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Fodor, R. V., Jacobs, R. S., Bauer, G. R. (1994) Hollandite in Hawaiian basalt: a relocation site for weathering-mobilized elements. Mineralogical Magazine, 58 (393) 589-596 doi:10.1180/minmag.1994.058.393.06

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Reference TypeJournal (article/letter/editorial)
TitleHollandite in Hawaiian basalt: a relocation site for weathering-mobilized elements
JournalMineralogical MagazineISSN0026-461X
AuthorsFodor, R. V.Author
Jacobs, R. S.Author
Bauer, G. R.Author
Year1994 (December)Volume58
Page(s)589-596Issue393
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_58/58-393-589.pdf+
DOIdoi:10.1180/minmag.1994.058.393.06Search in ResearchGate
Mindat Ref. ID2082Long-form Identifiermindat:1:5:2082:8
GUID364bfa37-3445-4bcd-90fe-f1359520cd24
Full ReferenceFodor, R. V., Jacobs, R. S., Bauer, G. R. (1994) Hollandite in Hawaiian basalt: a relocation site for weathering-mobilized elements. Mineralogical Magazine, 58 (393) 589-596 doi:10.1180/minmag.1994.058.393.06
Plain TextFodor, R. V., Jacobs, R. S., Bauer, G. R. (1994) Hollandite in Hawaiian basalt: a relocation site for weathering-mobilized elements. Mineralogical Magazine, 58 (393) 589-596 doi:10.1180/minmag.1994.058.393.06
In(1994, December) Mineralogical Magazine Vol. 58 (393) Mineralogical Society
Abstract/NotesAbstractEnrichments in Ba, REE and Y abundances, occurrences of REE, Y-bearing phosphate, depletions in K and Rb, and negative Ce anomalies in some lavas on Kahoolawe (Hawaii) reflect secondary mobilization of Ba, REE, Y, K and Rb. Hollandite (Ba-Mn-oxide) in the groundmass of a Kahoolawe lava contains nearly 10 wt.% BaO, ∼ 1.1 wt.% CeO2, and small amounts of La, Nd, Y, K, Na, P, Cl and Cu to provide an example of where elements mobilized during weathering processes on the Hawaiian Islands find residence. Fe-vernadite, a second Mn-oxide, also hosts mobilized REE and Ba. A positive Ce anomaly in the hollandite complements the negative Ce anomaly in some Kahoolawe lavas, this is analogous to Ce accumulation in todorokite of manganese nodules complementing Ce-depleted seawater. Mn-oxides, then, can serve as links between lavas depleted and enriched in certain elements.


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