SUP18684
Geological Society Supplementary Publication No. SUP18684
Parent Paper: Evolution of volcanism and magmatism during initial arc stage: constraints on the tectonic setting of the Oman Ophiolite
Y. KUSANO, M. HAYASHI, Y. ADACHI, S. UMINO & S. MIYASHITA
Appearing in Tectonic Evolution of the Oman Mountains. Geological Society, London, Special Publications, 392 http://dx.doi.org/10.1144/SP392.9
Locations, mode of occurrence, phenocryst assemblages and bulk-rock major and trace element compositions of lavas in the Wadi Bidi are provided as .csv files:
Table 1: Locations, mode of occurrence and phenocryst assemblages of the Wadi Bidi lavas. Pl, plagioclase; Ol, olivine; Cpx, clinopyroxene; Opx, orthopyroxene; Spl, spinel. (.csv5Kb)
Table 2: Bulk-rock major and trace element compositions analysed by XRF. (.csv8Kb)
Table 3: Bulk-rock trace element compositions analysed by ICP-MS. Duplicate analyses of USGS W-2 (diabase) and the recommended values by Eggins et al. (1997) are shown along with relative deviations between the measured and recommended values. (.csv9Kb)