LIMICA: A program for estimating Li from electron-microprobemica analyses and classifying trioctahedral micas in terms of composition and octahedral site occupancy

Computers and Geosciences

Volumn 27, Issue 2, 2001, Pages 215-227

  Yavuz, F ^a  

^a ISTANBUL TECHNICAL UNIVERSITY   (Turkey)

Author keywords

[No Author keywords available]

Indexed keywords

CHEMICAL COMPOSITION; CRYSTAL STRUCTURE; LITHIUM; MICA; SOFTWARE;

EID: 0035115371     PISSN: 00983004     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0098-3004(00)00086-8     Document Type: Article

References (17)

1. Lithium zonation in white micas from the Argemela microgranite (central Portugal): An in situ ion-, electron-microprobe and spectroscopic investigation
2. Titanium, aluminum and interlayer cation substitutions in biotite from high-grade gneisses, west Greenland
3. Interpretation of the composition of lithium micas
4. Crystal-structure analysis as a chemical analytical method: Application to light elements
5. Compositional relations in Li-micas from S.W. England and France: An ion- and electron-microprobe study
6. Micas from the Pikes Peak batholith and its cogenetic granitic pegmatites, Colorado: Optical properties, composition and correlation with pegmatite evolution
7. 2O-
8. Nomenclature of the micas
9. Mineralogy and geochemical evolution of the little three pegmatite-aplite layered intrusion
10. Compositions of trioctahedral micas in the Cornubian batholith
11. Composition of trioctahedral micas in the Karlovy Vary pluton
12. Estimation of lithium contents in trioctahedral micas using microprobe data: Application to micas from granitic rocks
13. 2O estimation from MgO data
14. On Li-bearing micas: Estimating Li from electron microprobe analyses and improved diagram for graphical representation
15. A revised program for microprobe-derived amphibole analyses using the IMA rules
16. PYROX: A computer program for the IMA pyroxene classification scheme
17. BIOTERM - A program for evaluating and plotting microprobe analyses a biotite from barren and mineralized magmatic suites