Strontium isotope constraints on fluid flow in the sheeted dike complex of fast spreading crust: Pervasive fluid flow at Pito Deep-Reference-Cited by-同舟云学术

Strontium isotope constraints on fluid flow in the sheeted dike complex of fast spreading crust: Pervasive fluid flow at Pito Deep

Published:2008-06 Issue:6 Volume:9 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Barker A. K.¹,Coogan L. A.¹,Gillis K. M.¹,Weis D.²

Affiliation:

1. School of Earth and Ocean Sciences; University of Victoria; P.O. Box 3055 STN CSC,; Victoria, British Columbia; V8W 3P6; Canada

2. Pacific Centre for Isotopic and Geochemical Research, Department of Earth and Ocean Sciences; University of British Columbia; 6339 Stores Road,; Vancouver, British Columbia; V6T 1Z4; Canada

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference63 articles.

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4. Stable and strontium isotopic profiles through hydrothermally altered upper oceanic crust, Hole 504B;Alt;Proc. Ocean Drill. Program Sci. Results,1996

5. Hydrothermal alteration of a section of upper oceanic crust in the eastern equatorial Pacific: A synthesis of results from DSDP/ODP Legs 69, 70, 83, 111, 137, 140, 148 at Site 504B;Alt;Proc. Ocean Drill. Program Sci. Results,1996

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