Abstract
The Cenozoic history of the abyssal circulation of the SW Atlantic is punctuated by tectonically or climatically controlled 'threshold' events, triggered by the changing geophysical boundary conditions associated with plate tectonic development of the basins.-from Author
Cite
CITATION STYLE
APA
Johnson, D. A. (1983). Paleocirculation of the southwestern Atlantic. Initial Reports DSDP, Leg 72, Santos, Brazil, 977–994. https://doi.org/10.2973/dsdp.proc.72.152.1983
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free