Abstract
The general composition of the lithologic units at Site DSDP 613 varies only slightly from those at Site 612, but the style of decomposition is significantly different. Whereas evenbedded hemipelagic deposition prevailed most of the time at Site 612, the section at Site 613 is characterized by the frequent occurrence of slump deposits and conglomeratic, sandy, channel-fill deposits.- from Authors
Cite
CITATION STYLE
APA
Poag, C. W., & Watts, A. B. (1987). Site 613. Initial Reports DSDP, Leg 95, St. John’s to Ft. Lauderdale, 155–241. https://doi.org/10.2973/dsdp.proc.95.104.1987
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