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They can be added by deep-sea sediments, igneous rocks, river sediments, and terranes.
Continental rock is MUCH older than sediments in the sea (unless the sediments in the sea come from continental crust, in which case they would be the same age).
Probably consolidated sediments (sedimentary rock), then the rock basalt.
Biogenous.
how do deep sea bacteria survive
The deep sea.
Deep-sea sediments most likely contribute to continent growth by being scraped off in a subduction zone and left at the surface.
Roberto Danovaro has written: 'Methods for the study of deep-sea sediments, their functioning and biodiversity' -- subject(s): Marine biology, Marine sediments, Benthic animals, Methodology, Benthos, Research 'Methods for the study of deep-sea sediments--their functioning and biodiversity' 'Methods for the study of deep-sea sediments--their functioning and biodiversity' -- subject(s): Marine biology, Marine sediments, Benthic animals, Methodology, Benthos, Research
Due to long shore currents the suspended particles transported as a suspended load to the deep sea.
They can be added by deep-sea sediments, igneous rocks, river sediments, and terranes.
Sture Landergren has written: 'On the geochemistry of deep-sea sediments'
A deep sea plain, sometimes called an abyssal plain is a wide, almost level area that covers about two-thirds of the entire ocean floor. There is a complete absence of river sediments on this plain.
scraped off in a subduction zone and left at the surface
Patricia Paluso has written: 'A guide to publications and subsequent investigations of Deep Sea Drilling Project materials' -- subject(s): Bibliography, Deep Sea Drilling Project, Marine sediments, Paleontology
To investigate the evolution of ocean basins by core drilling of ocean sediments and underlying oceanic crust.
Tsung-hung Peng has written: 'The impacts of bioturbation on the age difference between benthic and planktonic foraminifera in deep sea sediments' -- subject(s): Foraminifera, Marine sediments
V. I. Baranov has written: 'Radiochemical analysis of deep-sea sediments in connection with the determination of the rate of sediment accumulation'