A NEW GRAPHICAL PRESENTATION AND SUBDIVISION OF POTASSIUM MICAS
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Tischendorf G. | |
dc.contributor.author | Rieder M. | |
dc.contributor.author | Förster H.J. | |
dc.contributor.author | Gottesmann B. | |
dc.contributor.author | Guidotti Ch.V. | |
dc.date.accessioned | 2022-04-08T06:42:00Z | |
dc.date.available | 2022-04-08T06:42:00Z | |
dc.date.issued | 2004 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13924507 | |
dc.identifier.citation | Mineralogical Magazine, 2004, 68, 4, 649-667 | |
dc.identifier.issn | 0026-461X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/36916 | |
dc.description.abstract | A system based on variation of the octahedrally coordinated cations is proposed for graphical presentation and subdivision of tri- and dioctahedral K micas, which makes use of elemental differences (in a.p.f.u.): (Mg - Li) [= mgli] and (Fetot + Mn + Ti - VIAl) [= feal]. All common true tri- and dioctahedral K micas are shown in a single polygon outlined by seven main compositional points forming its vertices. Sequentially clockwise, starting from Mg3 (phlogopite), these points are: Mg2.5Al0.5, Al2.167⃞0.833, Al1.75Li1,25, Li2Al (polylithionite), Fe2+2Li, and Fe2+3 (annite). Trilithionite (Li1.5Al1.5), Li1.5Fe2+Al0.5, Fe2+2Mg, and Mg2Fe2+ are also located on the perimeter of the polygon. IMA-siderophyllite (Fe2+2Al) and muscovite (Al2⃞) plot inside. The classification conforms with the IMA-approved mica nomenclature and differentiates among the following mica species according to their position in a diagram consisting of mgli and feal axes plotted orthogonally; trioctahedral: phlogopite, biotite, siderophyllite, annite, zinnwaldite, lepidolite and tainiolite; dioctahedral: muscovite, phengite and celadonite. Potassium micas with [Si] <2.5 a.p.f.u. including IMA-siderophyllite, KFe2+2AlAl2Si2O10O(OH)2, and IMA-eastonite, KMg2AlAl2Si2O10O(OH)2 seem not to form in nature. The proposed subdivision has several advantages. All common true, trioctahedral and dioctahedral K micas, whether Li-bearing or Li-free, are shown within one diagram, which is easy to use and gives every mica composition an unambiguously defined name. Mica analyses with Fe2+, Fe3+, Fe2+ + Fe3+, or Fetot can be considered, which is particularly valuable for microprobe analyses. It facilitates easy reconstruction of evolutionary pathways of mica compositions during crystallization, a feature having key importance in petrologically oriented research. Equally important, the subdivision has great potential for understanding many of the crystal-chemistry features of the K micas. In turn this may allow one to recognize and discriminate the extent to which crystal chemistry or bulk composition controls the occurrence of some seemingly possible or hypothetical K mica. | |
dc.subject | micas | |
dc.title | A NEW GRAPHICAL PRESENTATION AND SUBDIVISION OF POTASSIUM MICAS | |
dc.type | Статья |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru