Europium isotope fractionation in highly fractionated igneous rocks with large Eu negative anomaly

نویسندگان

چکیده

One of peculiar geochemical characteristics in the chondrite-normalized REE patterns from highly fractionated granites and high silica rhyolite is extremely large negative Eu anomaly (Eu/Eu* < 0.10) due to very low concentration Eu. Particularly, provides a valuable information for evolution processes earth planetary materials. has only two isotopes, 151Eu 153Eu. In this study, isotope ratios igneous rocks curated GSJ USGS some with were determined by MC-ICP-MS using Sm internal standardization methods. The degree fractionation (δ153/151Eu) was calculated on basis NIST3117a standard. All study showed that their 153Eu/151Eu values are higher than standard, indicating enriched felsic magma. Our results suggest will provide key understanding related magmatic differentiation processes.

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ژورنال

عنوان ژورنال: Geochemical Journal

سال: 2021

ISSN: ['0016-7002', '1880-5973']

DOI: https://doi.org/10.2343/geochemj.2.0631