Terrestrial, lunar and interplanetary rock fragmentation /synopsis/.
Lunar surface, asteroids and meteorites properties by mass distributions of fragmented rocks
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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
Terrestrial solid powdered rocks HF electrical properties measurements at 450 MHz and 35 GHz for lunar radar observation
Lunar surface samples characteristics correlation with terrestrial igneous rocks /basalts/ and eucrite meteorites based on alpha scattering analysis
Gaseous species in equilibrium with Apollo 11 holocrystalline rocks during crystallization
Oceanic ridge volcanic rocks alkali metal, alkaline earth, rare earth, nickel and major element content, observing partial melting
Rb-Sr internal isochrons of crystalline lunar rocks from Tranquility Sea for moon age estimation
Oceanic volcanic rocks, discussing dispersed element characteristics to describe origin of magma types
Cretaceous rock paleomagnetism from Israel lava fields, determining original magnetization directions