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Showing 1 to 20 of 29 for “"silicate melt"”.

  1. Silicate Melt Inclusions in Igneous Petrogenesis

    Silicate melt inclusions are ubiquitous in quartz phenocrysts, yet there are few studies of such inclusions from porphyry copper systems. A melt inclusion forms when magma is trapped in a growing phenocryst. If a phenocryst is able to preserve the original parent magma, then accurate information …

    vt Repository record for Silicate Melt Inclusions in Igneous Petrogenesis (opens in a new tab)

  2. The dependence on oxygen fugacity of nickel and cobalt partitioning between olivine and silicate melt

    Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1991.

    mit Repository record for The dependence on oxygen fugacity of nickel and cobalt partitioning between olivine and silicate melt (opens in a new tab)

  3. Carbon in Silicate Melt - Experimental Constraints and Applications for the Subduction Zone and Magma Ocean Carbon Cycles

    … of CO2 solubility on natural hydrous rhyolitic melts. These studies are applicable to subduction zone settings of the Earth throughout its history. Carbon concentrations and speciation were measured using FTIR, and in the process, we determined absorption coefficients for the CO2 species …

    rice Repository record for Carbon in Silicate Melt - Experimental Constraints and Applications for the Subduction Zone and Magma Ocean Carbon Cycles (opens in a new tab)

  4. Trace element geochemistry of oceanic peridotites and silicate melt inclusions : implications for mantle melting and ocean ridge magmagenesis

    The mantle melting process is fundamental to basalt genesis and crustal accretion at mid-ocean ridges. It is believed that melts ascend more rapidly than the surrounding mantle, implying a process similar to fractional melting may be occurring, but geochemical evidence for this has been lacking. …

    woods-hole Repository record for Trace element geochemistry of oceanic peridotites and silicate melt inclusions : implications for mantle melting and ocean ridge magmagenesis (opens in a new tab)

  5. Trace element geochemistry of oceanic peridotites and silicate melt inclusions--implications for mantle melting and ocean ridge magmagenesis

    Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, and Woods Hole Oceanographic Institution, 1990.

    mit Repository record for Trace element geochemistry of oceanic peridotites and silicate melt inclusions--implications for mantle melting and ocean ridge magmagenesis (opens in a new tab)

  6. Studies of Magmatism by Trace Element Partitioning Between Clinopyroxene and Silicate Melt, Uranium-Series Disequilibria in Lavas From Subduction Zones, and Non-Traditional Stable Isotopes

    … Fe-Mg isotopic fractionations occur in the melt-present portion of the experiment. I conclude that the positive co-variation of Fe-Mg isotopes could be an important fingerprint of magma differentiation in a temperature gradient.

    uiuc Repository record for Studies of Magmatism by Trace Element Partitioning Between Clinopyroxene and Silicate Melt, Uranium-Series Disequilibria in Lavas From Subduction Zones, and Non-Traditional Stable Isotopes (opens in a new tab)

  7. Ghost granophyre: A new texture with implications for plagiogranite differentiation and Ti-in-Quartz thermometry

    … flow of recently described low temperature silicate liquids which span the magmatic-hydrothermal transition, as well as a way to make granophyre without the involvement of a silicate melt. These findings expand the definition of the term granophyre, which still sees heavy usage in the …

    uiuc Repository record for Ghost granophyre: A new texture with implications for plagiogranite differentiation and Ti-in-Quartz thermometry (opens in a new tab)

  8. Geochemical Evolution at White Island, New Zealand

    … deposits. In this study, the geochemistry of the silicate melt at White Island has been characterized through detailed studies of silicate melt inclusions, phenocrysts, and matrix glass contained in recent ejecta (1977-1991). Most melt inclusions contained only glass, however, daughter minerals …

    vt Repository record for Geochemical Evolution at White Island, New Zealand (opens in a new tab)

  9. Development of New Methods to Control Redox Conditions in High-pressure Experiments and their Application to Study Ore Metal Solubilities in Sulfur-bearing Magmatic Fluids

    … comparing redox-dependent Cu solubilities in silicate melts at fO2 imposed by redox buffers and identical target fO2 imposed by the hydrogen membrane confirmed consistency between the two methods within 0.3 log units fO2 deviation at T=1000⁰C and P=2000 bar. Experiments using Fe(II)-Mg …

    toronto-retro Repository record for Development of New Methods to Control Redox Conditions in High-pressure Experiments and their Application to Study Ore Metal Solubilities in Sulfur-bearing Magmatic Fluids (opens in a new tab)

  10. The partial molar volume of carbon dioxide in peridotite partial melt at high pressure

    The partial molar volume of CO2 (VCO2) in silicate melt was determined for a komatiite composition using high pressure sink/float experiments in a multi-anvil press. The density of the experimental melt at pressure was determined by observing sinking and floating of pure forsterite (Fo100) and 90% …

    unm Repository record for The partial molar volume of carbon dioxide in peridotite partial melt at high pressure (opens in a new tab)

