Wall rock assimilation by magnetite-series granitoid at the Miyako pluton, Kitakami, northeastern Japan.
نویسندگان
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: The Journal of the Geological Society of Japan
سال: 1985
ISSN: 0016-7630,1349-9963
DOI: 10.5575/geosoc.91.679