Fibrous foitite from Sebinkarahisar, Giresun Pb-Zn-Cu-(U) mineralized area, Northern Turkey

Fuat Yavuz*, Muazzez Çelik, Necati Karakaya

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

11 Citations (Scopus)

Abstract

Fibrous foitite occurs in cavities in quartz veins near Sebinkarahisar town, Giresun mineralized area [Pb-Zn-Cu-(U)], in northern Turkey. Veins of quartz + fibrous tourmaline generally cut monzonitic and syenitic rocks. Acicular and hairlike light gray crystals of foitite have a mean composition of []0.43Na0.52Ca0.07 (Fe1.55Mn0.08Mg0.52Al0.67Ti0.01) Al6(BO3)3 Si6 O18 (OH, O)3 (OH)1. The crystals of this low-temperature tourmaline radiate from irregular patches of schorl in cavities in quartz veins. Each fiber is zoned along its length with respect to Fe, Mn, Mg, Ca, Na, K, and P. The fibrous foitite from the Sebinkarahisar area contains higher Mg, Ca and Na contents than that from southern California and Elba.

Original languageEnglish
Pages (from-to)155-161
Number of pages7
JournalCanadian Mineralogist
Volume37
Issue number1
Publication statusPublished - Feb 1999

Keywords

  • Alkali-deficient
  • Cavity
  • Fibers
  • Foitite
  • Northern Turkey
  • Pb-Zn-Cu-(U) mineralization
  • Quartz vein
  • Sebinkarahisar
  • Tourmaline

Fingerprint

Dive into the research topics of 'Fibrous foitite from Sebinkarahisar, Giresun Pb-Zn-Cu-(U) mineralized area, Northern Turkey'. Together they form a unique fingerprint.

Cite this