Geochemistry of fluid phases and sediments: relevance to hydrothermal circulation in Middle Valley, ODP Legs 139 and 169

Author:

Gieskes Joris M,Simoneit Bernd R.T,Shanks Wayne C,Goodfellow Wayne D,James Rachael H,Baker Paul A,Ishibashi Jun-ishiro

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference41 articles.

1. Mineralogy and Geochemistry of active and inactive chimneys and massive sulfides, Middle Valley, northern Juan de Fuca Ridge: an evolving hydrothermal system;Ames;Can. Mineral.,1993

2. Natural gas seepage in the Gulf of Mexico;Bernard;Earth Planet. Sci. Lett.,1976

3. Hydrogen isotope systematics of phase separation in submarine hydrothermal systems: experimental calibration and theoretical models;Berndt;Geochim. Cosmochim. Acta,1996

4. Hydrothermal chemistry of seawater from 25° to 350 °C;Bischoff;Am. J. Sci.,1978

5. Böhlke, J.K. Shanks, W.C. III, 1995. Stable isotope study of hydrothermal vents at Escanaba Trough, NE Pacific: observed and calculated effects of sediment-seawater interaction. In: Morton J.L., Zierenberg, R.A., Reiss, C.A.(Eds.), Geologic, Hydrothermal, and Biologic Studies at Escanaba Trough, Gorda Ridge, Offshore Northern California. Bull. 2022, US Geol. Surv. pp. 223–239.

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