Use of tourmaline as a potential petrogenetic indicator in the determination of host magma: CRS, XRD and PED-XRF methods

GÜLLÜ B., KADIOĞLU Y. K.

SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY, cilt.183, ss.68-74, 2017 (SCI-Expanded) identifier identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 183
  • Basım Tarihi: 2017
  • Doi Numarası: 10.1016/j.saa.2017.04.032
  • Dergi Adı: SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.68-74
  • Anahtar Kelimeler: Confocal Raman spectroscopy, Schorl-elbaite, Tourmaline, Central Anatolia (Turkey), X-RAY-FLUORESCENCE, CRYSTAL-CHEMISTRY, RAMAN-SPECTROSCOPY, SCHORL, MINERALS, SPECTRA, ELBAITE, SERIES
  • Ankara Üniversitesi Adresli: Evet

Özet

Tourmaline defines a group of complex borosilicate forms as accessory mineral in igneous and metamorphic rocks and they act an important role in the interpretation of the chemical composition changes of the composition of the host fluid of the magma.