  11. The Early Evolution of Terrestrial Planets: Impact Simulations and Planetary Chemistry

    … the interacting atmosphere and impact- generated silicate melt. We analyse the production of reduced atmospheric species (e.g., H<sub>2</sub>, CH<sub>4</sub>, NH<sub>3</sub>), which are important to proposed prebiotic chemical pathways. We also analyse the geochemical signatures that such impacts …

    cambridge Repository record for The Early Evolution of Terrestrial Planets: Impact Simulations and Planetary Chemistry (opens in a new tab)

  12. Melt Inclusion Geochemistry

    Silicate melt inclusions (MI) are small samples of melt that are trapped during crystal growth at magmatic pressures and temperatures. The MI represent a sample of the melt that was isolated from the magma during host crystal growth. Thus, MI provide a valuable tool for constraining the magmatic …

    vt Repository record for Melt Inclusion Geochemistry (opens in a new tab)

  13. Characterization of Impact Melt Rocks and Hydrothermal Mineralization at the Haughton Impact Structure, Devon Island, Canada: An Investigation of Impacts into Carbonate Targets

    … impact, in particular whether they undergo melting or decomposition, is actively debated. The dominant process is significant as decomposition would cause severe climatic effects due to release of large amounts of carbon dioxide into the atmosphere. At the root of the problem is the …

    uwo Repository record for Characterization of Impact Melt Rocks and Hydrothermal Mineralization at the Haughton Impact Structure, Devon Island, Canada: An Investigation of Impacts into Carbonate Targets (opens in a new tab)

  14. Platinum-group elements in the ultrabasic rocks of the Braganca and Morais massifs, northern Portugal

    … the chromite mineralisation was derived from melts of boninitic affinity. The relatively high Pd/Cu ratios calculated for a silicate melt from which the chromite crystallised are consistent with this. The composition of the chromite grains, having 1000r/(Cr+Al) ratios clustering around 75, is …

    the-open-u Repository record for Platinum-group elements in the ultrabasic rocks of the Braganca and Morais massifs, northern Portugal (opens in a new tab)

  15. Metal-silicate Partitioning Behavior of Molybdenum, Tungsten, and Nickel: Implications for Core Formation

    … solid state convection and thus decompression melting and hot spot volcanism. Therefore determining how Earth's core formed and if that process was unique to our planet in the solar system is of great scientific interest. Core formation can be studied experimentally by examining the …

    unm Repository record for Metal-silicate Partitioning Behavior of Molybdenum, Tungsten, and Nickel: Implications for Core Formation (opens in a new tab)

  16. Using Lunar Apatite to Assess the Volatile Inventory of the Lunar Interior

    … volatiles (H<sub>2</sub>O, Cl, F) within lunar melt inclusions, glass beads, and the mineral apatite have challenged the previously held notion that the Moon is depleted in volatiles. As the most widespread volatile-bearing phase, apatite has been the focus of many studies aiming to constrain …

    the-open-u Repository record for Using Lunar Apatite to Assess the Volatile Inventory of the Lunar Interior (opens in a new tab)

  17. The X-discontinuity: Seismic signatures of a heterogeneous upper mantle

    … transition and/or the presence of carbonated silicate melt, shedding insight into the nature of mantle plumes and their role in mantle convection. I study the presence of the X beneath Africa, using continuous observations and a vote map style procedure to understand the length scales of the …

    cambridge Repository record for The X-discontinuity: Seismic signatures of a heterogeneous upper mantle (opens in a new tab)

  18. Origin of the Kleva Ni-Cu sulphide mineralisation in Småland, southeast Sweden

    … a basaltic magma that formed through partial melting of a metasomatically refertilised mantle wedge underneath an Andean-type continental magmatic arc. Lu-Hf signatures of zircon, together with other rocks of Palaeoproterozoic Fennoscandia indicate alternating stages of extension and …

    lund Repository record for Origin of the Kleva Ni-Cu sulphide mineralisation in Småland, southeast Sweden (opens in a new tab)

  19. Experimental constraints on the thermodynamic modelling of siderophile element distribution during core-segregation and basalt petrogenesis

    … edge structure (XANES) spectroscopic study of silicate glasses, synthesized at high pressure and quenched isobarically, has been conducted in order to assess the effect of pressure on the coordination environment of divalent Ni, Co, Fe, trivalent Fe and hexavalent W. The principle Ni …

    aus-cath Repository record for Experimental constraints on the thermodynamic modelling of siderophile element distribution during core-segregation and basalt petrogenesis (opens in a new tab)

  20. Experimental constraints on the thermodynamic modelling of siderophile element distribution during core-segregation and basalt petrogenesis

    … edge structure (XANES) spectroscopic study of silicate glasses, synthesized at high pressure and quenched isobarically, has been conducted in order to assess the effect of pressure on the coordination environment of divalent Ni, Co, Fe, trivalent Fe and hexavalent W. The principle Ni …

    anu Repository record for Experimental constraints on the thermodynamic modelling of siderophile element distribution during core-segregation and basalt petrogenesis (opens in a new tab)

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