International audienceThe development of metamorphic core complexes (MCC) corresponds to a mode of lithospheric continental stretching that follows collision. In most of the models that explain the formation of the MCC, high thermal gradients are necessary to weaken the lower crust and to induce its ascent. Such models fail to explain the exhumation of high pressure-low temperature metamorphic rocks in metamorphic core complex structures as observed in the Cycladic Blueschists in the Aegean domain. Besides, account for the lithological crustal stratification induced from collision has never been tested. In this paper, we use fully coupled thermomechanical modelling to investigate the impact of structural heritage and initial thermal gradien...
High Pressure - Low Temperature (HP-LT) rocks testify for burying and exhumation of crustal material...
International audiencePre-thickened hot orogenic crust is often considered a necessary condition for...
International audienceDeep crustal and mantle rocks are exhumed in core complex mode of extension in...
International audienceThe development of metamorphic core complexes (MCC) corresponds to a mode of l...
International audienceMetamorphic Core Complexes (MCCs) form when a thickened domain with a low-stre...
The development of metamorphic core complexes (MCCs) in a thickened continental lithosphere is studi...
The mechanics of metamorphic core complex (MCC) development and the associated process of lower crus...
International audienceThe Aegean domain is a well-suited place to study the formation of metamorphic...
The development of metamorphic core complexes (MCCs) in a thickened continental lithosphere is studi...
International audienceThe Mediterranean realm shaped by extensive back-arc extension after multiple ...
Metamorphic core complexes are classically interpreted to have formed during crustal extension, alth...
International audienceEven if the seminal comprehensive descriptions of Metamorphic Core Complexes (...
High Pressure - Low Temperature (HP-LT) rocks testify for burying and exhumation of crustal material...
International audiencePre-thickened hot orogenic crust is often considered a necessary condition for...
International audienceDeep crustal and mantle rocks are exhumed in core complex mode of extension in...
International audienceThe development of metamorphic core complexes (MCC) corresponds to a mode of l...
International audienceMetamorphic Core Complexes (MCCs) form when a thickened domain with a low-stre...
The development of metamorphic core complexes (MCCs) in a thickened continental lithosphere is studi...
The mechanics of metamorphic core complex (MCC) development and the associated process of lower crus...
International audienceThe Aegean domain is a well-suited place to study the formation of metamorphic...
The development of metamorphic core complexes (MCCs) in a thickened continental lithosphere is studi...
International audienceThe Mediterranean realm shaped by extensive back-arc extension after multiple ...
Metamorphic core complexes are classically interpreted to have formed during crustal extension, alth...
International audienceEven if the seminal comprehensive descriptions of Metamorphic Core Complexes (...
High Pressure - Low Temperature (HP-LT) rocks testify for burying and exhumation of crustal material...
International audiencePre-thickened hot orogenic crust is often considered a necessary condition for...
International audienceDeep crustal and mantle rocks are exhumed in core complex mode of extension in...