Potential and limitation of 230Th-excess as a chronostratigraphic tool for late Quaternary Arctic Ocean sediment studies: An example from the Southern Lomonosov Ridge

Author:

Purcell Karl,Hillaire-Marcel Claude,de Vernal Anne,Ghaleb Bassam,Stein Ruediger

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference98 articles.

1. Constraining the age of the last interglacial-glacial transition in the Hudson Bay lowlands (Canada) using U-Th dating of buried wood;Allard;Quat. Geochronol.,2012

2. Removal of 230Th and 231pa from the open ocean;Anderson;Earth Planet. Sci. Lett.,1983

3. Is the Central Arctic Ocean a sediment starved basin?;Backman;Quat. Sci. Rev.,2004

4. Scavenging of thorium isotopes by colloids in seawater of the Gulf of Mexico;Baskaran;Geochim. Cosmochim. Acta,1992

5. Reconstruction of Sea-Ice Drift and Terrigenous Sediment Supply in the Late Quaternary: Heavy-mineral Associations in Sediments of the Laptev-Sea Continental Margin and the Central Arctic Ocean;Behrends,1999

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