Unusually low234Th in a hydrothermal effluent plume over the Southwest Indian Ridge
Author:
Affiliation:
1. State Key Laboratory of Marine Environmental Science and College of Ocean and Earth Sciences; Xiamen University; Xiamen China
2. North China Sea Environmental Monitoring Center; State Oceanic Administration; Qingdao China
Funder
the COMRA Program
NSFC
State Oceanic Administration programs
Fundamental Research Funds for the Central Universities of China
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016GC006580/fullpdf
Reference62 articles.
1. Discovery of ancient and active hydrothermal systems along the ultra-slow spreading Southwest Indian Ridge 10°-16°E;Bach;Geochem. Geophys. Geosyst.,2002
2. Removal of 234Th in the bottom nepheloid layer of the ocean;Bacon;Earth Planet. Sci. Lett.,1989
3. 210Pb/226Ra and 210Po/210Pb disequilibria in seawater and suspended particulate matter;Bacon;Earth Planet. Sci. Lett.,1976
4. Testing a new small-volume technique for determining 234Th in seawater;Benitez-Nelson;J. Radioanal. Nucl. Chem.,2001a
5. A time-series study of particulate matter export in the North Pacific Subtropical Gyre based on 234Th:238U disequilibrium;Benitez-Nelson;Deep Sea Res., Part I,2001b
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