dc.contributor.author |
Augustithis, SS |
en |
dc.contributor.author |
Mposkos, E |
en |
dc.contributor.author |
Vgenopoulos, A |
en |
dc.date.accessioned |
2014-03-01T01:05:49Z |
|
dc.date.available |
2014-03-01T01:05:49Z |
|
dc.date.issued |
1980 |
en |
dc.identifier.issn |
0009-2541 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/9009 |
|
dc.subject.classification |
Geochemistry & Geophysics |
en |
dc.title |
Diffusion rings (sphaeroids) in bauxite |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1016/0009-2541(80)90101-1 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1016/0009-2541(80)90101-1 |
en |
heal.language |
English |
en |
heal.publicationDate |
1980 |
en |
heal.abstract |
Diffusion rings (sphaeroids) in bauxites from Klisoura (Dunionia), Helicon, Greece, are described and are studied mineralogically by X-ray diffraction and ore-microscopically. These diffusion rings are also analysed by X-ray fluorescence spectroscopy. The diffusion rings have Fe-rich and relatively Fe-depleted zones. Element leaching and mobilization under weathering is proposed to be the mechanism responsible for the formation of these diffusion rings. A comparison with similar diffusion rings in granite also suggests element leaching as the process responsible for their formation. © 1980. |
en |
heal.publisher |
ELSEVIER SCIENCE BV |
en |
heal.journalName |
Chemical Geology |
en |
dc.identifier.doi |
10.1016/0009-2541(80)90101-1 |
en |
dc.identifier.isi |
ISI:A1980KP19800004 |
en |
dc.identifier.volume |
30 |
en |
dc.identifier.issue |
4 |
en |
dc.identifier.spage |
351 |
en |
dc.identifier.epage |
362 |
en |