Mo, Sr, Nd isotopes and major and trace element concentrations for lavas and enclaves from Solander Volcano, basement rocks and one altered oceanic basalt

The dataset contains major, trace element concentrations and Mo (stable), Sr (radiogenic) and Nd (radiogenic) isotope composition of lavas and enclaves from Solander Volcano (Solander and Little Solander Islands) as well as local basement rocks (xenoliths or borehole samples) and one local AOC (altered oceanic crust) sample. Major elements were analysed by XRF at the University of Wollongong; trace elements by ICP-MS and Sr and Nd isotopic compositions by TIMS at Macquarie University; Th, Zr, Hf and Y by LA-ICP-MS at the Australian National University; Mo compositions by MC-ICP-MS at the University of Göttingen; and S by IR-SP at the University of Münster. These data are published as a supplement to Bezard et al. (submitted), The role of exsolved fluids on the Mo isotopic composition of arc lavas: insights from the adakitic rocks of Solander volcano, Geochemistry, Geophysics, Geosystems. A subset of these data were previously published in Foley et al. (2012). Magmatic Evolution and Magma Mixing of Quaternary Adakites at Solander and Little Solander Islands, New Zealand, Journal of Petrology, 54(4), 703–744, https://doi.org/10.1093/petrology/egs082 and Foley et al. (2014). 10Be, 18O and radiogenic isotopic constraints on the origin of adakitic signatures: a case study from Solander and Little Solander Islands, New Zealand, Contributions to Mineralogy and Petrology, 168(3), https://doi.org/10.1007/s00410-014-1048-9. This work was funded by the German Research Foundation (DFG Grant BE 6670/1-1, Project No. 418227749) and Australian Research Council Discovery Project 0986232.