An off-axis hydrothermal vent field near the Mid-Atlantic Ridge at 30° N

[1]  J. Charlou,et al.  Compared geochemical signatures and the evolution of Menez Gwen (37°50′N) and Lucky Strike (37°17′N) hydrothermal fluids, south of the Azores Triple Junction on the Mid-Atlantic Ridge , 2000 .

[2]  L. Parson,et al.  Non-transform offsets along the Mid-Atlantic Ridge south of the Azores (38°N–34°N): ultramafic exposures and hosting of hydrothermal vents , 2000 .

[3]  E. Shock,et al.  Distinguishing ultramafic‐from basalt‐hosted submarine hydrothermal systems by comparing calculated vent fluid compositions , 2000 .

[4]  Cindy Lee Van Dover,et al.  The Ecology of Deep-Sea Hydrothermal Vents , 2000 .

[5]  S. Petersen,et al.  A model for growth of steep-sided vent structures on the Endeavour Segment of the Juan de Fuca Ridge: Results of a petrologic and geochemical study (Paper 1999JB900107) , 1999 .

[6]  M. Schulte,et al.  Organic synthesis during fluid mixing in hydrothermal systems , 1998 .

[7]  Deborah K. Smith,et al.  Origin of extensional core complexes: Evidence from the Mid‐Atlantic Ridge at Atlantis Fracture Zone , 1998 .

[8]  C. German,et al.  FAMOUS and AMAR segments on the Mid-Atlantic Ridge: ubiquitous hydrothermal Mn, CH4, δ3He signals along the rift valley walls and rift offsets , 1998 .

[9]  J. Charlou,et al.  Intense CH4 plumes generated by serpentinization of ultramafic rocks at the intersection of the 15°20′N fracture zone and the Mid-Atlantic Ridge , 1998 .

[10]  R. Showstack.  Clinton proposes science funding increase , 1998 .

[11]  J. Karson,et al.  Faulting and magmatism at mid-ocean ridges , 1998 .

[12]  N. Pace.  A molecular view of microbial diversity and the biosphere. , 1997, Science.

[13]  M. Russell,et al.  The emergence of life from iron monosulphide bubbles at a submarine hydrothermal redox and pH front , 1997, Journal of the Geological Society.

[14]  J. Karson,et al.  Tectonic setting of serpentinite exposures on the western median valley wall of the MARK area in the vicinity of Site 920 , 1997 .

[15]  J. Cann,et al.  Corrugated slip surfaces formed at ridge–transform intersections on the Mid-Atlantic Ridge , 1997, Nature.

[16]  William E Seyfried,et al.  Reduction of CO2 during serpentinization of olivine at 300 °C and 500 bar , 1996 .

[17]  C. German,et al.  Hydrothermal exploration near the Azores Triple Junction: tectonic control of venting at slow-spreading ridges? , 1996 .

[18]  G. Früh-Green,et al.  Petrologic and stable isotope constraints on hydrothermal alteration and serpentinization of the EPR shallow mantle at Hess Deep (Site 895) , 1996 .

[19]  M. Palmer,et al.  The chemistry of hydrothermal fluids from the Broken Spur site, 29°N Mid-Atlantic ridge , 1995 .

[20]  Susan E. Humphris,et al.  Seafloor hydrothermal systems : physical, chemical, biological, and geological interactions , 1995 .

[21]  L. Parson,et al.  Hydrothermal vents and processes , 1995, Geological Society, London, Special Publications.

[22]  G. Massoth,et al.  Gradients in the composition of hydrothermal fluids from the Endeavour segment vent field: Phase separation and brine loss , 1994 .

[23]  M. Lilley,et al.  Anomalous CH4 and NH4+ concentrations at an unsedimented mid-ocean-ridge hydrothermal system , 1993, Nature.

[24]  J. Charlou,et al.  Hydrothermal circulation, serpentinization, and degassing at a rift valley-fracture zone intersection: Mid-Atlantic Ridge near 15°N, 45°W , 1992 .

[25]  W. Seyfried,et al.  The effect of temperature on metal mobility in subseafloor hydrothermal systems: constraints from basalt alteration experiments , 1990 .

[26]  M. Kusakabe,et al.  Origin of waters responsible for serpentinization of the Izu-Ogasawara-Mariana forearc seamounts in view of hydrogen and oxygen isotope ratios , 1990 .

[27]  M. E. Mackay,et al.  4. CONICAL SEAMOUNT: SeaMARC II, ALVIN SUBMERSIBLE, AND SEISMIC-REFLECTION STUDIES 1 , 1990 .

[28]  R. Batiza,et al.  Seamounts, Islands, and Atolls , 1987 .

[29]  W. Seyfried,et al.  Hydrothermal serpentinization of peridotite within the oceanic crust: Experimental investigations of mineralogy and major element chemistry , 1986 .

[30]  C. Neal,et al.  Calcium and magnesium hydroxide precipitation from alkaline groundwaters in Oman, and their significance to the process of serpentinization , 1984, Mineralogical Magazine.

[31]  C. Neal,et al.  Hydrogen generation from mantle source rocks in Oman , 1983 .

[32]  J. William Schopf,et al.  Earth's earliest biosphere : its origin and evolution , 1983 .

[33]  E. Bonatti,et al.  Aragonite from deep sea ultramafic rocks , 1980 .

[34]  Richard A. Sheppard,et al.  Metamorphic assemblages and the direction of flow of metamorphic fluids in four instances of serpentinization , 1972 .

[35]  R. Coleman.  Petrologic and Geophysical Nature of Serpentinites , 1971 .