Flow rate perturbations in a black smoker hydrothermal vent in response to a mid-ocean ridge earthquake swarm

Author:

Crone Timothy J.1,Wilcock William S. D.2,McDuff Russell E.2

Affiliation:

1. Lamont-Doherty Earth Observatory; Earth Institute at Columbia University; Palisades New York 10964 USA

2. School of Oceanography; University of Washington; Seattle Washington 98195-7940 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference51 articles.

1. Equation of state representation of phase equilibria and volumetric properties of the system NaCl-H2O above 573 K;Anderko;Geochim. Cosmochim. Acta,1993

2. Cataclysmic hydrothermal venting on the Juan de Fuca Ridge;Baker;Nature,1987

3. Large-scale electrical resistivity and bulk porosity of the oceanic crust, Deep Sea Drilling Project Hole 504B, Costa Rica Rift;Becker;Initial Rep. Deep Sea Drill. Proj.,1985

4. New evidence for age variation and scale effects of permeabilities of young oceanic crust from borehole thermal and pressure measurements;Becker;Earth Planet. Sci. Lett.,2003

5. A mechanism for sustained groundwater pressure changes induced by distant earthquakes;Brodsky;J. Geophys. Res.,2003

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