Origin and nature of the mineralizing fluids of thrust zone fluorites in Celikhan (Adiyaman, Eastern Turkey)

Basit Öğe Kaydı
dc.authoridSağıroğlu, Ahmet/0000-0001-8329-0506
dc.authoridSasmaz, Ahmet/0000-0003-1154-732X
dc.authoridAkgul, Bunyamin/0000-0002-2620-543X
dc.authorwosidSASMAZ, Ahmet/V-8309-2018
dc.authorwosidSağıroğlu, Ahmet/D-1933-2013
dc.authorwosidSasmaz, Ahmet/V-3954-2018
dc.authorwosidAkgul, Bunyamin/V-8334-2018
dc.contributor.authorSasmaz, A
dc.contributor.authorÖnal, A
dc.contributor.authorSagiroglu, A
dc.contributor.authorÖnal, M
dc.contributor.authorAkgul, B
dc.date.accessioned2024-08-04T20:14:46Z
dc.date.available2024-08-04T20:14:46Z
dc.date.issued2005
dc.departmentİnönü Üniversitesien_US
dc.description.abstractThe Celikhan fluorite mineralization is concentrated in the thrust zone between the Ptnarbast Formation, which forms the hanging wall, and the Kalecik Limestone foot wall. Fluorite occurs as fracture fills in the thrust zone and as replacement of the foot wall. The wall rock alteration consists of calcite, barite, quartz and kaolinite. The total REE contents of the country rocks, especially the mica- and calc-schists of the Pinarbasi formation at 519 ppm, are higher than those of fluorites. The chondrite normalized REE patterns of country rock and fluorites display generally identical trends. However, fluorite patterns show positive Eu and negative Cc anomaly indicative of low temperature and high fo(2) conditions. Cross plots of the Tb/Ca - Tb/La, (La/Yb)(n) - (Tb/Yb)(n) and (La/Yb)(n) (Eu/Eu*)(n) ratios of the fluorites indicate deposition by low temperature hydrothermal waters. The REE and F were probably leached from the Pinarbasi Formation by the mineralizing solutions. The mineralizing fluids are probably meteoric and formation waters heated at depth along the thrust zone by the natural thermal gradient and/or formation waters heated and mobilized by thrusting.en_US
dc.identifier.doi10.2343/geochemj.39.131
dc.identifier.endpage139en_US
dc.identifier.issn0016-7002
dc.identifier.issn1880-5973
dc.identifier.issue2en_US
dc.identifier.scopus2-s2.0-20444395870en_US
dc.identifier.scopusqualityQ3en_US
dc.identifier.startpage131en_US
dc.identifier.urihttps://doi.org/10.2343/geochemj.39.131
dc.identifier.urihttps://hdl.handle.net/11616/93967
dc.identifier.volume39en_US
dc.identifier.wosWOS:000229682200003en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherGeochemical Soc Japanen_US
dc.relation.ispartofGeochemical Journalen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectfluoriteen_US
dc.subjectrare earth elementen_US
dc.subjectmineralizationsen_US
dc.subjectthrust zoneen_US
dc.subjectTurkeyen_US
dc.titleOrigin and nature of the mineralizing fluids of thrust zone fluorites in Celikhan (Adiyaman, Eastern Turkey)en_US
dc.typeArticleen_US

Dosyalar

Koleksiyon

WoS İndeksli Yayınlar Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu