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GeoRef Categories
Era and Period
Epoch and Age
Book Series
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Availability
Kutahya Turkey
The Gümüşköy (Kütahya, Turkey) kaolin deposit and its ceramic properties Available to Purchase
Genetic Characteristics of the Gozecukuru As-Sb Deposits near Kutahya, Turkey Available to Purchase
The Şahin village (Kütahya, Turkey) clay deposit and its possible utilization Available to Purchase
Origin of the Basoren (Kutahya, W Turkey) bentonite deposits Available to Purchase
Fontarnauite, (Na,K) 2 (Sr,Ca)(SO 4 )[B 5 O 8 (OH)](H 2 O) 2 , a New Sulfate-borate Mineral from DoĞanlar (emet), KÜtahya Province, Western Anatolia, Turkey Available to Purchase
Veatchite-A, a new modification of veatchite Available to Purchase
The effect of initial water content on the swelling pressure of soils Available to Purchase
Analysis of tiles produced from a schist material and their ultraviolet, near-infrared, mid-infrared, longwave-infrared and far-infrared spectra Available to Purchase
Quantification of Fragment Size Distribution of Clay-Bearing Rocks after Slake Durability Testing Available to Purchase
Effect of ulexite concentrator waste on the physical and mechanical properties and sintering behaviour of floor tile bodies Available to Purchase
Petrogenesis and geodynamic evolution of the Late Neoproterozoic post-collisional felsic magmatism in NE Afyon area, western central Turkey Available to Purchase
Abstract In western Turkey, Late Neoproterozoic basement rocks are represented by variably deformed metasedimentary and meta-igneous rocks within different tectonostratigraphical units that make up the Alpine Tauride–Anatolide Platform. In the Kütahya–Bolkar Dagı unit to the NE of Afyon this basement mainly includes garnet-bearing mica schists intruded by metamorphic granitic rocks with relict porphyritic textures. The youngest zircon ages obtained from the granitic rocks by the single zircon evaporation method are 542±5.0 Ma on average, which correlate with the Late Pan-African–Cadomian granitic magmatism. The granitic rocks are rhyodacitic or dacitic and peraluminous in composition, and display geochemical characteristics of I-type (tonalite–trondhjemite–granodiorite (TTG) source) felsic intrusive rocks. Trace and rare earth element patterns with distinct depletion in Rb, K, Nb, Sr, P and Ti relative to the other trace elements correlate very well with a Proterozoic TTG source. The petrogenetic modelling also implies that they were developed by partial melting of a TTG source by 20% fractional melting plus 20% Rayleigh fractional crystallization. The emplacement temperatures estimated by using zircon (790–820 °C), apatite and monazite saturation thermometry are about 827–1035 °C; these are in accordance with I-type rather than S-type granite melts. A geochemical comparison of the NE Afyon granitic rocks with the coeval quartz-porphyries in the Sandikli area of the Geyik Dag tectonic unit suggests that the latter may represent the more evolved felsic part of the Cadomian magmatism. Hence, both basement complexes are parts of the same Gondwanan terrane and represent the eastern continuation of the North African–Southern European terrane assemblage.