McGee, D. et al. (2006): (super 232) Th-derived dust fluxes as a marker of deglacial changes in ITCZ position and intensity in the eastern Equatorial Pacific

Leg/Site/Hole:
Identifier:
2008-125247
georefid

10.1016/j.gca.2006.06.827
doi

Creator:
McGee, D.
Tulane University, Department of Earth and Environmental Sciences, New Orleans, LA, United States
author

Marcantonio, F.
Georgia Institute of Technology, United States
author

Lynch-Stieglitz, J.
author

Identification:
(super 232) Th-derived dust fluxes as a marker of deglacial changes in ITCZ position and intensity in the eastern Equatorial Pacific
2006
In: Anonymous, Abstracts of the 16th annual V. M. Goldschmidt conference
Coverage:Geographic coordinates:
North:7.0000
West:-110.0000East: -110.0000
South:-3.0000

Quaternary geology; Isotope geochemistry; actinides; atmospheric transport; Cenozoic; clastic sediments; clay mineralogy; climate change; cores; deglaciation; dust; East Pacific; Equatorial Pacific; geochemical indicators; geochemistry; Intertropical Convergence Zone; isotopes; last glacial maximum; marine sediments; metals; Ocean Drilling Program; Pacific Ocean; paleo-oceanography; paleoclimatology; provenance; Quaternary; radioactive isotopes; sediment transport; sedimentation; sediments; Th-232; thorium; wind transport; winds;

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