Halogen variations in alkaline rocks from the Upper Rhine Graben (SW Germany): Insights into F, Cl and Br behavior during magmatic processes

We present halogen compositions in a series of alkaline rocks from the Kaiserstuhl, Hegau and Urach areas of the Upper Rhine Graben region (South Germany). Most primitive rocks (olivine melilitites and olivine nephelinites) have lower Cl and Br concentrations (generally below 100μg/g and below 0.3μg/g, respectively) compared to more evolved tephrites, phonolites and related rocks (up to 7600μg/g Cl and 34μg/g Br). However, the Cl/Br ratios of the majority of the investigated samples are relatively uniform (371±120), regardless of rock type and sample locality, suggesting that partial melting, fractional crystallization, and degassing have limited effects on the fractionation of Cl from Br. The mean value of the Cl/Br ratio is similar to previous estimates for basaltic rocks representing MORB and OIB mantle signatures. Fluorine concentrations of the primitive rocks show limited variations (900–1100μg/g) and are within the range defined by the evolved rocks (400–2100μg/g), but are much higher than previous estimates for the MORB and OIB mantle (50–135μg/g). This may indicate a relatively F-rich mantle source beneath the Rhine Graben region. In contrast to Cl/Br ratios, the F/Cl ratios vary significantly over three orders of magnitudes (from