Linking basement carbonate vein compositions to porewater geochemistry across the eastern flank of the Juan de Fuca Ridge, ODP Leg 168-Reference-Cited by-同舟云学术

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Linking basement carbonate vein compositions to porewater geochemistry across the eastern flank of the Juan de Fuca Ridge, ODP Leg 168

Published:2004-02 Issue:1-2 Volume:219 Page:111-128
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Coggon Rosalind M,Teagle Damon A.H,Cooper Matthew J,Vanko David A

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference48 articles.

1. Constraints on hydrothermal heat-flux through the oceanic lithosphere from global heat-flow;Stein;J. Geophys. Res.,1994

2. The heat flow through oceanic and continental crust and the heat loss of the earth;Sclater;Rev. Geophys. Space Phys.,1980

3. Mid-ocean ridge hydrothermal fluxes and the chemical composition of the ocean;Elderfield;Annu. Rev. Earth Planet. Sci.,1996

4. Hydrothermal circulation through mid-ocean ridge flanks – fluxes of heat and magnesium;Mottl;Geochim. Cosmochim. Acta,1994

5. Compositions of pore and spring waters from Baby Bare: Global implications of geochemical fluxes from a ridge flank hydrothermal system;Wheat;Geochim. Cosmochim. Acta,2000

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