GEOLOGY AND ORIGIN OF THE ALBITE DEPOSITE OF THE ÇİNE SUBMASSIF, SOUTHERN MENDERES MASSIF (SW-TURKEY)

Yıl 2000, Cilt: 122 Sayı: 122, 23 - 30, 01.03.2000

Ali Uygun Ahmet Gümüşçü

Öz

Around 250 albite occurrences are recorded in the Cine Submassif
that represents the southern part of the Menderes Massif, from where annually
1.7 million tons of Na-feldspar is produced. The study area is covered by the
widespread exposures of the Pan-African Precambrian core-complex of the
southern Menderes Massif. The albite deposits are mainly within the
meta-pegmatites, located along NNW-SSE trending tectonic zones. In this study,
the effects of the Alpine metamorphic and metasomatic events on the
albitization process are discussed, and the importance of the younger
intrusives within the Cine Submassif are emphasized. Moreover, the geometry,
dimensions and petrologic properties of the albite deposits are explained and
the quality of the various market products is documented.

Anahtar Kelimeler

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Kaynakça

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