2003
DOI: 10.1016/s0375-9474(03)00816-9
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On search and identification of short-lived super heavy cosmic-ray nuclei (Z ≥ 110) by fossil track study of the extraterrestrial crystals: Results and perspectives [I]

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Cited by 7 publications
(4 citation statements)
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“…The atomic number of the nucleus giving one of these tracks was estimated to be = -+ Z 119 6 10 with error bars assuming a 95% confidence degree. However, it seems that this information should be cross-checked thoroughly as the results reported by the other groups [47,51,52] did not show any hint for such a high flux of SHN in GCRs. The effect of the track fading during the 10 8 years space travel is not discussed in [54,55].…”
Section: Searches For Shn In Galactic Cosmic Rays (Gcrs)mentioning
confidence: 89%
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“…The atomic number of the nucleus giving one of these tracks was estimated to be = -+ Z 119 6 10 with error bars assuming a 95% confidence degree. However, it seems that this information should be cross-checked thoroughly as the results reported by the other groups [47,51,52] did not show any hint for such a high flux of SHN in GCRs. The effect of the track fading during the 10 8 years space travel is not discussed in [54,55].…”
Section: Searches For Shn In Galactic Cosmic Rays (Gcrs)mentioning
confidence: 89%
“…The controlled annealing method of olivine, originally developed by these authors, was of paramount importance for this study because the lengths of the annealed tracks of Z70 nuclei were reduced to fit the sub-millimeter dimensions of the olivine crystals extracted from the meteorite. The last papers published by this group [51,52] inform that about 1600 fossil tracks of the Th-U group nuclei were revealed in olivine taken from the Marjalahti and Eagle Station pallasite meteorites and estimate a limit of 3×10 −3 for a flux ratio of the SHE and Th-U nuclei in GCRs.…”
Section: Searches For Shn In Galactic Cosmic Rays (Gcrs)mentioning
confidence: 99%
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“…They show different responses to different particles, filtering out the background of particles that would blur the tracks of particles or energies of interest. They have been used, for example, to find the exotic spontaneous emission of 14 C clusters by 223 Rn [5] or to find the long tracks produced by the natural decay of superheavy elements ( > 110) already disappeared [6]. Natural minerals are also useful for the fission track dating, oil search, and many other applications.…”
Section: Introductionmentioning
confidence: 99%