TY  - JOUR
A1  - Oberhänsli, Roland
A1  - Goffe, B.
A1  - Bousquet, Romain
T1  - Record of a HP-LT metamorphic evolution in the Valais zone : Geodynamics implications
Y1  - 1995
SN  - 0392 - 758X
ER  - 
TY  - JOUR
A1  - Jolivet, L.
A1  - Goffe, B.
A1  - Bousquet, Romain
A1  - Oberhänsli, Roland
A1  - Michard, Andre
T1  - Detachments in high-pressure mountain belts, Tethyan examples
Y1  - 1998
ER  - 
TY  - JOUR
A1  - Poupeau, G.
A1  - Saddiqi, O.
A1  - Michard, Andre
A1  - Goffe, B.
A1  - Oberhänsli, Roland
T1  - Late thermal evolution of the oman mountains subophiolitic windows : apatite fission-track thermochronology
Y1  - 1998
SN  - 0091-7613
ER  - 
TY  - JOUR
A1  - Oberhänsli, Roland
A1  - Wendt, A. S.
A1  - Goffe, B.
A1  - Michard, Andre
T1  - Detrital chromites in metasediments of East-Arabian continental margin in te Saih Hatat area : constraints for the palaeogeographic setting of the Hawasina and Semail basins (Oman Mountains)
Y1  - 1999
ER  - 
TY  - JOUR
A1  - Oberhänsli, Roland
A1  - Bousquet, Romain
A1  - Goffe, B.
T1  - Comment to "Chloritoid composition and formation in the eastern Central Alps : a comparison between Penninic and Helvetic occurrences" by M. Rahn, M. Steinmann and M. Frey
Y1  - 2003
SN  - 0036-7699
ER  - 
TY  - JOUR
A1  - Jolivet, L.
A1  - Rimmele, Gaetan
A1  - Oberhänsli, Roland
A1  - Goffe, B.
A1  - Candan, O.
T1  - Correlation of syn-orogenic tectonic and metamorphic events in the Cyclades, the Lycian nappes and the Menderes massif : Geodynamic implications
N2  - The recent discovery of HP-LT parageneses in the basal unit of the Lycian nappes and in the Mesozoic cover of the Menderes massif leads us to reconsider and discuss the correlation of this region with the nearby collapsed Hellenides in the Aegean domain. Although similarities have long been pointed Out by various authors, a clear correlation has not yet been proposed and most authors insist more on differences than similarities. The Menderes massif is the eastern extension of the Aegean region but it has been less severely affected by the Aegean extension during the Oligo-Miocene. It would thus be useful to use the structure of the Menderes massif as an image of the Aegean region before a significant extension has considerably reduced its crustal thickness. But the lack of correlation between the two regions has so far hampered Such comparisons. We describe the main tectonic units and metamorphic events in the two regions and propose a correlation. We then show possible sections of the two regions before the Aegean extension and discuss the involvement of continental basement in the Hellenic accretionary complex. In our interpretation the Hellenic- Tauric accretionary complex was composed of stacked basement and cover units which underwent variable P-T histories. Those which were not exhumed early enough later followed a high-T evolution which led to partial melting in the Cyclades during post-orogenic extension. Although the Menderes massif contains a larger volume of basement units it does not show significant evidence for the Oligo-Miocene migmatites observed in the center of the Cyclades suggesting that crustal partial melting is strictly related to post-orogenic extension in this case
Y1  - 2004
SN  - 0037-9409
ER  - 
TY  - JOUR
A1  - Bousquet, Romain
A1  - Goffe, B.
A1  - Le Pichon, X.
A1  - de Capitani, Christian
A1  - Chopin, C.
A1  - Henry, P.
T1  - Subduction factory : 1. Theoretical mineralogy, densities, seismic wave speeds, and H2O contents
Y1  - 2005
ER  - 
TY  - JOUR
A1  - Rimmele, Gaetan
A1  - Parra, T.
A1  - Goffe, B.
A1  - Oberhänsli, Roland
A1  - Jolivet, L.
A1  - Candan, O.
T1  - Exhumation paths of high-pressure-low-temperature metamorphic rocks from the Lycian Nappes and the Menderes Massif (SW Turkey) : a multi-equilibrium approach
N2  - The Menderes Massif and the overlying Lycian Nappes occupy an extensive area of SW Turkey where high-pressure- low-temperature metamorphic rocks occur. Precise retrograde P-T paths reflecting the tectonic mechanisms responsible for the exhumation of these high-pressure-low-temperature rocks can be constrained with multi-equilibrium P-T estimates relying on local equilibria. Whereas a simple isothermal decompression is documented for the exhumation of high-pressure parageneses from the southern Menderes Massif, various P-T paths are observed in the overlying Karaova Formation of the Lycian Nappes. In the uppermost levels of this unit, far from the contact with the Menderes Massif, all P-T estimates depict cooling decompression paths. These high-pressure cooling paths are associated with top-to-the-NNE movements related to the Akcakaya shear zone, located at the top of the Karaova Formation. This zone of strain localization is a local intra-nappe contact that was active in the early stages of exhumation of the high-pressure rocks. In contrast, at the base of the Karaova Formation, along the contact with the Menderes Massif, P-T calculations show decompressional heating exhumation paths. These paths are associated with severe deformation characterized by top-to-the-east shearing related to a major shear zone (the Gerit shear zone) that reflects late exhumation of high-pressure parageneses under warmer conditions
Y1  - 2005
SN  - 0022-3530
ER  -