Transport and transformation of dissolved and particulate materials on continental margins influenced by major rivers: benthic boundary layer and seabed processes-Reference-Cited by-同舟云学术

Transport and transformation of dissolved and particulate materials on continental margins influenced by major rivers: benthic boundary layer and seabed processes

Published:2004-05 Issue:7-8 Volume:24 Page:899-926
ISSN:0278-4343
Container-title:Continental Shelf Research
language:en
Short-container-title:Continental Shelf Research

Author:

McKee B.A.,Aller R.C.,Allison M.A.,Bianchi T.S.,Kineke G.C.

Publisher

Elsevier BV

Subject

Geology,Aquatic Science,Oceanography

Reference197 articles.

1. Sediment accumulation in a modern epicontinental-shelf setting;Alexander;Marine Geology,1991

2. Carbonate dissolution in nearshore terrigenous muds—the role of physical and biological reworking;Aller;Journal of Geology,1982

3. Mobile deltaic and continental shelf muds as suboxic, fluidized bed reactors;Aller;Marine Chemistry,1998

4. Transport and reactions in the bioirrigated zone;Aller,2001

5. Sulfur diagenesis and burial on the Amazon shelf;Aller;Geo-Marine Letters,1996

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