Results 111 to 120 of about 1,426 (164)
Some of the next articles are maybe not open access.
Material properties of the Menderes Massif Marbles from SW Turkey
Engineering Geology, 2005Marbles are extensively quarried at four different stratigraphical levels from Permo-Carbonifereous to Paleogene in the southern flank of the Menderes Massif in SW Turkey. These marbles differ in color, texture and pattern depending on their stratigraphical levels and are well known in the international trade as the Mugla Black (Permo-Carbonifereous ...
YAVUZ, ALİ BAHADIR, Koca, MY, Turk, N
openaire +4 more sources
Eclogites within the Menderes Massif/western Turkey
Lithos, 1997Metagabbros in the core series of the Menderes Massif, for some time considered as post orogenic Miocene intrusives, revealed a strong poly-metamorphic history. The metagabbro bodies exhibit a pronounced zonation. Within their cores, igneous minerals are still preserved.
Oberhänsli, Roland (Prof. Dr.) +3 more
openaire +5 more sources
The southern Menderes Massif (western Turkey): geochronology and exhumation history
Geological Journal, 2000AbstractIn the southern flank of the Menderes Massif, western Turkey, an E–W‐trending quartz–mica vein was recognized in the augen gneisses of the so‐called ‘core’ series. Rb‐Sr determinations of two undeformed or slightly deformed mica books from the vein yielded Palaeocene–Early Eocene ages (c. 62–43 Ma) for the vein formation.
Erdi̇n Bozkurt, Muharrem Satir
exaly +4 more sources
Monazite ages and the evolution of the Menderes Massif, western Turkey
International Journal of Earth Sciences, 2005The Menderes Massif experienced polyphase deformation, but distinguishing Pan-African events from Alpine tectono-metamorphic evolution, and discriminating Eocene–Oligocene shortening from recent extension remain controversial. To address this, monazite in garnet-bearing rocks from the massif’s Gordes, Central, and Cine sections were dated in thin ...
E. J. Catlos, Ibrahim �emen
openaire +3 more sources
Late Alpine evolution of the central Menderes Massif, western Turkey
International Journal of Earth Sciences, 2001The central Menderes Massif (western Turkey) is characterized by an overall dome-shaped Alpine foliation pattern and a N–NNE-trending stretching lineation. A section through the southern flank of the central submassif along the northern margin of Buyuk Menderes graben has been studied.
Erdin Bozkurt
openaire +3 more sources
The Menderes Massif geothermal province
Geothermics, 1970Abstract In the framework of the geothermal energy survey of western Anatolia Project, sponsored by the Mineral Research and Exploration Institute of Turkey and the United Nations, general geological investigations were made of the various geothermal provinces of western Anatolia.
A. Ten Dam, A.I. Khrebtov
openaire +1 more source
Multistage exhumation of the Menderes Massif, western Anatolia (Turkey)
International Journal of Earth Sciences, 2001Structural analyses along selected transects across the Menderes Massif and incorporation of existing data have resulted in a synthetic cross section across southwestern Turkey.
Lips, ALW +4 more
openaire +4 more sources
Bivergent extension in orogenic belts: The Menderes massif (southwestern Turkey)
Geology, 1995The central Menderes massif is characterized by an overall dome-shaped foliation pattern and a north-northeast‐trending stretching lineation. The asymmetry of shear bands and quartz c-axis fabrics on either side of the structural dome demonstrate a top to thenorth-northeastshearsenseinthenorthernpartandatoptothesouth-southwestshear sense in the ...
PASSCHIER, CW +3 more
openaire +2 more sources
Metamorphic history of the southern Menderes massif, western Turkey
Geological Society of America Bulletin, 2002Metamorphic mineral compositions and textures are integrated with microstructures to test tectonic models for the construction and exhumation of a mid-crustal terrane in western Turkey. The southern Menderes massif, part of the Alpine orogen, is composed of a tilted sequence of metasedimentary rocks that structurally overlies orthogneiss.
Whitney, DL, Bozkurt, Erdin
openaire +2 more sources
Miocene NNE-directed extensional unroofing in the Menderes Massif, southwestern Turkey
Journal of the Geological Society, 1995Structural investigations in the central part of the Menderes Massif (Ödemiº-Kiraz submas-sif) reveal the presence of a large-scale, low-angle extensional shear zone with a top-to-the-N-NE shear sense. Regional ductile deformation was accompanied by the intrusion of two syntectonic granodiorites that have been dated with the 40
HETZEL, R +3 more
openaire +2 more sources