Magmatic events can produce rapid changes in hydrothermal vent chemistry.
about
Discovery of new hydrothermal activity and chemosynthetic fauna on the Central Indian Ridge at 18°-20° SThe sound generated by mid-ocean ridge black smoker hydrothermal vents.Microbial ecology of the dark ocean above, at, and below the seafloor.Abundances of hyperthermophilic autotrophic Fe(III) oxide reducers and heterotrophs in hydrothermal sulfide chimneys of the northeastern Pacific Ocean.Qualitative and quantitative analysis of CO2 and CH4 dissolved in water and seawater using laser Raman spectroscopy.Characterization and quantitation of a tertiary mixture of salts by Raman spectroscopy in simulated hydrothermal vent fluid.Abiogenic hydrocarbon production at lost city hydrothermal field.Hydrogen and thiosulfate limits for growth of a thermophilic, autotrophic Desulfurobacterium species from a deep-sea hydrothermal vent.Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll.Magnetite formation from ferrihydrite by hyperthermophilic archaea from Endeavour Segment, Juan de Fuca Ridge hydrothermal vent chimneys.Young volcanism and related hydrothermal activity at 5°S on the slow-spreading southern Mid-Atlantic RidgeHydrological response to a seafloor spreading episode on the Juan de Fuca ridgeTemporal variability and tidal modulation of hydrothermal exit-fluid temperatures at the Lucky Strike deep-sea vent field, Mid-Atlantic RidgePhase equilibria controls on the chemistry of vent fluids from hydrothermal systems on slow spreading ridges: Reactivity of plagioclase and olivine solid solutions and the pH-silica connectionDissolved carbon species in associated diffuse and focused flow hydrothermal vents at the Main Endeavour Field, Juan de Fuca Ridge: Phase equilibria and kinetic constraintsThe Chemistry of Diffuse-Flow Vent Fluids on the Galapagos Rift (86°W)° Temporal Variability and Subseafloor Phase Equilibria Controls
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P2860
Magmatic events can produce rapid changes in hydrothermal vent chemistry.
description
2003 nî lūn-bûn
@nan
2003年の論文
@ja
2003年論文
@yue
2003年論文
@zh-hant
2003年論文
@zh-hk
2003年論文
@zh-mo
2003年論文
@zh-tw
2003年论文
@wuu
2003年论文
@zh
2003年论文
@zh-cn
name
Magmatic events can produce rapid changes in hydrothermal vent chemistry.
@en
Magmatic events can produce rapid changes in hydrothermal vent chemistry.
@nl
type
label
Magmatic events can produce rapid changes in hydrothermal vent chemistry.
@en
Magmatic events can produce rapid changes in hydrothermal vent chemistry.
@nl
altLabel
Magmatic events can produce rapid changes in hydrothermal vent chemistry
@en
prefLabel
Magmatic events can produce rapid changes in hydrothermal vent chemistry.
@en
Magmatic events can produce rapid changes in hydrothermal vent chemistry.
@nl
P2093
P2860
P356
P1433
P1476
Magmatic events can produce rapid changes in hydrothermal vent chemistry.
@en
P2093
Eric J Olson
John E Lupton
Marvin D Lilley
P2860
P2888
P304
P356
10.1038/NATURE01569
P407
P577
2003-04-01T00:00:00Z
P6179
1045548408
P698
P819
2003Natur.422..878L