Fluid evolution in the Strange Lake granitic pluton, Canada: Implications for HFSE mobilisation
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چکیده
منابع مشابه
U-series isotopic disequilibrium produced during experimental melting of granitic crust: Implications for shallow-level assimilation and pluton remobilisation
Although the production of U-series disequilibria during metasomatic and partial-melting processes in Earth’s mantle is well studied, the effects of melting and assimilation processes during ascent and storage of magma in the crust are less well understood. To investigate disequilibria arising via this mechanism, we have conducted U-series measurements on the products of laboratory experiments ...
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ژورنال
عنوان ژورنال: Chemical Geology
سال: 2016
ISSN: 0009-2541
DOI: 10.1016/j.chemgeo.2016.10.009