Mineral and whole-rock geochemistry of high-Al podiform chromitites in the Fizh Massif of the Cretaceous Oman ophiolite: origin of hydrous, N–MORB melts in a nascent forearc setting
The Devonian subsurface Adavale Basin occupies a central position in the Paleozoic central Thomson Orogen of eastern Australia and records its tectonic setting during this time interval. Here, we have
This dataset is about: (Table 8) Major and trace element content of basalts from DSDP Hole 49-412A. Please consult parent dataset @ https://doi.org/10.1594/PANGAEA.710816 for more information.
Supplementary Tables 1-8 in the manuscript entitled "The role of sulfate and fluorine in the liquid immiscibility between carbonatitic and silicate melts"