Kinematics and geometry of active detachment faulting beneath the Trans-Atlantic Geotraverse (TAG) hydrothermal field on the Mid-Atlantic Ridge

Low-temperature iron and manganese mineral phases of an inactive hydrothermal mound; TAG hydrothermal field, Mid-Atlantic Ridge

The occurrence of gold in sulfide deposits of the TAG hydrothermal field, Mid-Atlantic Ridge

Active and relict sea-floor hydrothermal mineralization at the TAG hydrothermal field, Mid-Atlantic Ridge

Conductive heat flow anomalies associated with hydrothermal sulfide mounds

Hydrothermal quartz vug from the Mid-Atlantic Ridge

Noble metals in seafloor hydrothermal mineralization from the Juan de Fuca and Mid-Atlantic ridges; a fractionation of gold from platinum metals in hydrothermal fields

Near-seafloor magnetics reveal tectonic rotation and deep structure at the TAG (Trans-Atlantic Geotraverse) hydrothermal site (Mid-Atlantic Ridge, 26°N)

Hydrothermal circulation and the dike-gabbro transition in the detachment mode of slow seafloor spreading

Mineralogy, sulphur isotope geochemistry and the development of sulphide structures at the Broken Spur hydrothermal vent site, 29°10’N, Mid-Atlantic Ridge

Oceanic detachment faults focus very large volumes of black smoker fluids

Self-organization of submarine hydrothermal siliceous deposits: Evidence from the TAG hydrothermal mound, 26°N Mid-Atlantic Ridge

Chemistry of ore-forming fluids and mineral formation rates in an active hydrothermal sulfide deposit on the Mid-Atlantic Ridge

The formation of atacamite during weathering of sulfides on the modern seafloor

Gold-rich sea-floor gossans in the Troodos Ophiolite and on the Mid-Atlantic Ridge

Block-tilting, transfer faults, and structural control of magmatic and hydrothermal processesin the TAG area, Mid-Atlantic Ridge 26°N

Sulfidation equilibria as guides to gold mineralization in volcanogenic massive sulfides; evidence from sulfide mineralogy and the composition of sphalerite

Hydrothermal mineralization at oceanic ridges

Active vents and massive sulfides at 26 degrees N (TAG) and 23 degrees N (Snakepit) on the Mid-Atlantic Ridge