Dissolved and particulate 230Th–232Th in the Central Equatorial Pacific Ocean: Evidence for far-field transport of the East Pacific Rise hydrothermal plume

Author:

Lopez Grecia I.,Marcantonio Franco,Lyle Mitch,Lynch-Stieglitz Jean

Funder

NSF

Publisher

Elsevier BV

Subject

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

Reference50 articles.

1. Removal of 230Th and 231Pa at ocean margins;Anderson;Earth Planet. Sci. Lett.,1983

2. GEOTRACES intercalibration of 230Th, 232Th, 231Pa, and prospects for 10Be;Anderson;Limnol. Oceanogr., Methods,2012

3. Glacial to interglacial changes in carbonate and clay sedimentation in the Atlantic Ocean estimated from 230Th measurements;Bacon;Chem. Geol.,1984

4. Distribution of thorium isotopes between dissolved and particulate forms in the deep sea;Bacon;J. Geophys. Res.,1982

5. Hydrothermal iron in the deep western South Pacific;Boyle;Geochim. Cosmochim. Acta, Suppl.,2008

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