Listwaenitization and enrichment of precious metals in the hydrothermal mineralization zones of serpentinites in Sugecer-Van (Eastern Anatolia, Turkey)

Üner T.

GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS, cilt.20, sa.1, ss.68-79, 2020 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 20 Sayı: 1
  • Basım Tarihi: 2020
  • Doi Numarası: 10.1144/geochem2018-087
  • Dergi Adı: GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Agricultural & Environmental Science Database, Aquatic Science & Fisheries Abstracts (ASFA), CAB Abstracts, Geobase, Pollution Abstracts
  • Sayfa Sayıları: ss.68-79
  • Anahtar Kelimeler: alteration, serpentinites, listwaenites, ophiolites, Eastern Anatolia, SILICA-CARBONATE ALTERATION, OCEANIC-CRUST, ABYSSAL PERIDOTITES, ULTRAMAFIC ROCKS, SAMAIL OPHIOLITE, HIGH PLATEAU, GEOCHEMISTRY, GOLD, LISTVENITE, DESERT
  • Van Yüzüncü Yıl Üniversitesi Adresli: Evet

Özet

An ophiolitic complex containing hydrothermally altered serpentinized ultramafic rocks was studied in an area on the eastern side of Lake Van near the village of Sugecer, Eastern Anatolia. Field observations and petrographic and geochemical analyses clearly showed that the serpentinites were altered to listwaenites via silicification and carbonatization. The listwaenites were classified as type-I and type-II listwaenites based on their mineral composition. The type-I listwaenites contained carbonate minerals, rare serpentine minerals, chromite and mariposite, whereas the type-II listwaenites contained mainly silicate minerals. The listwaenites were enriched in Au, As, Cu, Ni and Co relative to the serpentinites. The listwaenites also showed chondrite-normalized enrichment in light rare earth elements and depletion in heavy rare earth elements. The effects of tectonism were widely observed in the study area. Mineral enrichment in the Sugecer region was shown to be associated with the transport of minerals by hydrothermal fluids under the influence of tectonism.