Late magmatic – hydrothermal tourmaline occurrences within leucogranites in NW Anatolia (Turkey): Mineral chemistry and genetic implications

AYSAL N., Öngen S., HANİLÇİ N., KASAPÇI C., LAÇİN D., Boroğlu M. Ş., ...Daha Fazla

Chemie der Erde, cilt.81, 2021 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 81
  • Basım Tarihi: 2021
  • Doi Numarası: 10.1016/j.chemer.2020.125676
  • Dergi Adı: Chemie der Erde
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Aerospace Database, Aquatic Science & Fisheries Abstracts (ASFA), Artic & Antarctic Regions, Chemical Abstracts Core, INSPEC, Civil Engineering Abstracts
  • Anahtar Kelimeler: Late-stage magmatic evolution, Tourmaline, Mineral chemistry, Hydrothermal fluid, BIGA PENINSULA, TRACE-ELEMENT, AU DEPOSIT, BORON, EVOLUTION, INDICATOR, FLUID, CLASSIFICATION, EQUILIBRIA, BEARING
  • İstanbul Üniversitesi Adresli: Hayır

Özet

© 2020 Elsevier GmbHNumerous Oligo-Miocene plutonic and associated aplite-pegmatite rocks occur in the Western Anatolian Magmatic Complex. However, only the plutons of Namazgah, Karadağ, Soğucak and Karadoru, in the Biga Peninsula, host three different types of tourmaline: disseminated, nodular, and vein-type. These all fall into the alkali subgroup and schorl-oxy-schorl-dravite-oxy-dravite solid solution series. This study shows they were formed during late magmatic to hydrothermal stages in the roof sections (at shallow crustal levels) of the granitoid intrusions. Tourmaline compositions remained fairly homogeneous during the formation and evolution of each stage.