Abstract
Most igneous, metamorphic, and sedimentary rocks contain rubidium (Rb) and strontium (Sr) in detectable amounts. However, the concentrations of these elements are almost always less than 1 percent, and they are therefore rarely determined in routine chemical analyses. Neither rubidium nor 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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© 1972 Springer-Verlag Berlin, Heidelberg
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Faure, G., Powell, J.L. (1972). The Geochemistry of Rubidium and Strontium. In: Strontium Isotope Geology. Minerals, Rocks and Inorganic Materials, vol 5. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-65367-4_1
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DOI: https://doi.org/10.1007/978-3-642-65367-4_1
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-65369-8
Online ISBN: 978-3-642-65367-4
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