Akademik Veri Yönetim Sistemi
INTERNATIONAL JOURNAL OF EARTH SCIENCES, cilt.89, sa.4, ss.757-765, 2001 (SCI-Expanded, Scopus)
The Simav metamorphic core complex of the northern Menderes massif, western Turkey, consists of a plutonic (Tertiary) and metamorphic (Precambrian) core (footwall) separated from an allochthonous cover sequence (hanging wall) by a low-angle, ductile-to-brittle, extensional fault zone (i.e. detach ment fault). The core rocks below the detachment fault are converted into mylonites with a thickness of a few hundred metres. Two main deformation events have affected the core rocks. The first deformational event (D-1) was developed within the Precambrian metamorphic rocks. The second event (D-2), associated with the Tertiary crustal extension. includes two distinct stages. Stage one is the formation of a variably developed ductile (mylonitic) deformation (D-2d) in metamorphic and granitic core rocks under greenschist facies conditions. The majority of the mylonites in the study area have foliations that strike NNW to NNE and dip SW to SE. Stretched quart and feldspar grains define the mineral lineation trending SW-NE direction and plunging gently to SW. The kinematic indicators indicate a top-to-NE sense of shear. Stage two formation of brittle deformation (D-2b) that affected all core and cover rocks, D-2b involves the and high-angle normal development of cataclasites faults. An overall top towards the north sense of shear for the ductile (mylonitic) fabrics in the core rocks is consistent with the N-S regional extension in western Turkey.