Al(Fe,Ti,Si)-mobility and secondary mineralization implications: A case study of the karst unconformity diasporite-type bauxite horizons in Milas (Mugla), Turkey

HATİPOĞLU M.

JOURNAL OF AFRICAN EARTH SCIENCES, cilt.60, sa.3, ss.175-195, 2011 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 60 Sayı: 3
  • Basım Tarihi: 2011
  • Doi Numarası: 10.1016/j.jafrearsci.2011.02.009
  • Dergi Adı: JOURNAL OF AFRICAN EARTH SCIENCES
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.175-195
  • Anahtar Kelimeler: Metamorphic remobilized reactions, Submicroscopic paragenesis, Diaspore (zultanite), Al-mobility, Karst unconformity diasporite-type bauxite horizons, Menderes Massif, Turkey, SOUTHERN MENDERES MASSIF, HIGH-PRESSURE METAMORPHISM, X-RAY-DIFFRACTION, DEPOSITS, GEOCHEMISTRY, METABAUXITES, GEOCHRONOLOGY, DEHYDRATION, GEOLOGY, ORIGIN
  • Dokuz Eylül Üniversitesi Adresli: Evet

Özet

The Paleogene aged metabauxite deposit in the Upper Cretaceous-Early Paleogene aged marble sequence within the southwestern Menderes Massif in the Ilbir Mountains of the Milas (Mugla) region of SW Turkey comprises many initially karst unconformity-type bauxite horizons with unusual Al-mobility. Thus, it displays singular geochemical and mineralogical implications.