Skip to main content
Log in

Change of the Composition of Solution During Its Migration Through the Sedimentary Cover in the Modern Hydrothermal System Center (Juan de Fuca Ridge, Pacific Ocean, ODP Hole 858B)

  • Published:
Lithology and Mineral Resources Aims and scope Submit manuscript

Abstract

The article presents the results of studying alteration of the hydrothermal solution composition during its percolation in the Pleistocene sediments drilled by ODP Hole 858B (38.6 m deep) in the northern segment of Middle Valley, Juan de Fuca Ridge (Dead Dog hydrothermal field), 20 m away from the hydrothermal source with a temperature 276°C. Influence of sediments in Units I, IIB, and IID from this hole on the solution composition variation during the solution–sediment interaction has been established. The greatest influence on the solution composition occurred during its interaction with sediments of Units IIB and IID under high-temperature conditions (200–350°C) expressed in enrichment of the solution with a large amount of chemical elements. A possible alteration in the solution composition is shown in the process of solution–sediment interaction during its percolation in the sedimentary cover 250–300 m thick.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1.
Fig. 2.
Fig. 3.
Fig. 4.
Fig. 5.

Similar content being viewed by others

REFERENCES

  1. Blinova, E.V. and Kurnosov, V.B., Hydrothermal alterations of sediments in the southern trough of the Guaymas Basin (Gulf of California) and transformation of the composition of solutions, Lith. Miner. Resour., 2015, no. 6, pp. 433–451.

  2. Bogdanov, Yu.A., Lisitsyn, A.P., Sagalevich, A.M., and Gurvich, E.G., Gidrotermal’nyi rudogenez okeanskogo dna (Hydrothermal Ore Genesis in the Ocean Floor), Moscow: Nauchn. Mir, 2006.

  3. Bogdanov, Yu.A. and Sagalevich, A.M., Geologicheskie issledovaniya s glubokovodnykh obitaemykh apparatov (Geological Studies with the Deep-Sea Manned Submersibles), Moscow: Nauchn. Mir, 2002.

  4. Buatier, M.D., Karpoff, A.M., Boni, M., et al., Mineralogical and petrographic records of sediment-fluid interaction in the sedimentary sequence at Middle Valley, Juan de Fuca Ridge, Leg 139, Proc. ODP, Sci. Res., 139, Mottl, M.J., Davis, E.E., Fisher, A.T., and Slack, J.F., Eds., College Station, 1994, pp. 133‒154.

  5. Butterfield, D.A., McDuff, R.A., Franrlin, J., and Wheat, C.G., Geochemistry of hydrothermal vent fluids from Middle Valley, Juan de Fuca Ridge, Proc. ODP, Sci. Res., 139, Mottl, M.J., Davis, E.E., Fisher, A.T., and Slack, J.F., Eds., College Station, 1994, pp. 395–410.

  6. Currey, J.R., Moore, D.G., Aguayo, J.E., et al., Init. Repts. DSDP, vol. 64, pt. 1, Washington, DC: U.S. Govt. Print. Off., 1982.

    Google Scholar 

  7. Davis, E.E., Mottl, M.J., Fisher, A.T., et al., Init. Repts. DSDP, 139, College Station, 1992.

  8. Davis, E.E. and Villinger, H., Tectonic and thermal structure of the Middle Valley sedimented rift, northern Juan de Fuca Ridge, Proc. ODP, Sci., 139, Mottl, M.J., Davis, E.E., Fisher, A.T., and Slack, J.F., Eds., College Station, 1994, pp. 9‒41.

  9. Frü-Green, G.L., McKenzie, J.A., Boni, M., et al., Stable isotope and geochemical record of convective hydrothermal circulation in the sedimentary sequence of Middle Valley, Juan de Fuca Ridge, Leg 139, Proc. ODP, Sci. Results, 139, Mottl, M.J., Davis, E.E., Fisher, A.T., and Slack, J.F., Eds., College Station, 1994, pp. 291‒306.

    Book  Google Scholar 

  10. Goodfellow, W.D. and Peter, J.M., Geochemistry of hydrothermally altered sediment, Middle Valley, northern Juan De Fuca Ridge, Proc. ODP, Sci. Res. 139, Mottl, M.J., Davis, E.E., Fisher, A.T., and Slack, J.F., Eds., College Station, 1994, pp. 207‒289.

  11. Gurvich, E.G., Metallonosnye osadki Mirovogo okeana (Metalliferous Sediments in the World Ocean), Moscow: Nauchn. Mir, 1998.

