Impact of depositional and biogeochemical processes on small scale variations in nodule abundance in the Clarion‐Clipperton Fracture Zone

Author:

Mewes K.,Mogollón J.M.,Picard A.,Rühlemann C.,Kuhn T.,Nöthen K.,Kasten S.

Funder

University of Southern California

AWI

Irene Bitz (BGR)

RV SONNE

Bundesministerium für Bildung und Forschung

DFG Research Center/Cluster of Excellence “The Ocean in the Earth System” (MARUM)

Max Planck Society

Helmholtz Association.

Publisher

Elsevier BV

Subject

Aquatic Science,Oceanography

Reference107 articles.

1. The neodymium isotopic composition of manganese nodules from the Southern and Indian Oceans, the global oceanic neodymium budget, and their bearing on deep ocean circulation;Albarede;Geochim. Cosmochim. Acta,1997

2. Environmental aspects of manganese nodule mining;Amos;Mar. Policy,1977

3. The Hawaii-Tahiti transect: the oceanographic environment of manganese nodule deposits in the Central Pacific;Andrews;Mar. Geol.,1983

4. Seafloor spreading anomalies and crustal ages of the Clarion–Clipperton Zone;Barckhausen;Mar. Geophys. Res.,2013

5. The behaviour of deep-sea sediments under the impact of nodule mining processes;Becker;Deep-sea Res. Part II – Top. Stud. Oceanogr.,2001

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