Abstract
In the central southern Pacific, quartz accumulation reflects the changing position of the site with respect to the terrigenous source areas and the variations in wind systems through time.-from Authors
Cite
CITATION STYLE
APA
Schramm, C. T., & Leinen, M. S. (1987). Eolian transport to Hole 595A from the Late Cretaceous through the Cenozoic. Initial Reports DSDP, Leg 91, Wellington to Papeete, 469–473. https://doi.org/10.2973/dsdp.proc.91.113.1987
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