TY  - JOUR
T1  - YENİŞARBADEMLİ (ISPARTA, TÜRKİYE) BATISINDAKİ MAFİK-ORTAÇ DAYKLARDAKİ EPİDOTLARIN MİNERALOJİSİ VE JEOKİMYASAL KARAKTERİ
TT  - MINERALOGICAL AND GEOCHEMICAL CHARACTERISTICS OF EPIDOTES IN THE MAFIC-INTERMEDIATE DYKES IN WEST OF YENİŞARBADEMLİ (ISPARTA, TURKEY)
AU  - Dedeoğlu Yıldız, Deniz
PY  - 2025
DA  - March
Y2  - 2025
DO  - 10.21923/jesd.1587413
JF  - Mühendislik Bilimleri ve Tasarım Dergisi
JO  - MBTD
PB  - Süleyman Demirel Üniversitesi
WT  - DergiPark
SN  - 1308-6693
SP  - 275
EP  - 285
VL  - 13
IS  - 1
LA  - tr
AB  - Beydağları-Karacahisar otoktonun temelini oluşturan Bozburun şistini kesen dayklar; bazalt, bazaltik andezit ve andezit bileşimlidir. Bazalt, bazaltik andezit, ve andezit bileşimli kayaçlarda bulunan epidotların incelenmesi bu çalışmanın konusudur. Özşekilli ve yarı özşekilli epidotların, hem magmadan doğrudan kristallenmiş hem de biyotit, hornblend ve plajioklas minerallerinin alterasyonu sonucunda oluştuğu tespit edilmiştir. Magmatik epidotların, Ps içeriği %25-32 arasında olup, genellikle allanit çekirdekli ve düşük TiO2 konsantrasyonuna (
KW  - Batı-Orta Toroslar
KW  - Dayk
KW  - Mineral Kimyası
KW  - Epidot
N2  - The dykes cutting the Bozburun schist forming the base of the Beydağları-Karacahisar autochthonous are basalt, basaltic andesite and andesite in composition. The examination of the epidotes found in these basalt, basaltic andesite and andesite rocks is the subject of this study. It has been determined that euhedral and subhedral epidotes are formed as a result of both direct crystallization from magma and alteration of biotite, hornblende and plagioclase minerals. The Ps content of magmatic epidotes is between 25-32% and generally has an allanite core and low TiO2 concentration (
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UR  - https://doi.org/10.21923/jesd.1587413
L1  - https://dergipark.org.tr/tr/download/article-file/4375863
ER  -