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Combined chemical and high-precision isotope analysis of silicate melt inclusions – Advancing the understanding of Earth’s heterogeneous mantle

Applicant Dr. Felix Genske
Subject Area Mineralogy, Petrology and Geochemistry
Term from 2018 to 2024
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 398351295
 
Final Report Year 2024

Final Report Abstract

The most important scientific advances that emerged from the project was the discovery and establishment of the much greater isotopic variability of mantle derived melts as manifested by olivine hosted melt inclusions from the Azores, Tristan da Cunha and Gough Island and Hawai’i. All studied locations reveal that large heterogeneity is captured within single eruptions (lava flows) and that the mantle sources of OIB are indeed more heterogeneous than displayed by the compositions of bulk rocks. Further studies from many different OIB and MORB settings are strongly requested as these will improve our current understanding not only on magma genesis, but on the geodynamic cycles that form the surface of Earth and other rocky planets. Due to their small size – most inclusions were 50 micrometres or smaller – the amount of the analyte extractable was often too small (<<30 pg of Nd, <500 of Sr) to be measured for isotope ratios. Instead, several inclusions as captured in single olivine crystals were analysed. Nevertheless, by comparison to the host lavas, the new isotope data from melt inclusions obtained during this study reveal isotopic variability extending that of the erupted lavas. Severe restrictions led to some interruptions during the analytical work of the project.

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