Boron isotope systematics of a fossil hydrothermal system from the Troodos ophiolite, Cyprus: Water–rock interactions in the oceanic crust and subseafloor ore deposits

Abstract

Abstract We determined concentrations and isotopic compositions of boron in a complete section of the hydrothermally altered Cretaceous oceanic crust of the Troodos ophiolite. The boron content and δ 11 B value for each lithological section are: pillow lava (3.8–206.8 μg/g, 63 μg/g average; δ 11 B = + 0.17‰ to + 15.6‰, + 8.1‰ average), sheeted dike complex (0.6–18.0 μg/g, 4.0 μg/g average; δ 11 B = + 3.3‰ to + 10.6‰, + 6.0‰ average), and plutonic complex (0.3–8.4 μg/g, 1.7 μg/g average; δ 11 B = − 1.7‰ to + 18.5‰, + 4.5‰ average). These boron contents are higher than the estimated original igneous values throughout the oceanic crust, indicating uptake of boron from seawater and hydrothermal fluid at temperatures ranging from ≤ 50 °C to > 300 °C. Although our boron data for the Troodos ophiolite are generally consistent with those for the Oman ophiolite of similar age, the distinctly low δ 11 B values of the lower gabbro section in the Troodos ophiolite ( 11 B-depleted fluid at a very small water/rock ratio. The boron content of the bulk oceanic crust (12.3 μg/g) estimated for the Troodos ophiolite is relatively high as a result of strong boron enrichment in the pillow lava section, which underwent prolonged seafloor weathering. Despite these differences, the weighted average δ 11 B value of the bulk oceanic crust (+ 7.6‰) is similar to that of the Oman ophiolite (+ 7.9‰). We also analyzed the boron isotope geochemistry of a subseafloor hydrothermal stockwork sulfide deposit in the Troodos ophiolite to investigate its formation processes. In contrast to the normal upper oceanic crust, the δ 11 B values of the rocks below the ore body decrease with increasing depth and have large negative values (− 6‰) in the highly altered uppermost dike section. These low δ 11 B values are coupled with high boron contents (2.5–17 μg/g) and high and uniform 87 Sr/ 86 Sr ratios (0.7064 average), and are unlikely to have resulted from interactions with fluids at a small water/rock ratio. These characteristics are better explained by interaction of ore-forming hydrothermal fluids with oceanic crust that had previously been enriched in boron through hydrothermal alteration at low temperatures. These observations demonstrate that boron and boron isotopes are useful for quantitative evaluation of fluid-related processes with multiple stages, including petrogenesis of hydrothermal ore deposits.