共 39 条
[1]
HydrothermalalterationoforganicmatterinsedimentsoftheNortheasternPacificOcean:Part1.MiddleValley,JuandeFucaRidge. RushdiAI,SimoneitBRT. Applied Geochemistry . 2002
[2]
Origin of elevated sediment permeability in a hydrothermal seepage zone, eastern flank of the Juan de Fuca Ridge, and implications for transport of fluid and heat. Giambalvo E R,Fisher A T,Martin J T,et al. Chinese Journal of Geophysics . 2000
[3]
Rare earth element mobility in the oceanic lower sheeted dyke complex: Evidence from geochemical data and leaching experiments. Bach W,Irber W. Chemical Geology . 1998
[4]
Chemical fluxes during hydrothermal alteration of a 1200-m long section of dikes in the oceanic crust, DSDP/ODP Hole 504B. Laverne C,Agrinier P,Hermitte D,et al. Chemical Geology . 2001
[5]
Discharge of hydrothermal fluids through sediment at the Escanaba Trough, Gorda Ridge(ODP Leg 169): Assessing the effects on the rock magnetic signal. Urbat M,Dekkers M J,Krumsiek K. Earth and Planet . 2000
[6]
Dissolved organic carbon in interstitial waters from sediments of Middle Valley and Escanaba Trough, Northeast Pacific, ODP Legs 139 and 169. Simoneit B R T,Sparrow M A. Applied Geochemistry . 2002
[7]
Amino acid abundances and stereochemistry in hydrothermally altered sediments from the Juan de Fuca Ridge, northeastern Pacific Ocean. Andersson E,Simoneit B R T,Holm N G. Applied Geochemistry . 2000
[8]
Two-dimensional variations of exchangeable cation composition in the terrigenous sediment, eastern flank of the Juan de Fuca Ridge. Inoue A. Marine Geology . 2000
[9]
Hydrothermal geochemistry of sediments and pore waters in Escanaba Trough—ODP Leg 169. Gieskes J M,Simoneit B R T,Goodfellow W D,et al. Applied Geochemistry . 2002
[10]
The alkali element and boron geochemistry of the Escanaba Trough sediment-hosted hydrothermal system. James R H,Rudnicki M D,Palmer M R. Earth and Planet . 1999