Shelf-edge delta overreach at the shelf break can guarantee the delivery of terrestrial sediments to deep water at all sea-level stands

How and when sediment moves from terrestrial sources to deep-water sinks is a significant area of research. We have used an array of seismic, borehole, and gravity core datasets to explore the timing and magnitude of sediment-routing to Pearl River slope over the last 478 k.y.

Please log in to read the full article

You may also be interested in ...