Shock-induced preferred disorder in solids.
X ray detectable preferred disorder in solids by shock loading studied in Ainsworth meteorite and in hexagonal alpha silicon dioxide
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Publications and source records attributed to Lipschutz, M. E..
X ray detectable preferred disorder in solids by shock loading studied in Ainsworth meteorite and in hexagonal alpha silicon dioxide
V 50/V 51 abundance ratios in chondrite, terrestrial diabase standard W-1 and reagent V
Shock histories of hexahedrites and Ga-Ge group III octahedrites based on metallographic and X ray diffraction analysis, noting meteorites shocked preterrestrially
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Stony meteorite trace elements groups neutron activation analysis with computer reduction of Ge/Li spectra
Shock loading history effect on solid state response of iron meteorites to annealing at moderate temperatures permits deductions about thermal history
X ray diffraction studies of kamacite /alpha-iron/ from iron meteorites indicating shock induced alteration and unstable polymorph influence
Naturally and artificially shocked iron meteorites, analyzing microstructure and alterations induced by pressure wave and high temperatures
Microscopic and X-ray diffraction study of octahedrite shock history
Cohenite grains from iron meteorites studied by X-ray diffraction for establishing pressure scale, using solid state recrystallization
X-ray diffraction and metallographic investigation show iron meteorites shock at pressures of at least 130 kbar
X-ray diffraction study of minerals from shocked iron meteorites
Canyon Diablo meteorite examined, using mass spectrometry and metallography, noting shock effects
Critique of paper by Carter and Kennedy regarding origin of diamonds in Canyon Diablo and Novo Urei meteorite
X-ray diffraction investigation of cohenite from Canyon Diablo meteorites and Odessa shock standards to determine shock-induced alterations in crystal character
Origin of atypical meteorites from Arizona meteorite crater
Chemical composition of major and minor phases in two specimens of Odessa iron meteorite analyzed by electron probe