Abstract
The 7 lithologic units pernetrated are, from bottom to top,: limestone and chalk (U.Berriasian-Barremian), green-gray and black claytone (Barremian to Cenomanian), multicolored claystones (?Turonian-Maestrichtan), marly chalk (U.Maestrichtian) siliceous turbidites, siliceous claystones and chert (L.Paleocene-M.Eocene), radiolarian mud (M.Eocene-U.Oligocene), and hemipelagic clay (?Miocene-Quaternary). Sediment accumulation at Site 387 appears to have been nearly continuous, except for a possible hiatus or extremely low accumulation rate within the U.Cretaceous multi-colored claystones. -from Authors
Cite
CITATION STYLE
Tucholke, B. E. (1979). ( DSDP) Site 387: Cretaceous to Recent sedimentary evolution of the western Bermuda Rise. Initial Reports of the Deep Sea Drilling Project, Leg 43, Istanbul, Turkey to Norfolk, Virginia, 1975, (Scripps Institution of Oceanography; UK Distributors IPOD Committee, NERC, Swindon), 323–292. https://doi.org/10.2973/dsdp.proc.43.107.1979
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
