Minor and trace elements in meteoritic minerals:

"Nickel-iron, troilite, olivine, pyroxenes, plagioclase, chromite, and phosphate minerals (chlorapatite and/or merrillite) have been separated from a number of meteorites (Modoc, St. Severin, Winona, Haraiya, Marjalahti, Springwater, Johnstown, Mt. Egerton, Soroti) and analyzed for minor and tr...

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Bibliographische Detailangaben
Hauptverfasser: Mason, Brian 1917-2009 (VerfasserIn), Graham, A. L. (VerfasserIn)
Format: Buch
Sprache:English
Veröffentlicht: Washington, D.C. Smithsonian Institution Press 1970
Schriftenreihe:Smithsonian contributions to the earth sciences 3
Schlagworte:
Zusammenfassung:"Nickel-iron, troilite, olivine, pyroxenes, plagioclase, chromite, and phosphate minerals (chlorapatite and/or merrillite) have been separated from a number of meteorites (Modoc, St. Severin, Winona, Haraiya, Marjalahti, Springwater, Johnstown, Mt. Egerton, Soroti) and analyzed for minor and trace elements with the spark-source mass spectrometer. The elements Ni, Co, Ge, As, Ru, Rh, Pd, Sn, Sb, W, Re, Os, Ir, Pt, and Au are concentrated in nickel-iron; Se and Ag in troilite; Th, U, and the lanthanides in the phosphate minerals and in diopside; Eu, Sr, Ba, Rb, and Cs in plagioclase. Molybdenum and tellurium are concentrated in nickel-iron and troilite. The elements Ti, Sc, V, Cu, Zn, Mn, and Ga are distributed over several coexisting minerals."--verso.
Beschreibung:Literaturverz. S. 16 - 17
Beschreibung:17 S. graph. Darst.

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