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Dear Eliza, Sorry to say, but there’s not really a one-size-fits-all answer to this question.Consider the number of variables involved in answering: Are there children involved?Of the young tourmalines, three of them give ages of 80–85 Ma, indicating possible examples of incomplete degassing and/or possible incorporation of excess radiogenic Ar in the mineral during the Alpine metamorphism.The tourmaline ages are compared with the ages of the coexisting micas.
Distinct convex-upward rare earth element (REE) patterns of the leachates suggest that the precipitation of early diagenetic apatite controls the trace element budget of the rock, forcing a depletion of middle REEs on the subsequently formed diagenetic phyllosilicates.
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In all cases, leaching of the fine fractions results in a high (0.05–0.14) residual component.
The observed fractionation is an ancient feature related to diagenesis, burial and metamorphism.