GEODYNAMIC PHASES OF THE ARAÇ MASSIF, WESTERN PONTIDS, KASTAMONU, TURKEY

This paper is concerned with the geological, mineralogical and geochemical properties of Araç massif. The Araç massif is mainly composed of ophiolites and metamorphic rocks. The age of the metamorphic rocks, which are dominant rock group in the study area, are ranging from Pre-Malm to Upper Cretaceous. K-Ar age determination were performed in hornblendes derived from amphibolites, which are previously thought to be Precambriam age in the study area. According to the KAr age results, which gives 130-146 ma, suggests that the amphibolites were affected by retrograde metamorphism, which took place in Berriasian (Lower Cretaceous). These ages are believed to represent the metamorphism age, not the occurence age of the formation. Because of this, the occurence of the Bekirçay formation should have taken place before this retrograde metamorphism. Some very intensely altered metaophiolitic bloks were found as xenolits in Bekirçay metamorphic units. Therefore the age of the metaophiolites shoud have been older than the Bekirçay formation. Mercimekdere metaophiolites were overlain, not only by Bekirçay formation, but also by Kavacık formation, which is represented by graphite-garnet micaschist in the study area. The Bekirçay formation and the other above mentioned formation is overlayed discordantly by Palaeozoic metasediments, namely the Dumantepe formation, which consists of various low grade schists and phyllites. The Mesozoic is represented by Yongalıdağ formation, Pelitveren ophiolitic melange and serpentinized, carbonatized and sillicified rocks, so called listwaenites of the Gemiköy formation. Finally, this Mesozoic formations were transgresively superseded by biosparite and biomicrite units of the Araç formation. The area and surroundings were then affected by post Eocene faulting. According to the geochemical investigations, it can easily be said that ultramafic rocks occured as mantle fractionates and all mafic rocks were originated from subalcaline tholeiitic magma. Amphibolites are found as metaluminous, while garnet-micaschist are peraluminous and epidoteamphibolites show both character in different places. Carbonaceous rocks in the study area are found to be rich in calcite rather than dolomite and other minerals.

Keywords:

GEODYNAMIC, PHASES ARAÇ MASSIF,

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ISSN: 0026-4563
Yayın Aralığı: Yılda 3 Sayı
Başlangıç: 1950
Yayıncı: Cahit DÖNMEZ

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