Ilvaite trace mineral chemistry as a thermodynamic recorder of retrograde alteration and metallogenic indicator for discrimination of skarn deposits: an example from the iron deposit in North Sanandaj-Sirjan Zone
Ilvaite, CaFe22+Fe3+(Si2O7)O(OH), is one of the important trace minerals in the retrograde alteration stage of skarn deposits. In this contribution, by using microscopic evidence, X-ray diffraction (XRD) and electron microprobe analysis (EPMA), the crystallographic characteristics, crystal chemistry...
Guardat en:
| Autor principal: | |
|---|---|
| Format: | Artigo |
| Idioma: | Persa |
| Publicat: |
Kharazmi University
2023-09-01
|
| Col·lecció: | علوم زمین خوارزمی |
| Matèries: | |
| Accés en línia: | http://gnf.khu.ac.ir/article-1-2885-en.pdf |
| Etiquetes: |
Sense etiquetes, Sigues el primer a etiquetar aquest registre!
|