SEARCH

SEARCH BY CITATION

References

  • Anderson, R., and M. Hobart (1976), The relation between heat flow, sediment thickness, and age in the Eastern Pacific, J. Geophys. Res., 81, 29682989.
  • Becker, K., and E. Davis (2003), New evidence for age variation and scale effects of permeabilities of young oceanic crust from borehole thermal and pressure measurements, Earth. Planet. Sci. Lett., 210, 499508.
  • Becker, K., and E. Davis (2004), In situ determinations of the permeability of the igneous oceanic crust, in Hydrogeology of the Oceanic Lithosphere, edited by E. E. Davis, and H. Elderfield, pp. 189224, Cambridge Univ. Press, New York.
  • Becker, K., and A. Fisher (2000), Permeability of upper oceanic basement on the eastern flank of the Endeavor Ridge determined with drill-string packer experiments, J. Geophys. Res., 105(B1), 897912.
  • Becker, N. C., C. G. Wheat, M. J. Mottl, J. Karsten, and E. E. Davis (2000), A geological and geophysical investigation of Baby Bare, locus of a ridge flank hydrothermal system in the Cascadia Basin, J. Geophys. Res., 105(B10), 23,55723,568.
  • Currie, R. G., D. S. Seemann, and R. Riddihough (1982), Total magnetic field anomaly, offshore British Columbia, Geol. Surv. of Can., Sydney, British Columbia, Canada.
  • Davis, E. E., and K. Becker (2002), Observations of natural-state fluid pressures and temperatures in young oceanic crust and inferences regarding hydrothermal circulation, Earth. Planet. Sci. Lett., 204, 231248.
  • Davis, E. E., and K. Becker (2004), Observations of temperature and pressure: Constraints on ocean crustal hydrologic state, properties, and flow, in Hydrogeology of the Oceanic Lithosphere, edited by E. E. Davis, and H. Elderfield, pp. 225271, Cambridge Univ. Press, New York.
  • Davis, E. E., and R. G. Currie (1993), Geophysical observations of the northern Juan de Fuca Ridge system: Lessons in seafloor spreading, Can. J. Earth Sci., 30, 278300.
  • Davis, E. E., and C. R. B. Lister (1977), Heat flow measured over the Juan de Fuca Ridge: Evidence for widespread hydrothermal circulation in a highly heat-transportive crust, J. Geophys. Res., 82, 48454860.
  • Davis, E. E., D. S. Chapman, C. Forster, and H. Villinger (1989), Heat-flow variations correlated with buried basement topography on the Juan de Fuca Ridge flank, Nature, 342, 533537.
  • Davis, E. E., et al. (1992), FlankFlux: An experiment to study the nature of hydrothermal circulation in young oceanic crust, Can. J. Earth Sci., 29(5), 925952.
  • Davis, E. E., D. S. Chapman, H. Villinger, S. Robinson, J. Grigel, A. Rosenberger, and D. Pribnow (1997a), Seafloor heat flow on the eastern flank of the Juan de Fuca Ridge: Data from the “FlankFlux” studies through 1995, Proc. Ocean Drill. Program Initial Rep., 168, 2333.
  • Davis, E. E., A. T. Fisher, and J. Firth (1997b), Proceedings of the Ocean Drilling Program, Initial Reports, vol. 168, 470 pp., Ocean Drill. Program, College Station, Tex.
  • Davis, E. E., K. Wang, J. He, D. S. Chapman, H. Villinger, and A. Rosenberger (1997c), An unequivocal case for high Nusselt-number hydrothermal convection in sediment-buried igneous oceanic crust, Earth. Planet. Sci. Lett., 146, 137150.
  • Davis, E. E., D. S. Chapman, K. Wang, H. Villinger, A. T. Fisher, S. W. Robinson, J. Grigel, D. Pribnow, J. Stein, and K. Becker (1999), Regional heat-flow variations across the sedimented Juan de Fuca Ridge eastern flank: Constraints on lithospheric cooling and lateral hydrothermal heat transport, J. Geophys. Res., 104(B8), 17,67517,688.
  • Davis, E. E., K. Wang, K. Becker, and R. E. Thomson (2000), Formation-scale hydraulic and mechanical properties of oceanic crust inferred from pore-pressure response to periodic seafloor loading, J. Geophys. Res., 105(B6), 13,42313,435.
