Abstract
Several recent studies have shown notable regularities in the behavior of incompatible trace elements in alkaline volcanic suites [1–5], and there has been some discussion of the significance of these features, especially of linear correlation (or lack of it) between such trace elements [5]. This contribution is not an exhaustive treatment of trace element behavior, the principles of which have been applied to alkaline rocks by others [4,6,7]. Rather it is proposed to discuss some petrogenetic uses to which such data may be put.
This work has been supported in part by National Science Foundation Grants GA 32333 and EAR75-20664, and by NERC.
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References
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© 1978 D. Reidel Publishing Company, Dordrecht, Holland
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Baker, B.H. (1978). A Note on the Behavior of Incompatible Trace Elements in Alkaline Magmas. In: Neumann, ER., Ramberg, I.B. (eds) Petrology and Geochemistry of Continental Rifts. NATO Advanced Study Institutes Series, vol 36. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-9803-2_2
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DOI: https://doi.org/10.1007/978-94-009-9803-2_2
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