volume 79, issue 15, P185-185 1998
DOI: 10.1029/98eo00135
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Abstract: A simple method may provide greater insights into the sort of pathways and time‐scales in which magmatic systems evolve. The method, employing isotopic fingerprinting of the mineral components that characterize most magmatic rocks, may lead to a more comprehensive understanding of these types of rocks. Such an understanding is critical to resolving fundamental problems in geoscience, ranging from the origin and differentiation of the crust and mantle to the prediction of volcanic hazards. Much progress has be…

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