  • Elderfield, H., C. G. Wheat, M. J. Mottl, C. Monnin, and B. Spiro (1999), Fluid and geochemical transport through oceanic crust: A transect across the eastern flank of the Juan de Fuca Ridge, Earth. Planet. Sci. Lett., 172, 151165.
  • Fisher, A. (2004), Rates and patterns of fluid circulation, in Hydrogeology of the Oceanic Lithosphere, edited by E. E. Davis, and H. Elderfield, pp. 339377, Cambridge Univ. Press, New York.
  • Fisher, A. T. (1998), Permeability within basaltic oceanic crust, Rev. Geophys., 36(2), 143182.
  • Fisher, A. T. (2005), Marine hydrogeology: Future prospects for major advances, Hydrol. J., 13, 6997, doi:10.1007/s10040-004-0400-y.
  • Fisher, A. T., and K. Becker (2000), Channelized fluid flow in oceanic crust reconciles heat-flow and permeability data, Nature, 403, 7174.
  • Fisher, A. T., K. Becker, and E. E. Davis (1997), The permeability of young oceanic crust east of Juan de Fuca Ridge determined using borehole thermal measurements, Geophys. Res. Lett., 24, 13111314.
  • Fisher, A. T., E. E. Davis, and C. Escutia (2000), Proceedings of the Ocean Drilling Program, Science Results, vol. 168, 185 pp., Ocean Drill. Program, College Station, Tex.
  • Fisher, A. T., et al. (2003a), Hydrothermal recharge and discharge across 50 km guided by seamounts on a young ridge flank, Nature, 421, 618621.
  • Fisher, A. T., C. A. Stein, R. N. Harris, K. Wang, E. A. Silver, M. Pfender, M. Hutnak, A. Cherkaoui, R. Bodzin, and H. Villinger (2003b), Abrupt thermal transition reveals hydrothermal boundary and role of seamounts within the Cocos Plate, Geophys. Res. Lett., 30(11), 1550, doi:10.1029/2002GL016766.
  • Fisher, A. T., and R. P. Von Herzen (2005), Models of hydrothermal circulation within 106 Ma seafloor: Constraints on the vigor of fluid circulation and crustal properties, below the Madeira Abyssal Plain, Geochem. Geophys. Geosyst., 6, Q11001, doi:10.1029/2005GC001013.
  • Fisher, A. T., T. Urabe, and A. Klaus (2005a), Proceedings of the IODP: Expedition Reports, vol. 301, Integrated Ocean Drill. Program, College Station, Tex.
  • Fisher, A. T., et al. (2005b), Scientific and technical design and deployment of long-term, subseafloor observatories for hydrogeologic and related experiments, IODP Expedition 301, eastern flank of Juan de Fuca Ridge, in Proceedings of the IODP, vol. 301, edited by A. T. Fisher, T. Urabe, and A. Klaus, Integrated Ocean Drill. Program, College Station, Tex.
  • Giambalvo, E., A. T. Fisher, L. Darty, J. T. Martin, and R. P. Lowell (2000), Origin of elevated sediment permeability in a hydrothermal seepage zone, eastern flank of Juan de Fuca Ridge, and implications for transport of fluid and heat, J. Geophys. Res., 105(B1), 913928.
  • Harris, R. N., A. T. Fisher, and D. Chapman (2004), Fluid flow through seamounts and implications for global mass fluxes, Geology, 32(8), 725728, doi:10.1130/G20387.1.
  • Jacobson, R. S. (1992), Impact of crustal evolution on changes of the seismic properties of the uppermost oceanic crust, Rev. Geophys., 30, 2342.
  • Johnson, H. P., K. Becker, and R. P. V. Herzen (1993), Near-axis heat flow measurements on the northern Juan de Fuca Ridge: Implications for fluid circulation in oceanic crust, Geophys. Res. Lett., 20(17), 18751878.
  • Kappel, E. S., and W. B. F. Ryan (1986), Volcanic episodicity and a non-steady state rift valley along the northeast pacific spreading centers: Evidence from sea marc I, J. Geophys. Res., 91(B14), 13,92513,940.
  • Karsten, J., N. C. Becker, M. J. Mottl, and C. G. Wheat (1998), Petrology of Baby Bare and Mama Bare lavas, Geophys. Res. Lett., 25(1), 117120.
