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Showing 1 to 10 of 10 for “"mantle geochemistry"”.

  1. Mantle Heterogeneity Through Mid-Ocean Ridge Basalts

    The chemical heterogeneity of Earth's upper mantle is often examined through mid-ocean ridge basalts (MORB), which contest the prevalent assumption of a well-mixed convecting mantle. This dissertation delves into studying mantle heterogeneity from a local to regional scale. Initially, petrological …

    houston Repository record for Mantle Heterogeneity Through Mid-Ocean Ridge Basalts (opens in a new tab)

  2. A heavy stable isotope approach to tracing mantle source and process

    The geochemistry of global mantle melts suggests that both mid-ocean ridge basalts (MORB) and ocean island basalts (OIB) sample lithological heterogeneities originating in both the upper and lower mantle, with recycled crustal material accounting for a significant part of this variability. …

    cambridge Repository record for A heavy stable isotope approach to tracing mantle source and process (opens in a new tab)

  3. Inside-out diversity of rocky planets

    … bare-minimum, dynamic topography due directly to mantle convection, by finding scaling laws of dynamic topography with convective parameters. For increasingly massive planets, topography almost disappears. Smaller ocean basins might suggest flooded worlds, all else equal. Yet large portions of a …

    cambridge Repository record for Inside-out diversity of rocky planets (opens in a new tab)

  4. Insights into the location, nature and influence of mantle heterogeneity in the Galápagos mantle plume

    … of the Earth's, highly heterogeneous, convecting mantle. Our view of the Earth's mantle is, however, partially obscured by processes that influence mantle-derived melts as they transition through the lithosphere (e.g. mixing, assimilation). Nevertheless, via careful consideration of the magmatic …

    cambridge Repository record for Insights into the location, nature and influence of mantle heterogeneity in the Galápagos mantle plume (opens in a new tab)

  5. Mantle-Melting at High Pressure: Experimental Constraints on Magma Ocean Differentiation

    … melt ratios. This shows that the Earth’s upper mantle Mg/Si ratio is unlikely to be derived from chondrites by MgPv fractionation. Partition coefficients of tri- and tetravalent elements increase with increasing Al concentration of MgPv. A crystal chemical model indicates that Al3+ substitutes …

    bayreuth Repository record for Mantle-Melting at High Pressure: Experimental Constraints on Magma Ocean Differentiation (opens in a new tab)

  6. Magma genesis beneath active continental rifts

    … with geophysical evidence for low-density mantle underlying both rifts, have traditionally been interpreted as evidence for anomalously hot mantle plumes actively rising from the deep mantle beneath both regions. However, in light of increasing evidence that these mantle structures may also …

    unh-thes Repository record for Magma genesis beneath active continental rifts (opens in a new tab)

  7. Understanding Non-Plume Related Intraplate Volcanism

    … of intraplate volcanism are dominated by mantle plumes, but alternative explanations, such as adiabatic decompression triggered by lithospheric delamination, and edge driven convection (EDC), could be responsible for magmatism. This dissertation explores intraplate volcanic locations that …

    vt Repository record for Understanding Non-Plume Related Intraplate Volcanism (opens in a new tab)

  8. Mantle melting processes: evidences from ophiolites, large igneous provinces, and intraplate seamounts

    Melting processes in the mantle have a key role in plate tectonics and in the most colossal phenomena in the Earth, like large igneous provinces, mantle plume upwellings, and the constant growth of the planet's tectonic plates. In this study we use the geochemical and petrological evidence …

    vt Repository record for Mantle melting processes: evidences from ophiolites, large igneous provinces, and intraplate seamounts (opens in a new tab)

  9. Geochemical Implications of Stirring and Mixing in the Earth's Mantle

    … state convection that occurs in the Earth's mantle, but to do so requires suitable quantitative models. A new statistical model is introduced to better understand the observed heterogeneity in isotopic ratios 143Nd/144Nd, 87Sr/86Sr, 176Hf/177Hf,208Pb/204Pb, 206Pb/204Pb and 207Pb/204Pb …

    cambridge Repository record for Geochemical Implications of Stirring and Mixing in the Earth's Mantle (opens in a new tab)

  10. Edelgase als Tracer für Wechselwirkungen von Krusten- und Mantelfluiden mit diamantführenden Gesteinen des östlichen Baltischen Schildes

    In der vorliegenden Arbeit werden anhand der Edelgaszusammensetzung von Kimberliten und Lamproiten sowie ihrer gesteinsbildenden Minerale die Wechselwirkungen dieser Gesteine mit Fluiden diskutiert. Die untersuchten Proben stammen vom östlichen Baltischen Schild, vom Kola-Kraton (Poria Guba und …

    potsdam-diss Repository record for Edelgase als Tracer für Wechselwirkungen von Krusten- und Mantelfluiden mit diamantführenden Gesteinen des östlichen Baltischen Schildes (opens in a new tab)