The Origin of Carbonate Veins Within the Sedimentary Cover and Igneous Rocks of the Cocos Ridge: Results From IODP Hole U1414A-Reference-Cited by-同舟云学术

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The Origin of Carbonate Veins Within the Sedimentary Cover and Igneous Rocks of the Cocos Ridge: Results From IODP Hole U1414A

Published:2018-10 Issue:10 Volume:19 Page:3721-3738
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Brandstätter Jennifer¹^ORCID,Kurz Walter¹^ORCID,Richoz Sylvain¹²^ORCID,Cooper Matthew J.³^ORCID,Teagle Damon A. H.³^ORCID

Affiliation:

1. Institute of Earth Sciences, NAWI Graz Geocenter; University of Graz; Graz Austria

2. Department of Geology; Lund University; Lund Sweden

3. Ocean and Earth Science, National Oceanography Centre Southampton; University of Southampton; Southampton England, UK

Funder

Austrian Science Fund

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018GC007729/fullpdf

Reference83 articles.

1. Trace-element behavior and redox facies in core shales of Upper Pennsylvanian Kansas-type cyclothems;Algeo;Chemical Geology,2004

2. Geophysical Monograph Series;Alt,1995

3. The uptake of carbon during alteration of ocean crust;Alt;Geochimica et Cosmochimica Acta,1999

4. Hydrothermal alteration of upper oceanic crust formed at a fast-spreading ridge: Mineral, chemical, and isotopic evidence from ODP Site 801;Alt;Chemical Geology,2003

5. Carbonate veins trace seawater circulation during exhumation and uplift of mantle rock: Results from ODP Leg 209;Bach;Earth and Planetary Science Letters,2011

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