hdl:10013/epic.37856
Does the seafloor morphology of the southern Mozambique Channel provide evidence for persistent bottom-current flow and deep-reaching eddy activity?
Breitzke, Monika, Jokat, Wilfried 
ORCID: https://orcid.org/0000-0002-7793-5854, Krocker, Ralf and Watkeys, M.
;
ORCID: https://orcid.org/0000-0002-7793-5854, Krocker, Ralf and Watkeys, M.
;
Contact
Monika.Breitzke [ at ] awi.de
Abstract
Item Type
Conference
(Poster)
Authors
Breitzke, Monika, Jokat, Wilfried ORCID: https://orcid.org/0000-0002-7793-5854, Krocker, Ralf and Watkeys, M.
;
ORCID: https://orcid.org/0000-0002-7793-5854, Krocker, Ralf and Watkeys, M.
;
Divisions
Programs
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past > WP 3.2: Tectonic, Climate and Biosphere Development from Greenhouse to Icehouse
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past > WP 3.2: Tectonic, Climate and Biosphere Development from Greenhouse to Icehouse
Publication Status
Published
Event Details
AGU Fall Meeting, 5-9 December, San Francisco, CA, USA..
Eprint ID
24723
Cite as
Breitzke, M.
,
Jokat, W.
,
Krocker, R.
and
Watkeys, M.
(2011):
Does the seafloor morphology of the southern Mozambique Channel provide evidence for persistent bottom-current flow and deep-reaching eddy activity?
,
AGU Fall Meeting, 5-9 December, San Francisco, CA, USA.
.
Share
Research Platforms
Campaigns
N/A
Actions
Edit Item
