On the bases of geochemical properties and lithostragraphic location of the Payas mineralization region can be
differentiated into three groups: 1- Limestone wall rock represents by Paşanın Eğreği plateau, Sarıyokuş Mağarabaşı site and
Kozlu dere appearances. 2- Sandstone wall rock represents by Fındık plateau-l appearences. 3- Iron enrichment serpentinite
wall rock represents by Findik plateau-II appearances. According to the results of chemical analyses of these three groups Fe,
Ca, and P elements are behaviour together, Al, Si, Ti and K elements group behave parallel to other group formation. The
elements which have parallel behaviour distribute reversibly with each other. This situation indicates two different genesis. The
enrichment of iron in the mineralization is derived from ultrabazic rocks. The lateritic iron which is formed due to of ultrabazic
rocks lateritization is transported and precipitated in karstic cavity forming the mineralization. The sources of aluminium can
also be explained by the same way. However in order to give sufficient explanation more data is required.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Temmuz 1992 |
Yayımlandığı Sayı | Yıl 1992 Cilt: 114 Sayı: 114 |
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