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Stefano, Christopher J., Hackney, Stephen A., Kampf, Anthony R. (2020) The occurrence of iron silicides in a fulgurite: Implications for fulgurite genesis. The Canadian Mineralogist, 58 (1) 115-123 doi:10.3749/canmin.1900019

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Reference TypeJournal (article/letter/editorial)
TitleThe occurrence of iron silicides in a fulgurite: Implications for fulgurite genesis
JournalThe Canadian Mineralogist
AuthorsStefano, Christopher J.Author
Hackney, Stephen A.Author
Kampf, Anthony R.Author
Year2020 (January 16)Volume58
Issue1
PublisherMineralogical Association of Canada
DOIdoi:10.3749/canmin.1900019Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID65637Long-form Identifiermindat:1:5:65637:1
GUID0
Full ReferenceStefano, Christopher J., Hackney, Stephen A., Kampf, Anthony R. (2020) The occurrence of iron silicides in a fulgurite: Implications for fulgurite genesis. The Canadian Mineralogist, 58 (1) 115-123 doi:10.3749/canmin.1900019
Plain TextStefano, Christopher J., Hackney, Stephen A., Kampf, Anthony R. (2020) The occurrence of iron silicides in a fulgurite: Implications for fulgurite genesis. The Canadian Mineralogist, 58 (1) 115-123 doi:10.3749/canmin.1900019
In(2020, January) The Canadian Mineralogist Vol. 58 (1) Mineralogical Association of Canada
Abstract/NotesABSTRACT
Rapidly formed eutectic textures are observed in Fe silicides in a fulgurite from Michigan. The 14 cm-diameter fulgurite was formed in sandy glacial till in 2014 near Houghton Lake, Michigan. Spherical droplets of iron silicides up to ∼200 μm in diameter were found in the natural glass. Back-scattered electron images of some droplets show a eutectic intergrowth texture of two iron silicides with individual crystals up to ∼1 μm in maximum dimension. X-ray diffraction study showed the specimens to be an intergrowth of naquite (FeSi) and linzhiite (FeSi2) or naquite and xifengite (Fe5Si3). Droplets also contain minor native silicon, Fe-Ti silicides, and/or other Ti- rich phases which were discovered during TEM observations. It is important to note that the lower-temperature phase luobusaite (Fe3Si7) was not observed in any droplets, indicating rapid quenching of the fulgurite, consistent with a natural origin during a lightning strike as opposed to an artificial origin, e.g., resulting from a downed power line.

Locality Pages

LocalityCitation Details
Houghton Lake fulgurite, Roscommon County, Michigan, USA

Mineral Pages

MineralCitation Details
Fulgurite

Mineral Occurrences

LocalityMineral(s)
Houghton Lake fulgurite, Roscommon County, Michigan, USAⓘ Fulgurite, ⓘ Linzhiite, ⓘ Naquite, ⓘ Native Silicon, ⓘ Till, ⓘ Xifengite


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