We found a match
Your institution may have access to this item. Find your institution then sign in to continue.
- Title
Aluminum-fluorine sphene (Titanite) as an indicator of fluorine fluid.
- Authors
Sharova, O.; Chudnenko, K.; Avchenko, O.; Badredinov, Z.; Vakh, A.
- Abstract
The article focuses on the study regarding the structure of aluminum-fluorine (Al-F) sphene (titanite) mineral which observed in various geological environments in metamorphic, magmatic, and metasomatic rocks as an indicator of fluorine fluid in a wide range of geochemical and pressure temperature (PT)-conditions. It says that the structure of sphene allows different anion and cation isomorphism. It states that the sphenes with high concentrations of F and aluminum Al were originally established in high-pressure metamorphic rocks. It also examines the F content in fluid by the composition of Al-F sphene fluorimeter.
- Subjects
SPHENE; METAMORPHIC rocks; MAGMATISM; FLUIDS; FLUORINE; GEOCHEMISTRY; ISOMORPHISM (Crystallography); ALUMINUM; FLUORIMETER
- Publication
Doklady Earth Sciences, 2012, Vol 442, Issue 1, p126
- ISSN
1028-334X
- Publication type
Article
- DOI
10.1134/S1028334X12010217