Baker, J. H. (1985) Rare earth and other trace element mobility accompanying albitization in a Proterozoic granite, W. Bergslagen, Sweden. Mineralogical Magazine, 49 (350) 107-115 doi:10.1180/minmag.1985.049.350.17
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Rare earth and other trace element mobility accompanying albitization in a Proterozoic granite, W. Bergslagen, Sweden | ||
| Journal | Mineralogical Magazine | ISSN | 0026-461X |
| Authors | Baker, J. H. | Author | |
| Year | 1985 (March) | Volume | 49 |
| Issue | 350 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_49/49-350-107.pdf+ | ||
| DOI | doi:10.1180/minmag.1985.049.350.17Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 3706 | Long-form Identifier | mindat:1:5:3706:2 |
| GUID | 0 | ||
| Full Reference | Baker, J. H. (1985) Rare earth and other trace element mobility accompanying albitization in a Proterozoic granite, W. Bergslagen, Sweden. Mineralogical Magazine, 49 (350) 107-115 doi:10.1180/minmag.1985.049.350.17 | ||
| Plain Text | Baker, J. H. (1985) Rare earth and other trace element mobility accompanying albitization in a Proterozoic granite, W. Bergslagen, Sweden. Mineralogical Magazine, 49 (350) 107-115 doi:10.1180/minmag.1985.049.350.17 | ||
| In | (1985, March) Mineralogical Magazine Vol. 49 (350) Mineralogical Society | ||
| Abstract/Notes | AbstractZones of albitization 20 m wide are developed in the peraluminous, undeformed Proterozoic Bastfallshöjden granite, W. Bergslagen, central Sweden. During albitization Na, Si, Mg, Ni, Zn, and Ga are added, while Fe2+, Fe3+, Mn, K, Sc, Rb, Cs, Ba, Pb, U, and F are lost, together with the rare earth elements (REE) in decreasing amounts with increasing atomic number. Ti, Al, P, and Y were immobile. Trace element data for chlorites separated from hydrothermally altered country rocks and from a quartz-chlorite vein in the albitized granite show similar REE patterns indicating a common origin: the most altered granite has a similar REE pattern, probably resulting from interaction with the same hydrothermal fluid which produced the chlorites, in which seawater is thought to have been an important constituent. | ||
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