  12. Hajash, A. and Archer, P., Experimental seawater/basalt interaction: effects of cooling, Contrib. Mineral. Petrol., 1980, vol. 75, pp. 1–13.

    Article  CAS  Google Scholar 

  13. Kelts, K., Petrology of hydrothermally metamorphosed sediments at deep sea drilling Site 477, southern Guaymas Basin rift, Gulf of California, Init. Repts. DSDP, vol. 64, pt. 2, Washington: U.S. Govt. Print. Off., 1982, pp. 1123‒1136.

  14. Kristmanndottir, H., Types of clay minerals in hydrothermally altered basaltic rocks, Reykjanes, Iceland, Jökull, 1976, vol. 26, pp. 30–39.

    Article  Google Scholar 

  15. Kurnosov, V.B. and Blinova, E.V., Hydrothermal alteration of sediments and compositional evolution of solutions in the Guaymas Basin of the Gulf of California, Dokl. Earth Sci., 2015, vol. 461, no. 2, pp. 217–220.

    Article  CAS  Google Scholar 

  16. Kurnosov, V., Murdmaa, I., Rosanova, T., et al., Mineralogy of hydrothermally altered sediments and igneous rocks at Site 856-858, Middle Valley, Juan de Fuca Ridge, Leg 139, Proc. ODP, Sci. Res., 139, Mottl, M.J., Davis, E.E., Fisher, A.T., and Slack, J.F., Eds., College Station, 1994, pp. 113‒131.

  17. Leybourne, M.I. and Goodfellow, W.D., Mineralogy and mineral chemistry of hydrothermally altered sediment, Middle Valley, Juan de Fuca Ridge, Proc. ODP, Sci. Res. 139, Mottl, M.J., Davis, E.E., Fisher, A.T., and Slack, J.F., Eds., College Station, 1994, pp. 155‒206.

  18. Marakushev, A.A., Termodinamika metamorficheskoi gidratatsii mineralov (Thermodynamics of the Metamorphic Hydration of Minerals), Moscow: Nauka, 1968.

  19. Peter, J.M., Goodfellow, W.D., and Leybourne, M.I., Fluid inclusion petrography and microthermometry of the Middle Valley hydrothermal system, northern Juan de Fuca Ridge, Proc. ODP, Sci. Res.139, Mottl, M.J., Davis, E.E., Fisher, A.T., and Slack, J.F., Eds., College Station, 1994, pp. 411‒428.

  20. Rona, P.A. and Trivett, D.A., Discrete and diffuse heat transfer at ASHES vent field, Axial Volcano, Juan de Fuca Ridge, Earth Planet. Sci. Lett., 1992, vol. 109, no. 1, pp. 57–71.

    Article  CAS  Google Scholar 

  21. Sakharov, B.A. and Kurnosov, V.B., Peculiarities of clay mineral formation in sediments from the hydrothermal system center, Hole 858B, Juan de Fuca Ridge, Lith. Miner. Resour., 2022, no. 2, pp. 161–182.

  22. Seyfried, W.E. and Bischoff, J.L., Experimental seawater-basalt interaction at 300°C, 500 bars, chemical exchange, secondary mineral formation and implications for transport of heavy-metals, Geochim. Cosmochim. Acta, 1981, pp. 135–151.

  23. Von Damm, K.L., Edmond, J.M., Grant, B., et al., Chemistry of submarine hydrothermal solutions at 21° N, East Pacific Rise, Geochim. Cosmochim. Acta, 1985, vol. 49, no. 11, pp. 2197–2220.

    Article  CAS  Google Scholar 

Download references

ACKNOWLEDGMENTS

The authors express gratitude to G.N. Novikov who prepared rock samples for the chemical analyses.

Funding

In this study, we used rock samples from the ODP core storage, Texas A&M University, College Station.

The work was carried out under the state research plan, registration no. AAAAA 19-119020490093-6.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to V. B. Kurnosov.

Ethics declarations

The authors of this work declare that they have no conflicts of interest.

Additional information

Translated by D. Sakya

Publisher’s Note.

Pleiades Publishing remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Kurnosov, V.B., Konovalov, Y.I., Okina, O.I. et al. Change of the Composition of Solution During Its Migration Through the Sedimentary Cover in the Modern Hydrothermal System Center (Juan de Fuca Ridge, Pacific Ocean, ODP Hole 858B). Lithol Miner Resour 59, 136–150 (2024). https://doi.org/10.1134/S0024490223700475

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1134/S0024490223700475

Keywords:

Navigation