Peer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/143706/1/tect20719.pdfhttps://deepblue.lib.umich.edu/bitstream/2027.42/143706/2/tect20719_am.pd
A continent-oceanic island arc collision model was proposed as a new geodynamic scenario for the evo...
The Variscan structures of the Caucasus region are still quite difficult to decipher, they certainly...
In our paper (Hollingsworth et al., 2008), we present a model of how the distribution of active faul...
Comparison of plate convergence with the timing and magnitude of upper crustal shortening in collisi...
Continental lithosphere exhibits complex deformation across broad regions, challenging simplistic te...
International audienceThe Greater Caucasus (GC) Mountains within the central Arabia-Eurasia collisio...
Convergent plate margins serve as the principal locations of lithospheric assembly and destruction w...
Apatite fission-track analysis and thermochronologic statistical modeling of Precambrian–Oligocene p...
International audienceThis article summarizes the geodynamic evolution of the Caucasus mountain belt...
International audienceWe appreciate the interest of Dr. Yurdal Genç and Dr. Tekin Yürür in the work ...
International audienceThis article summarizes the geodynamic evolution of the Variscan to Mesozoic T...
The western Greater Caucasus formed by the tectonic inversion of the western strand of the Greater C...
none6siPublished online: 27 October 2015Low-temperature thermochronological data for the Eurasian fo...
The Greater Caucasus (GC) fold-and-thrust belt lies on the southern deformed edge of the Scythian Pl...
Shafaii Moghadam et al. (2020) contribute important new data on Late Cretaceous-Tertiary subduction-...
A continent-oceanic island arc collision model was proposed as a new geodynamic scenario for the evo...
The Variscan structures of the Caucasus region are still quite difficult to decipher, they certainly...
In our paper (Hollingsworth et al., 2008), we present a model of how the distribution of active faul...
Comparison of plate convergence with the timing and magnitude of upper crustal shortening in collisi...
Continental lithosphere exhibits complex deformation across broad regions, challenging simplistic te...
International audienceThe Greater Caucasus (GC) Mountains within the central Arabia-Eurasia collisio...
Convergent plate margins serve as the principal locations of lithospheric assembly and destruction w...
Apatite fission-track analysis and thermochronologic statistical modeling of Precambrian–Oligocene p...
International audienceThis article summarizes the geodynamic evolution of the Caucasus mountain belt...
International audienceWe appreciate the interest of Dr. Yurdal Genç and Dr. Tekin Yürür in the work ...
International audienceThis article summarizes the geodynamic evolution of the Variscan to Mesozoic T...
The western Greater Caucasus formed by the tectonic inversion of the western strand of the Greater C...
none6siPublished online: 27 October 2015Low-temperature thermochronological data for the Eurasian fo...
The Greater Caucasus (GC) fold-and-thrust belt lies on the southern deformed edge of the Scythian Pl...
Shafaii Moghadam et al. (2020) contribute important new data on Late Cretaceous-Tertiary subduction-...
A continent-oceanic island arc collision model was proposed as a new geodynamic scenario for the evo...
The Variscan structures of the Caucasus region are still quite difficult to decipher, they certainly...
In our paper (Hollingsworth et al., 2008), we present a model of how the distribution of active faul...
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