Are fission tracks in meteorites from super heavy elements?
Evidence of superheavy elements as source of fission tracks in meteorites
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Evidence of superheavy elements as source of fission tracks in meteorites
X ray diffraction patterns, like patterns from kamacite in iron meteorites, formed by static deformation at low stresses
Hypervelocity meteorite impacts by nuclear and chemical explosions
Radiation effects of accelerated heavy ions in minerals characteristic of meteorites
Carbon isotope fractionation in Fischer-Tropsch synthesis and in meteorites
Worldwide data inventory of rock features associated with meteorite impact structures, including photomicrographs of petrographic features
Naturally and artificially shocked iron meteorites, analyzing microstructure and alterations induced by pressure wave and high temperatures
Isotopic composition and contents of xenon and krypton in Pesyanoe meteorite suggesting presence of solar type gas component
Electron microprobe determinations of Si concentrations in metal of iron meteorites, showing weak evidence for Si presence in earth core
Cliftonite occurrence, internal structure, orientation within kamacite and implications on origin of diamonds in meteorites
Lunar surface samples characteristics correlation with terrestrial igneous rocks /basalts/ and eucrite meteorites based on alpha scattering analysis
Pueblo de Allemande chondrite unexctractable carbon content using meteorite pyrolysis, obtaining aromatic hydrocarbons
Iron troilite meteorites lead isotopic, Pb and U concentrations, considering fractionation and terrestrial contamination effects
Allende meteorite showing presence of Ca-Al-rich glasses associated with other crystalline phases
Microscopic meteoritic spherules in soil surrounding terrestrial impact craters
Carbonaceous meteorites analyzed for soluble organic compounds, carbonate and residual carbon, showing endogenous nature
Olivine and metal compositions of pallasitic meteorites by electron microprobe measurements, obtaining cooling rates
Iron-nickel alloy phase and diffusion relationships, composition gradients and hardness variations involving long time metallic meteorite anneals