Hydrothermal exploration with the Autonomous Benthic Explorer

[1]  C. German,et al.  Hydrothermal activity on the ultra‐slow spreading southern Knipovich Ridge , 2007 .

[2]  E. Baker,et al.  Opposing trends in crustal thickness and spreading rate along the back-arc Eastern Lau Spreading Center: Implications for controls on ridge morphology, faulting, and hydrothermal activity , 2006 .

[3]  E. Baker,et al.  Abundant hydrothermal venting along melt‐rich and melt‐free ridge segments in the Lau back‐arc basin , 2006 .

[4]  H. Elderfield.  The oceans and marine geochemistry , 2006 .

[5]  E. Baker,et al.  Hydrothermal activity on near‐arc sections of back‐arc ridges: Results from the Mariana Trough and Lau Basin , 2005 .

[6]  C. German,et al.  Iron (II) distribution and oxidation kinetics in hydrothermal plumes at the Kairei and Edmond vent sites, Indian Ocean , 2005 .

[7]  E. Baker,et al.  Tectonic/volcanic segmentation and controls on hydrothermal venting along Earth's fastest seafloor spreading system, EPR 27°–32°S , 2004 .

[8]  C. Langmuir,et al.  Hydrothermal venting in magma deserts: The ultraslow‐spreading Gakkel and Southwest Indian Ridges , 2004 .

[9]  C. German,et al.  The Thermal Structure of the Oceanic Crust, Ridge-Spreading and Hydrothermal Circulation: How Well do we Understand their Inter-Connections? , 2004 .

[10]  C. German,et al.  Mid-ocean ridges : hydrothermal interactions between the lithosphere and oceans , 2004 .

[11]  Dana R. Yoerger,et al.  Deep submergence synergy: Alvin and ABE explore the gálapagos rift at 86°W , 2003 .

[12]  C. German.  Hydrothermal activity on the eastern SWIR (50°–70°E): Evidence from core‐top geochemistry, 1887 and 1998 , 2003 .

[13]  C. Langmuir,et al.  Discovery of abundant hydrothermal venting on the ultraslow-spreading Gakkel ridge in the Arctic Ocean , 2003, Nature.

[14]  Suzanne M. Carbotte,et al.  Magmatic subsidence of the East Pacific Rise (EPR) at 18°14′S revealed through fault restoration of ridge crest bathymetry , 2003 .

[15]  J. Charlou,et al.  Geochemistry of high H2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14'N, MAR) , 2002 .

[16]  E. Baker,et al.  Discovery of ancient and active hydrothermal systems along the ultra‐slow spreading Southwest Indian Ridge 10°–16°E , 2002 .

[17]  G. F. Lane-Serff,et al.  Flow and mixing in the rift valley of the Mid-Atlantic Ridge , 2002 .

[18]  E. Oelkers,et al.  The rainbow vent fluids (36°14′N, MAR): the influence of ultramafic rocks and phase separation on trace metal content in Mid-Atlantic Ridge hydrothermal fluids , 2002 .

[19]  C. German,et al.  Evolution and Biogeography of Deep-Sea Vent and Seep Invertebrates , 2002, Science.

[20]  Christopher R. German,et al.  Temporal variability of the hydrothermal plume above the Kairei vent field, 25°S, Central Indian Ridge , 2002 .

[21]  J. Charlou,et al.  Initial indications of abiotic formation of hydrocarbons in the Rainbow ultramafic hydrothermal system, Mid-Atlantic Ridge , 2001 .

[22]  C. German,et al.  Distribution and behavior of dissolved hydrogen sulfide in hydrothermal plumes , 2001 .

[23]  P. Tyler,et al.  Hydrothermal plumes above the East Scotia Ridge: an isolated high-latitude back-arc spreading centre , 2000 .

[24]  R. Sherrell,et al.  Dissolved and particulate Fe in a hydrothermal plume at 9°45′N, East Pacific Rise:: Slow Fe (II) oxidation kinetics in Pacific plumes , 2000 .

[25]  E. Baker,et al.  Hydrothermal activity along the southwest Indian ridge , 1998, Nature.

[26]  C. German,et al.  Distributions of hydrothermal activity along the Mid-Atlantic Ridge: interplay of magmatic and tectonic controls , 1998 .

[27]  C. R. German,et al.  Hydrothermal Plume Detection in the Deep Ocean—A Combination of Technologies , 1998 .

[28]  C. German,et al.  Topographic control of a dispersing hydrothermal plume , 1998 .

[29]  E. Baker,et al.  The relationship between near-axis hydrothermal cooling and the spreading rate of mid-ocean ridges , 1996 .

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

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

[32]  H. Elderfield,et al.  Near-field variability of the TAG non-buoyant plume, 26°N, Mid-Atlantic Ridge , 1994 .

[33]  J. Charlou,et al.  Hydrothermal methane venting between 12°N and 26°N along the Mid‐Atlantic Ridge , 1993 .

[34]  Robert J Collier,et al.  Chemical reaction rates and entrainment within the Endeavour Ridge hydrothermal plume , 1990 .

[35]  Peter A. Rona,et al.  A model of an Atlantic and Pacific hydrothermal plume , 1989 .

[36]  P. Rona,et al.  Hydrothermal manganese plumes in the Mid-Atlantic Ridge rift valley , 1985, Nature.

[37]  F. Morel.  Principles of Aquatic Chemistry , 1983 .

[38]  H. Elderfield,et al.  Rare earth elements in seawater near hydrothermal vents , 1983, Nature.

[39]  J. Lupton,et al.  A Major Helium-3 Source at 15�S on the East Pacific Rise , 1981, Science.

[40]  J. Middleton.  Times of rise for turbulent forced plumes , 1979 .

[41]  Mitchell W Lyle,et al.  The chemistry of hydrothermal mounds near the Galapagos Rift , 1978 .

[42]  J. Turner,et al.  Buoyancy Effects in Fluids , 1973 .

[43]  Geoffrey Ingram Taylor,et al.  Turbulent gravitational convection from maintained and instantaneous sources , 1956, Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences.