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Titlebook: Strontium Isotope Geology; Gunter Faure,James L. Powell Book 1972 Springer-Verlag Berlin, Heidelberg 1972 Isotope.Rubidium-Strontium-Alter

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楼主: Hypothesis
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The Moon,xploring the lunar surface in the vicinity of their spacecraft they returned safely to Earth with 22 kilograms of rocks and dust they had collected. The exploration of the Moon and the collection of rock samples for analysis has been continued by subsequent American flights of the Apollo program and
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The Geochemistry of Rubidium and Strontium,is a major constituent in the common rock-forming silicate minerals, although strontium does form a carbonate (strontianite) and a sulfate (celestite) which are found in some hydrothermal deposits and certain sedimentary rocks, particularly carbonates.
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Meteorites,ther silicate minerals such as feldspar and diopside. The irons are composed mainly of the iron-nickel alloys taenite and kamacite, but they also contain troilite (FeS) and inclusions of silicate minerals. The stony-irons consist of roughly equal proportions of metallic and silicate phases.
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Volcanic Rocks,nly about the isotopic composition of strontium in the upper mantle, but also about its possible Rb/Sr ratio. G. (1960) and H. (1968 a, b), among others, have shown how Rb/Sr ratios can be used as a clue to the chemical composition and evolution of the mantle.
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Ultramafic and Related Rocks,s in differentiated basic sills and in minor intrusions,(4) kimberlites, (5) ultrmafic nodules, (6) alkali ultrabasic rocks in ring complexes, and (7) ultrabasic lavas. In the following sections of this chapter we shall review the strontium isotopic data for the first five of these associations; the last two have been covered in Chapter VI.
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