Results 81 to 90 of about 1,426 (164)

Spatial patterns of erosion and landscape evolution in a bivergent metamorphic core complex revealed by cosmogenic 10Be: The central Menderes Massif (western Turkey) [PDF]

open access: yes, 2019
In extensional provinces with low-angle normal faulting (such as the Aegean region), both tectonic processes and erosion induce landscape change, but their interaction during the evolution of topography and relief accompanying continental extension has ...
Akal, Cüneyt   +6 more
core   +3 more sources

Plio-quaternary evolution of the Kucuk Menderes Graben southwestern Anatolia, Turkey [PDF]

open access: yes, 2005
The Kucuk Menderes Graben (KMG) is part of the horst-graben system of southwestern Anatolia (Turkey), bounded by the Bozdag horst in the north and the Aydin horst in the south.
Demirci, C   +3 more
core   +1 more source

Protoliths and phase petrology of whiteschists [PDF]

open access: yes, 2018
Whiteschists appear in numerous high- and ultrahigh-pressure rock suites and are characterized by the mineral assemblage kyanite+talc (+-quartz or coesite).
de Capitani, Christian   +2 more
core  

A Quaternary Solution Model for White Micas Based on Natural Coexisting Phengite-Paragonite Pairs [PDF]

open access: yes, 2017
A thermodynamic model for the quaternary white mica solid solution with end-members muscovite-Mg-celadonite-paragonite-Fe-celadonite (Ms-MgCel-Pg-FeCel) is presented.
ABART, R.   +2 more
core  

Exhumation of high-pressure rocks driven by slab rollback

open access: yes, 2008
International audienceRocks metamorphosed under high-pressure (HP) and ultra high-pressure (UHP) conditions in subduction zones come back to the surface relatively soon after their burial and at rates comparable to plate boundary velocities.
Brun, Jean-Pierre, Faccenna, C.
core   +3 more sources

Grands gisements d'albite dans le massif métamorphique de Menderes (Turquie occidentale)

open access: yesComptes Rendus. Géoscience, 2005
Les gisements d'albite de Turquie occidentale sont situés au sein de gneiss, dans la partie basale du massif métamorphique de Menderes. Les plus importants gisements se trouvent dans la zone de minéralisation de Karadere, qui est un anticlinorium de 15 km de longueur de direction N10–30E.
openaire   +1 more source

Mesozoic-Tertiary structural evolution of an extensional gneiss dome—the Kesebir-Kardamos dome, eastern Rhodope (Bulgaria-Greece) [PDF]

open access: yes, 2018
The tectonic evolution of the Rhodope massif involves Mid-Cretaceous contractional deformation and protracted Oligocene and Miocene extension. We present structural, kinematic and strain data on the Kesebir-Kardamos dome in eastern Rhodope, which ...
Bonev, Nikolay   +2 more
core  

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