 10.1144/jgs2020-217
- Ductile Versus Brittle Tectonics in the Anatolian–Aegean–Balkan System E. Mantovani et al. 10.3390/geosciences14100277
- Spacing and strain during multiphase boudinage in 3D B. Bamberg et al. 10.1016/j.jsg.2022.104636
- Rheological behaviour of mafic dykes deformed in a granite host, Wanna, Eyre Peninsula, South Australia C. Wilson et al. 10.1016/j.jsg.2020.104164
- Geodynamics of the Mediterranean Region: Primary Role of Extrusion Processes E. Mantovani et al. 10.3390/encyclopedia5030097
- The 3D geometry of the Naxos detachment fault and the three-dimensional tectonic architecture of the Naxos metamorphic core complex, Aegean Sea, Greece H. Linnros et al. 10.1007/s00531-018-1654-2
- The Cycladic Blueschist Unit on Tinos, Greece: Cold NE Subduction and SW Directed Extrusion of the Cycladic Continental Margin Under the Tsiknias Ophiolite T. Lamont et al. 10.1029/2019TC005890
- Kinematic analyses of the asymmetric boudins in the Tutak area within the Zagros hinterland fold-and-thrust belt, Iran S. Derikvand et al. 10.1016/j.jseaes.2023.105597
- Failure mode transition in brittle boudinage: Effects of cohesion, confining pressure, and layer thickness S. Abe et al. 10.1016/j.jsg.2025.105427
- Outcrop-scale tomography: Insights into the 3D structure of multiphase boudins C. von Hagke et al. 10.1016/j.jsg.2018.02.014
- Polyphase development of chocolate-tablet boudins in the SAT zone, Kumaun Lesser Himalaya, India A. Ojha et al. 10.1016/j.jsg.2019.103863
- Numerical modelling of boudinage under pure shear: Implications for estimating viscosity ratios and finite strain from natural examples M. Dabrowski & B. Grasemann 10.1016/j.jsg.2019.05.009
- Paleostress, deformation mechanisms and finite strain related to chocolate-tablet boudinage and folding of a Permian rock salt/anhydrite sequence (Morsleben site, Germany) M. Mertineit et al. 10.1016/j.tecto.2023.229703
- Compressional origin of the Naxos metamorphic core complex, Greece: Structure, petrography, and thermobarometry T. Lamont et al. 10.1130/B31978.1
- Coeval boudinage and folding of oblique single layers under coaxial plane strain: Layer rotation around the principal stretching axis (X) J. Zulauf et al. 10.1016/j.jsg.2020.104217
Latest update: 05 Nov 2025
Short summary
The marbles of the migmatitic dome on the island Naxos contain deformed layers of amphibolite with multiple phases of boudinage. The boudins formed by E–W shortening normal to the layers and layer parallel extension in various directions. We identified five different generations of boudins that show that E–W shortening is the prevalent deformation in these rocks during the peak metamorphosis and the following cooling, different from other parts of the island dominated by top-to-north shearing.
The marbles of the migmatitic dome on the island Naxos contain deformed layers of amphibolite...