• BALIKESİR-SINDIRGI-DÜVERTEPE KAOLEN

Abstract
The Turkish land lies within the Alpine orogenic belt and has been affected by intense tectonic
movement repeatedly since earyy Paleozoic. Such a long history of geologic evoluation brought localization
of various type kaolin clay deposits.
The Turkish kaolin is characterized by a significant occurrence of hydrothermal kaolin deposits. Sevaral
productivite kaolin deposits occur in the Neogene terrestrial tuffaceous formations, and their mode of
occurrence is remarkably controlled by pre-and post-alteration tectonic movements. Some of hydrothermal
kaolin deposits occur in the Pre-Neogene rocks, forexample the Cretaceous volcanic sediments in the Black
Sea region and some metamorphic formations in the Eastern Anatolia.
The most extensive kaolin deposit in Turkey is located at the Sindirgi-Düvertepe Region in Balikesir
province. The total reserve of this area, where almost ali the Turkish Ceramic Producers exploit kaolin, is
over 70 million tons. The area contains kaolin suitable also paper and refractory industries beside ceramic.
Annual production is abaut 60 thausand tons. Kaolinization in the region has occured in the result of the
hydrothermal alteration of volcanic-sedimantary material. The DTA investigation of various samples revealed
that the deposit contained kaolin and alunitic kaolin in general.

Rapor Özellikleri
Rapor No 13318
Rapor Adı BALIKESİR-SINDIRGI-DÜVERTEPE KAOLEN
Konu KAOLEN
Yer - Konum BALIKESİR-SINDIRGI
Dil İNGİLİZCE
Yayın Tarihi 1986
Yazarlar BİRKAN, Ö KARTAL, G.

BALIKESİR-SINDIRGI-DÜVERTEPE KAOLEN

  • Markalar MTA
  • Ürün Kodu: DR13318
  • Stok Durumu: Stokta var
  • 48,00TL


Etiketler: BALIKESİR, SINDIRGI, DÜVERTEPE, KAOLEN