The Na/K ratio of fluid inclusions in pegmatitic quartz and its genetic implications. A study by neutron activation analysis |
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Authors: | RA Horn FE Wickman |
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Institution: | Department of Geosciences, Pennsylvania State University, University Park, Pa 16802, U.S.A. |
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Abstract: | Samples of quartz and its fluid inclusions (f.i.) from Black Hills pegmatites and from graphic granites were analyzed for Na, K, Rb and Cs by neutron activation analysis. The Na/K ratios of the whole quartz and its f.i. seem unrelated. The spatial locations for six samples from the Helen Beryl pegmatite were known. The Na/K ratios of their f.i. are mainly a function of their vertical positions in the pegmatite. The ratios of the central-core quartz f.i. seemingly indicate a much higher temperature than those closer to the upper wall. This is consistent with the theory of pegmatite genesis by Jahns & Burnham. The f.i. of quartz from two graphic granites give very different Na/K ratios, seemingly related to differences in their formation history. |
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