Gravity core MSM101_44-3 was recovered from the St. Anns Basin on the northeastern Scotian Shelf (45°46.651′N, 58°31.967′W) at 274 m water depth during expedition MSM101 (RV...
Serpentinization of abyssal peridotites is known to produce extremely reducing conditions as a result of dihydrogen (H2,aq) release upon oxidation of ferrous iron in primary...
We propose to determine the mineral phase composition in 15 iron stone samples from the Tall Bazi excavation site in Syria. The results of this investigation will be compared...
