High sensitivity isotope geochemistry
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Chemical analysis of sediment and oil hydrocarbon content by gas chromatography and mass spectrometry to establish inception period of bio-organic evolution
Chemical analysis of quartz monzonites and associated gruss from Fremont Lake area, California
Stable isotope dilution method used to determine lanthanides in six basalts of central Japan
Stable isotope dilution method to determine lanthanides in basalts from central Japan
Organic geochemical laboratories solvent purification procedures
Hydrocarbon contents of two sediments from Scottish Carboniferous Formation, examining isoprenoid alkanes abiogenesis
Major and trace element concentration in contact zones of Precambrian diabase dikes from Wyoming ranges, showing dikes as continental tholeiites
Radioactive age determination and isotopic composition analyses on rocks, meteorites, and lunar samples
Analyzing glaciers, hot springs, and volcanic ash from erupting volcanoes in Iceland for hydrocarbon content as test for life detection techniques
Soil and ground rock amino acids preparation and analysis by desalting method
Spectral reflectance curves for red spruce and balsam fir in the 350- to 1100-nanometer region showed differences between specimens growing over and away from a concealed copper deposit at Catheart Mountain, Maine. A sample group of 15 anomalous spruce, 9 background spruce, 10 anomalous fir, and 10 background fir was studied. Measurements of copper and molybdenum contents in the supporting soil were used to categorize the trees as anomalous or background. Analyses using parametric and nonparametric statistical tests were performed to establish whether significant differences existed between the anomalous and background groups. At the 95% confidence level, significant differences were found to exist for both species, generally in the chlorophyll band centered at about 550 nanometers and in the region from 700 to 900 nanometers.
A new indirect approach to crustal analysis of a specific sector of the Ethiopian plateaus and rift is discussed. It is suggested that progressive changes in basalt chemistry across this area are related to crustal thinning and shallowing of the zone of melting under the Afar rift.
Data are presented on major and trace element concentrations determined by atomic absorption spectrophotometry, colorimetry, and isotope dilution in Apollo 15 mare basalt 15555 from the Hadley Rille area, as well as on trace element concentrations determined in plagioclase and pyroxene separates from basalt 15555 and in soil 15531 from the same area. Most of the chemical differences between basalt 15555 and soil 15531 could be accounted for if the soil were a mixture of 88% basalt, 6% KREEP (a component, identified in other Apollo soils, rich in potassium, rare-earth elements, and phosphorus), and 6% plagioclase.
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Aluminum/silicon and magnesium/silicon concentration measurements along Apollo-15 and -16 lunar groundtracks by X-rays show that the highlands are very rich in aluminum, and that mare basalts cover large areas.