Showing 14,121 - 14,140 results of 32,159 for search '(( 50 ((nn decrease) OR (we decrease)) ) OR ( 5 ((wt decrease) OR (mean decrease)) ))', query time: 0.98s Refine Results
  1. 14121

    Presentation1.ppt by Julien Leuthold (4921660)

    Published 2018
    “…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr<sup>*</sup> ratios increase. …”
  2. 14122

    Table1.xlsx by Julien Leuthold (4921660)

    Published 2018
    “…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr<sup>*</sup> ratios increase. …”
  3. 14123
  4. 14124

    Image1.JPEG by Julien Leuthold (4921660)

    Published 2018
    “…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr<sup>*</sup> ratios increase. …”
  5. 14125
  6. 14126
  7. 14127
  8. 14128

    Table4.XLSX by Julien Leuthold (4921660)

    Published 2018
    “…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr<sup>*</sup> ratios increase. …”
  9. 14129
  10. 14130

    Table2.xlsx by Julien Leuthold (4921660)

    Published 2018
    “…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr<sup>*</sup> ratios increase. …”
  11. 14131

    Table3.XLSX by Julien Leuthold (4921660)

    Published 2018
    “…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr<sup>*</sup> ratios increase. …”
  12. 14132
  13. 14133
  14. 14134
  15. 14135

    Image4.jpg by Julien Leuthold (4921660)

    Published 2018
    “…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr<sup>*</sup> ratios increase. …”
  16. 14136

    Image2.JPEG by Julien Leuthold (4921660)

    Published 2018
    “…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr<sup>*</sup> ratios increase. …”
  17. 14137

    Image3.jpg by Julien Leuthold (4921660)

    Published 2018
    “…Kane Megamullion and Hess Deep clinopyroxene core1 primocrysts and their plagioclase inclusions indicate crystallization from high temperature basalt (>1,160 and >1,200°C, respectively), close to clinopyroxene saturation temperature (<50% and <25% crystallization). Step-like compatible Cr (and co-varying Al) and incompatible Ti, Zr, Y and rare earth elements (REE) decrease from anhedral core1 to overgrown core2, while Mg# and Sr/Sr<sup>*</sup> ratios increase. …”
  18. 14138
  19. 14139
  20. 14140