Vn. Lukashin et al., Particle fluxes, mineralogy, and chemistry of sedimentary material in the broken spur hydrothermal field, Mid-Atlantic Ridge, 29 degrees N, GEOCHEM INT, 38(4), 2000, pp. 331-342
The particle flux near the Saracen's Head "black smoker," Broken Spur hydro
thermal field, was determined using a sediment trap. We studied the mineral
ogical and chemical composition of the material. The ore minerals are Fe su
lfides (pyrite and pyrrhotite), and Zn and Cu sulfides, which occur in equa
lly low amounts. Ca minerals (anhydrite, gypsum, and calcite) are the major
gangue minerals. The sediment traps within and below the hydrothermal plum
e collected mainly biogenic material with an admixture of hydrothermal comp
onents. This material is enriched in Fe, Zn, Ca, Si, Ba, and P relative to
the background concentrations.