Terrestrial, lunar and interplanetary rock fragmentation /synopsis/
Terrestrial, lunar, and interplanetary rock fragmentation
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Terrestrial, lunar, and interplanetary rock fragmentation
Neurons reaction in reticular formation of cats during rocking
Meteorite impact recognition from microscopic structure of rocks
X Ray fluorescence of rock samples as applied to geological problems, noting standard deviations for element distribution
Lead isotope composition and concentrations of U, Th, Ra, total Pb and Pb 210 in recent volcanic rocks, noting disequilibrium due to chemical fractionations
Indium abundances in chondritic and achondritic meteorites and terrestrial rocks determined by radiochemical neutron activation analysis
NASA lunar receiving laboratory for lunar rock samples examination by gamma ray spectrometry for induced radioactive nuclides and naturally occurring isotopes
Lunar surface, asteroids and meteorites properties by mass distributions of fragmented rocks
Amino acid components in paleozoic plant fossils and rock samples noting glycine, serine and glutamic acid
Thermal conductivities /K/ of rock forming minerals reveals K as linear function of density for constant mean atomic weight
Spectroradiometer is used for either close or remote identification of rocks not heated to high temperatures. Instrument yields reproducible data spectra with excellent signal-to-noise ratios and readily identifiable spectral details, including differences in subclasses.
Relict diagenetic textures and structures in regional metamorphic rocks, northern Michigan
Preliminary petrologic inferences from crystalline rocks collected at Mare Tranquillitatis by Apollo 11 crew
Reflectance of rocks and minerals to visible and ultraviolet radiation
Hydrothermally altered rocks as water source on Moon and Mars
Ultraviolet reflectance measurements of rocks and minerals from 2000 A to 3000 A
Worldwide data inventory of rock features associated with meteorite impact structures, including photomicrographs of petrographic features
Polycrystalline rocks elastic constant and nonelastic behavior, discussing Voigt, Reuss and Hill averaging methods