[1] RISE Project Group. East Pacific Rise:Hot springs and geophysical experiments[J]. Science, 1980, 207:1 421-1 444.

[2] Kong L,Ryan W B F,Mayer L,et al. Bare-rock drill sites,ODP Legs 106 and 109:Evidence for hydrothermal activity at 23°N in the Mid-Atlantic ridge rift valley [J]. EOS,1985,65:1 106.

[3] Honnorez J,Mevel C,Honnorez-Guerstein B M. Mineralogy and chemistry of sulfide deposits drilled from hydrothermal mound of the snake pit active field,MAR[A]. In:Detrick R,Honnorez J,Bryan W B,et al, eds. Proceedings of the Ocean Drilling Program,Scientific Results [C].1990,106/109:145-162.

[4] Kase K, Yamamoto M, Shibata T. Copper-rich sulfide deposit near 23°N, Mid-Atlantic Ridge:Chemical composition, mineral chemistry and sulfur isotopes[A]. In:Detrick R,Honnorez J,Bryan W B,et al, eds.Proceedings of the Ocean Drilling Program,Scientific Results [C].1990,106/109:163-177.

[5] Goto S,Kinoshita M,Matsubayashi O,et al. Geothermal constraints on the hydrological regime of the TAG active hydrothermal mound, inferred from long-term monitoring [J]. Earth and Planetary Science Letters, 2002, 203(1):149-163.

[6] Davis E E,Becke K. Observations of natural-state fluid pressures and temperatures in young oceanic crust and inferences regarding hydrothermal circulation [J]. Earth and Planetary Science Letters,2002,204(1/2):231-248.

[7] James R H,Rudnicki M D,Palmer M R. The alkali element and boron geochemistry of the Escanaba Trough sediment-hosted hydrothermal system[J]. Earth and Planetary Science Letters,1999,171(1):157-169.

[8] Gieskes J M, Simoneit B R T, Goodfellow W D,et al.Hydrothermal geochemistry of sediments and pore waters in Escanaba Trough—ODP Leg 169[J].Applied Geochemistry,2002,17(11):1 435-1 456.

[9] Buatier M D,Monnin C,Früh-Green G,et al. Fluid-sediment interactions related to hydrothermal circulation in the Eastern Flank of the Juan de Fuca Ridge[J].Chemical Geology,2001,175(3/4):343-360.

[10] Inoue A. Two-dimensional variations of exchangeable cation composition in the terrigenous sediment, eastern flank of the Juan de Fuca Ridge[J]. Marine Geology,2000,162(2/4):501-528.

[11] Andersson E,Simoneit B R T,Holm N G. Amino acid abundances and stereochemistry in hydrothermally altered sediments from the Juan de Fuca Ridge,northeastern Pacific Ocean[J]. Applied Geochemistry,2000,15(8):1 169-1 190.

[12] Simoneit B R T,Sparrow M A. Dissolved organic carbon in interstitial waters from sediments of Middle Valley and Escanaba Trough,Northeast Pacific,ODP Legs 139 and 169[J]. Applied Geochemistry,2002,17(11):1 495-1 502.

[13] Urbat M,Dekkers M J,Krumsiek K. Discharge of hydrothermal fluids through sediment at the Escanaba Trough, Gorda Ridge (ODP Leg 169):Assessing the effects on the rock magnetic signal[J]. Earth and Planetary Science Letters,2000,176(3/4):481-494.

[14] Laverne C,Agrinier P,Hermitte D,et al. Chemical fluxes during hydrothermal alteration of a 1200-m long section of dikes in the oceanic crust,DSDP/ODP Hole 504B[J]. Chemical Geology,2001,181(1/4):73-98.

[15] Bach W,Irber W. Rare earth element mobility in the oceanic lower sheeted dyke complex:Evidence from geochemical data and leaching experiments[J]. Chemical Geology,1998,151(1/4):309-326.

[16] Michard A,Albarede F. The REE content of some hydrothermal fluids[J]. Chemical Geology,1986,55: 51-60.

[17] Gillis K M,Ludden J N,Smith A D. Mobilization of REE during crustal aging in the Troodos Ophiolite,Cyprus [J]. Chemical Geology,1992,98:71-86.

[18] Chan L-H,Alt J C,Teagle D A H. Lithium and lithium isotope profiles through the upper oceanic crust:A study of seawater-basalt exchange at ODP Sites 504B and 896A[J]. Earth and Planetary Science Letters,2002,201(1):187-201.

[19] Hunter A G,Kempton P D,Greenwood P. Low-temperature fluid-rock interaction—An isotopic and mineralogical perspective of upper crustal evolution,eastern flank of the Juan de Fuca Ridge (JdFR),ODP Leg 168[J]. Chemical Geology,1999,155(1/2):3-28.

[20] Elderfield H,Wheat C G,Mottl M J,et al. Fluid and geochemical transport through oceanic crust:A transect across the eastern flank of the Juan de Fuca Ridge[J]. Earth and Planetary Science Letters,1999,172(1/2):151-165.