  • Karsten, J. L., S. R. Hammond, E. E. Davis, and R. G. Currie (1986), Detailed geomorphology and neotectonics of the Endeavour segment, Juan de Fuca Ridge: New results from Seabeam swath mapping, Geol. Soc. Am. Bull., 97, 213221.
  • Langseth, M. G., and B. Herman (1981), Heat transfer in the oceanic crust of the Brazil Basin, J. Geophys. Res., 86, 10,80510,819.
  • Langseth, M. G., R. D. Hyndman, K. Becker, S. H. Hickman, and M. H. Salisbury (1984), The hydrogeological regime of isolated sediment ponds in mid-oceanic ridges, Initial Rep. Deep Sea Drill. Proj., 78B, 825837.
  • Lister, C. R. B. (1970), Heat flow of the Juan de Fuca Ridge, J. Geophys. Res., 75, 26482654.
  • Lister, C. R. B. (1977), Qualitative models of spreading center processes, including hydrothermal penetration, Tectonophysics, 37, 203218.
  • Marescotti, P., D. A. Vanko, and R. Cabella (2000), From oxidizing to reducing alteration: Mineralogical variations in pillow basalts from the east flank, Juan de Fuca Ridge, Proc. Ocean Drill. Program Sci. Results, 168, 119136.
  • Mottl, M. J., and C. G. Wheat (1994), Hydrothermal circulation through mid-ocean ridge flanks: Fluxes of heat and magnesium, Geochim. Cosmochim. Acta, 58, 22252237.
  • Mottl, M. J., et al. (1998), Warm springs discovered on 3.5 Ma oceanic crust, eastern flank of the Juan de Fuca Ridge, Geology, 26, 5154.
  • Parsons, B., and J. G. Sclater (1977), An analysis of the variation of ocean floor bathymetry and heat flow with age, J. Geophys. Res., 82, 803829.
  • Press, W. H., B. P. Flannery, S. A. Teukolsky, and W. T. Vetterling (1989), Numerical Recipes: The Art of Scientific Computing, 702 pp., Cambridge Univ. Press, New York.
  • Pribnow, D. F. C., E. E. Davis, and A. T. Fisher (2000), Borehole heat flow along the eastern flank of the Juan de Fuca Ridge, including effects of anisotropy and temperature dependence of sediment thermal conductivity, J. Geophys. Res., 105(B6), 13,44913,456.
  • Rosenberg, N., A. T. Fisher, and J. Stein (2000), Large-scale lateral heat and fluid transport in the seafloor: Revisiting the well-mixed aquifer model, Earth. Planet. Sci. Lett., 182, 93101.
  • Rosenberger, A., E. E. Davis, and H. Villinger (2000), Data report: Hydrocell-95 and -96 single-channel seismic data on the eastern Juan de Fuca Ridge flank, Proc. Ocean Drill. Program, Sci. Results, 168, 919.
  • Shipboard Scientific Party (1997a), Buried Basement Transect (Sites 1028, 1029, 1030, 1031, and 1032), Proc. Ocean Drill. Program Initial Rep., 168, 161214.
  • Shipboard Scientific Party (1997b), Scientific Party, Hydrothermal Transition Transect (Sites 1023, 1024, and 1025), Proc. Ocean Drill. Program Initial Rep., 168, 49100.
  • Shipboard Scientific Party (1997c), Introduction and summary: Hydrothermal circulation in the oceanic crust and its consequences on the eastern flank of the Juan de Fuca Ridge, Proc. Ocean Drill. Program Initial Rep., 168, 721.
  • Shipboard Scientific Party (1997d), Rough Basement Transect (Sites 1026 and 1027), Proc. Ocean Drill. Program Initial Rep., 168, 101160.
  • Siegel, S. (1956), Nonparametric Statistics for the Behavioral Sciences, 279 pp., McGraw-Hill, New York.
  • Smith, W. H. F., and D. T. Sandwell (1997), Global sea floor topography from satellite altymetry and ship depth soundings, Science, 277, 19561962.
  • Spinelli, G. A., and A. T. Fisher (2004), Hydrothermal circulation within topographically rough basaltic basement on the Juan de Fuca Ridge flank, Geochem. Geophys. Geosyst., 5, Q02001, doi:10.1029/2003GC000616.
  • Spinelli, G. A., E. G. Giambalvo, and A. T. Fisher (2004a), Hydrologic properties and distribution of sediments, in Hydrogeology of the Oceanic Lithosphere, edited by E. E. Davis, and H. Elderfield, pp. 151188, Cambridge Univ. Press, New York.
