A potential barrier to deep Antarctic circumpolar flow until the late Miocene?

Dalziel, I. W. D., Lawver, L. A., Pearce, J. A., Barker, P. F., Hastie, A. R., Barfod, D. N., Schenke, Hans-Werner and Davis, M. B. ;

Contact

Karsten.Gohl [ at ] awi.de

Abstract

Item Type

Article

Authors

Dalziel, I. W. D., Lawver, L. A., Pearce, J. A., Barker, P. F., Hastie, A. R., Barfod, D. N., Schenke, Hans-Werner and Davis, M. B. ;

Divisions

AWI Organizations > Geosciences > Geophysics

Primary Division

Organizations > AWI Organizations > Geosciences > Geophysics

Programs

Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.2: Earth system on tectonic time scales: From greenhouse to icehouse world

Primary Topic

Helmholtz Programs > Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.2: Earth system on tectonic time scales: From greenhouse to icehouse world

Publication Status

Published

Eprint ID

44599

DOI 10.1130/G34352.1

Cite as

Dalziel, I. W. D. , Lawver, L. A. , Pearce, J. A. , Barker, P. F. , Hastie, A. R. , Barfod, D. N. , Schenke, H. W. and Davis, M. B. (2013): A potential barrier to deep Antarctic circumpolar flow until the late Miocene? , Geology, 41 (9), pp. 947-950 . doi: 10.1130/G34352.1

Citation

Geographical region

Atlantic Ocean > South Atlantic Ocean > Southwest Atlantic Ocean (20w) > Scotia Sea

Research Platforms

N/A

Campaigns

N/A

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