The possible existence of Hs in nature from a geochemical point of view

dc.creatorIvanov, A. V.
dc.date2006-04-21
dc.date2006-04-23
dc.date.accessioned2026-07-07T07:36:05Z
dc.date.available2026-07-07T07:36:05Z
dc.descriptionA hypothesis of the existence of a long-lived isotope 271Hs in natural molybdenites and osmirides is considered from a geochemical point of view. It is shown that the presence of Hs in these minerals can be explained only by making an additional ad hoc assumption on the existence of an isobaric pair of 271Bh-271Hs. This assumption could be tested by mass-spectrometric measurements of U, Pb, Kr, Xe, and Zr isotopic shifts.
dc.description5 pages, no figures. Physics of Particles and Nuclei Letters, 2006, Vol. 3, No. 3, pp. 165-168 in press
dc.identifierhttps://arxiv.org/abs/nucl-th/0604052
dc.identifierhttp://arxiv.org/abs/nucl-th/0604052
dc.identifierProg.Part.Nucl.Phys. 3 (2006) 165-168; Pisma Fiz.Elem.Chast.Atom.Yadra 3 (2006) 42-48
dc.identifierdoi:10.1134/S1547477106030046
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/120307
dc.subjectNuclear Theory
dc.titleThe possible existence of Hs in nature from a geochemical point of view
dc.typetext

Files

Collections