Time Series Studies and Drilling Results from IODP Expedition 376 to Brothers Volcano, New Zealand: Insights into Petrology, Hydrothermal Processes, and Mineralization—Introduction

Indian Ocean Ridge System and Seafloor Hydrothermal Activity

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

Oceanic detachment faults focus very large volumes of black smoker fluids

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

Conductive heat flow anomalies associated with hydrothermal sulfide mounds

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

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

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 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

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

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

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

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

Hydrothermal mineralization at oceanic ridges