Accretion, structure and hydrology of intermediate spreading-rate oceanic crust from drillhole experiments and seafloor observations

Author:

Pezard Philippe A.,Anderson Roger N.,Ryan William B. F.,Becker Keir,Alt Jeffrey C.,Gente Pascal

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Oceanography

Reference132 articles.

1. Adamides, N. G., 1987, Diverse Modes of Occurrence of Cyprus Sulfide Deposits and Comparison with Recent Analogues,Geol. Surv. Canada, paper 85-29, 153?168.

2. Alt, J. C., Laverne, C., and Muehlenbachs, K., 1985, Alteration of the Upper Oceanic Crust: Minerology and Processes in DSDP Hole 504B, Leg 83,Init. Repts. Deep Sea Drill. Proj. 83, 217?248.

3. Alt, J. C., Honnorez, J., Laverne, C., and Emmermann, R., 1986a, Hydrothermal Alteration of a 1-km Section through the Upper Oceanic Crust, DSDP Hole 504B: the Mineralogy, Chemistry and Evolution of Seawater-Basalt Interactions,J. Geophys. Res. 91, 309?335.

4. Alt, J. C., Muehlenbachs, K., and Honnorez, J., 1986b, An Oxygen Isotopic Profile through the Upper Kilometer of the Oceanic Crust, DSDP Hole 504B,Earth Planet. Sci. Lett. 80, 217?229.

5. Anderson, R. N., and Noltimier, H. C., 1973, A Model for the Horst and Graben Structure of Mid-Ocean Ridge Crests Based Upon Spreading Velocity and Basalt Delivery to the Oceanic Crust,Geophys. J.R. Astron. Soc. 34, 137?147.

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