Combined Lithophile‐Siderophile Isotopic Constraints on Hadean Processes Preserved in Ocean Island Basalt Sources
نویسندگان
چکیده
Detection of Hadean isotopic signatures within modern ocean island basalts (OIB) has greatly influenced understanding Earth's earliest history and long-term dynamics. However, a relationship between two tools for studying early Earth processes, the short-lived 146Sm-142Nd 182Hf-182W systems, not been established in this context. The differing chemical behavior these systems means that they are complementary tracers range proposed events, including core formation, magma late accretion. There is negative trend 142Nd/144Nd 182W/184W ratios among Réunion OIB extended by Deccan continental flood basalts. This finding contrary to expectations if both were affected silicate differentiation during lifetime 182Hf. observed compositions attributed interaction remnants core, coupled with later assimilation recycled mafic crust. effects scenario on long-lived 143Nd-176Hf systematics mirror classical models invoking mixing trace-element enriched (sedimentary) depleted (igneous) domains mantle sources. If provides detectible contribution tungsten element budget Earth, represents critical component planetary-scale mass balance. A basic model explored reconciles W abundance composition bulk resulting from accretion core-mantle interaction. veracity as here would have many implications thermochemical cycling.
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ژورنال
عنوان ژورنال: Geochemistry Geophysics Geosystems
سال: 2021
ISSN: ['1525-2027']
DOI: https://doi.org/10.1029/2020gc009479