Primary versus secondary high-Cr signatures in ophiolitic chromitite: grain-scale evidence from the Kop ophiolite, NE Türkiye
INTERNATIONAL GEOLOGY REVIEW, 2026 (SCI-Expanded, Scopus)
- Yayın Türü: Makale / Tam Makale
- Basım Tarihi: 2026
- Doi Numarası: 10.1080/00206814.2026.2749582
- Dergi Adı: INTERNATIONAL GEOLOGY REVIEW
- Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Geobase, Academic Search Ultimate (EBSCO), Natural Science Collection (ProQuest), Earth, Atmospheric, & Aquatic Science Collection (ProQuest)
- Recep Tayyip Erdoğan Üniversitesi Adresli: Evet
Özet
Fresh chromite from the Kop chromitites in northeastern T & uuml;rkiye exhibits Cr# values of 0.73-0.84 and TiO2 content of 0.03-0.26 wt%. BSE imaging, electron-probe analyses, and WDS element maps distinguish relatively preserved interiors from fracture-related replacement domains and secondary vein assemblages. Parental melts calculated from the fresh analyses contain 9.6-12.6 wt% Al2O3 and 0.07-0.39 wt% TiO2. The estimates are compatible with a supra-subduction-zone setting involving boninite-like melts. Altered chromite is characterized by lower Al2O3 and MgO, higher total Fe, and lower Mg#, with Cr# values reaching 0.99. Its high Cr# is therefore principally consistent with preferential Al depletion during replacement and does not require a more depleted parental melt. Mn and Zn are generally more variable or enriched in altered domains, whereas TiO2 overlaps between fresh and altered chromite. Calculated ferric ratios are non-monotonic. In one sample, highly altered analyses have lower Ni and higher V than fresh analyses, although low analytical totals limit quantitative interpretation. In another sample, Cr-bearing Mg-chlorite and Ca-Cr-Fe garnet of andradite-uvarovite affinity record local element redistribution without establishing net fluxes or a unique fluid source. The proposed screening workflow separates preserved, replaced, and indeterminate domains before parental-melt reconstruction.