[21] Elderfield H,Schultz A. Mid-ocean ridge hydrothermal fluxes and the chemical composition of the oceans [J]. Annual Review of Earth and Planetary Sciences,1996,24:191-224.

[22] Giambalvo E R,Fisher A T,Martin J T,et al. 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 [J]. Journal of Geophysical Research,2000,105:897-912.

[23] Teagle D A H,Alt J C,Chiba H,et al. Strontium and oxygen isotopic constraints on fluid mixing,alteration and mineralization in the TAG hydrothermal deposit[J]. Chemical Geology,1998,149(1/2):1-24.

[24] Teagle D A H,Bickle M J,Alt J C. Recharge flux to ocean-ridge black smoker systems:A geochemical estimate from ODP Hole 504B[J]. Earth and Planetary Science Letters,2003,210:81-89.

[25] Stein C A,Stein S. Constraints on hydrothermal heat flux through the oceanic lithosphere from global heat flow [J]. Journal of Geophysical Research,1994,99:3 081-3 095.

[26] Mottl M J,Wheat C G. Hydrothermal circulation through mid-ocean ridge and anks:Fluxes of heat and magnesium [J]. Geochimica et Cosmochimica Acta,1994,58:2 225-2 237.

[27] Buatier M D,Monnin C,Davis E E,et al. Hydrothermal circulation in the Eastern flank of the Juan de Fuca ridge (Leg ODP 168) [J]. Earth and Planetary Science Letters ,1998,326(3):201-206.

[28] Rudnicki M D,Elderfield H,Mottl M J. Pore fluid advection and reaction in sediments of the eastern flank, Juan de Fuca Ridge,48°N[J]. Earth and Planetary Science Letters,2001,187(1/2):173-189.

[29] Gieskes J M,Simoneit B R T,Shanks W C III,et al. Geochemistry of fluid phases and sediments:Relevance to hydrothermal circulation in Middle Valley,ODP Legs 139 and 169[J]. Applied Geochemistry,2002,17(11): 1 381-1 399.

[30] Kopf A,Behrmann J H,Deyhle A,et al. Isotopic evidence (B, C, O) of deep fluid processes in fault rocks from the active Woodlark Basin detachment zone[J]. Earth and Planetary Science Letters,2003,208(1/2):51-68.

[31] Rushdi A I,Simoneit B R T. Hydrothermal alteration of organic matter in sediments of the Northeastern Pacific Ocean:Part 1.Middle Valley,Juan de Fuca Ridge[J]. Applied Geochemistry,2002,17(11):1 401-1 428.

[32] Simoneit B R T. Carbon isotope systematics of individual hydrocarbons in hydrothermal petroleum from Middle Valley,Northeastern Pacific Ocean[J]. Applied Geochemistry,2002,17(11):1 429-1 433.

[33] Ishibashi J,Sato M,Sano Y,et al. Helium and carbon gas geochemistry of pore fluids from the sediment-rich hydrothermal system in Escanaba Trough[J]. Applied Geochemistry,2002,17(11):1 457-1 466.

[34] Rushdi A I,Simoneit B R T. Hydrothermal alteration of organic matter in sediments of the Northeastern Pacific Ocean:Part 2.Escanaba Trough,Gorda Ridge[J]. Applied Geochemistry,2002,17(11):1 467-1 494.

[35] Zierenberg R A,Fouquet Y,Miller D J,et al. The deep structure of a sea-floor hydrothermal deposit [J]. Nature,1998,392:485-488. 

[36] Zierenberg R A,Miller D J. Overview of Ocean Drilling Program Leg 169: Sedimented Ridges II[A]. In: Zierenberg,R A,Fouquet Y,Miller D J,Normark W R,eds. Proceedings of the Ocean Drilling Program,Scientific Results[C]. 2000,169:1-39.

[37] Humphris S E,Herzig P M,Miller D J,et al. The internal structure of an active seafloor massive sulphide deposit[J]. Nature,1995,377:713-716.

[38] Hannington M,Galley A G,Herzig P M,et al. Comparison of the TAG mound and stockwork complex with Cyprus-type massive sulfide deposits[A]. In:Herzig P M,Humphris S E,Miller J,eds.Proceedings of the Ocean Drilling Program,Scientific Results [C].1998,158:389-415.

[39] Shipboard Scientific Party. Leg 193 summary[A].In:Binns R A,Barriga F J A S,Miller D J,et al, eds. Proceedings of the Ocean Drilling Program,Initial Reports [C].2002,193:1-84.

[40] Cowen J P,Giovannoni S J,Kenig Fabien,et al. Fluids from Aging Ocean Crust that support microbial life [J]. Science,2003,299:120-123.

[41] Furnes H,Staudigel H. Biological mediation in ocean crust alteration:How deep is the deep biosphere? [J]. Earth and Planetary Science Letters,1999,166(3/4):97-103.