  • Spinelli, G. A., L. Zühlsdorff, A. T. Fisher, C. G. Wheat, M. Mottl, V. Spieß, and E. R. Giambalvo (2004b), Hydrothermal seepage patterns above a buried basement ridge, eastern flank of the Juan de Fuca Ridge, J. Geophys. Res., 109, B01102, doi:10.1029/2003JB002476.
  • Stein, C., and S. Stein (1992), A model for the global variation in oceanic depth and heat flow with lithospheric age, Nature, 359, 123129.
  • Stein, J. S., and A. T. Fisher (2001a), Lateral hydrothermal circulation beneath the eastern flank of the Juan de Fuca Ridge: Thermal, chemical and modeling constraints, Eos Trans AGU, 82(47), Fall Meet. Suppl., Abstract S21A-0560.
  • Stein, J. S., and A. T. Fisher (2001b), Multiple scales of hydrothermal circulation in Middle Valley, northern Juan de Fuca Ridge: Physical constraints and geologic models, J. Geophys. Res., 106(B5), 85638580.
  • Stein, J. S., and A. T. Fisher (2003), Observations and models of lateral hydrothermal circulation on a young ridge flank: Numerical evaluation of thermal and chemical constraints, Geochem. Geophys. Geosyst., 4(3), 1026, doi:10.1029/2002GC000415.
  • Thomson, R. E., E. Davis, and B. J. Burd (1995), Hydrothermal venting and geothermal heating in Cascadia Basin, J. Geophys. Res., 100, 61216141.
  • Underwood, M., K. D. Hoke, A. T. Fisher, E. G. Giambalvo, E. E. Davis, and L. Zühlsdorff (2005), Provenance, stratigraphic architecture, and hydrogeologic effects of turbidites in northwestern Cascadia Basin, Pacific Oceanz, J. Sediment. Res., 75(1), 149164.
  • Villinger, H., I. Grevemeyer, N. Kaul, J. Hauschild, and M. Pfender (2002), Hydrothermal heat flux through aged oceanic crust: Where does the heat escape? Earth. Planet. Sci. Lett., 202(1), 159170.
  • Von Herzen, R. P. (2004), Geothermal evidence for continuing hydrothermal circulation in older (>60 Ma) ocean crust, in Hydrogeology of the Oceanic Lithosphere, edited by E. E. Davis, and H. Elderfield, pp. 414450, Cambridge Univ. Press, New York.
  • Wheat, C. G., and M. J. Mottl (1994), Hydrothermal circulation, Juan de Fuca Ridge eastern flank: Factors controlling basement water composition, J. Geophys. Res., 99, 30673080.
  • Wheat, C. G., H. Elderfield, M. J. Mottl, and C. Monnin (2000), Chemical composition of basement fluids within an oceanic ridge flank: Implications for along-strike and across-strike hydrothermal circulation, J. Geophys. Res., 105(B6), 13,43713,447.
  • Wheat, C. G., M. J. Mottl, A. T. Fisher, D. Kadko, E. E. Davis, and E. Baker (2004), Heat flow through a basaltic outcrop on a sedimented young ridge flank, Geochem. Geophys. Geosyst., 5, Q12006, doi:10.1029/2004GC000700.
  • Williams, D. L., K. Green, T. H. van Andel, R. P. Von Herzen, J. R. Dymond, and K. Crane (1979), The hydrothermal mounds of the Galapagos Rift: Observations with DSRV Alvin and detailed heat flow studies, J. Geophys. Res., 84, 74677484.
  • Wilson, D. S. (1993), Confidence intervals for motion and deformation of the Juan de Fuca plate, J. Geophys. Res., 98(B16), 16,05316,071.
  • Zühlsdorff, L., M. Hutnak, A. Fisher, V. Speiss, E. Davis, M. Nedimovic, S. Carbotte, H. Villinger, and K. Becker (2005), Site surveys related to IODP Expedition 301: ImageFlux (SO149) and RetroFlux (TN116) expeditions and earlier studies, Proc. Ocean Drill. Program Sci., 301.
  • Zyvoloski, G. A., B. A. Robinson, Z. D. Dash, and L. L. Trease (1996), Users manual for the FEHMN application, Los Alamos Natl. Lab., Los Alamos, N. M.