DOUBTFUL FLUORESCENCE but sometimes cited in luminescence literature
Chemical formula: See BRANCHITE C20H34
Family: Organic
Status: IMA-GP
Crystal system : Triclinic
Display mineral: NON
Longwave UV (365nm) colors: |
Bluish White , | ||
Intensity LW:Very weak | |||
Shortwave UV (254nm) colors: |
Bluish White , | ||
Intensity SW:Extremely weak |
Daylight picture
Hartite, Bilin, Bohemia, Czech Republic;
Col. G. Barmarin; Spectre: G. Barmarin
Longwave (365nm) picture
Hartite UVLW, Bilin, Bohemia, Czech Republic;
Col. G. Barmarin; Spectre: G. Barmarin
Shortwave (254nm) picture
Hartite UVSW, Bilin, Bohemia, Czech Republic;
Col. G. Barmarin; Spectre: G. Barmarin
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No phosphorescence visible to the naked eye under any type of UV
Natural cyclic hydrocarbon to be checked for luminescence (equivalent to α-phyllocladane)
The terpenoid minerals fichtelite (norabietane) and hartite (α-phyllocladane) seems to have a luminescence under UV LW. Some of these hydrocarbons occur in soil and peat environments of Holocene age. However, hartite occurs in lignite, in fossilised Glyptostrobus (Taxodiaceae) trees and in pelosiderites of the Bílina Miocene series (about 20 Ma); it represents the accumulated and crystallised product of diagenetic transformation of precursor biogenic terpenoids. Raman spectra of earth waxes investigated confirm their dominantly aliphatic character and oxidative degradation (related to weathering and/or subaerial alteration in museum cabinets).
Activator(s): Matière organique intrinsèque,
No spectrum yet
(*)The data are not exhaustive and are limited to a few remarkable localities for fluorescence
http://www.mindat.org/show.php?name=Hartite
http://webmineral.com/data/Hartite.shtml
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