Abstract
Indicates that original global sediment flux rates varied cyclically by a factor of up to three. This implies significant changes in the rates of uplift and mountain buliding and global plate tectonic activity. -from Authors
Cite
CITATION STYLE
APA
Wold, C. N., & Hay, W. W. (1990). Estimating ancient sediment fluxes. American Journal of Sciences, 290(9), 1069–1089. https://doi.org/10.2475/ajs.290.9.1069
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