V. Afanasyeva
ORCID:
0000-0001-6023-1570
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About
Contact & Profiles
Research Areas
- Methane Hydrates and Related Phenomena
- Geology and Paleoclimatology Research
- Paleontology and Stratigraphy of Fossils
- Seismic Imaging and Inversion Techniques
- Cryospheric studies and observations
- Hydrocarbon exploration and reservoir analysis
- Landslides and related hazards
All Russian Research Institute of Geology and Mineral Resources of the World Ocean
2020-2022
Johann Philipp Klages
Ulrich Salzmann
Torsten Bickert
Claus‐Dieter Hillenbrand
Karsten Gohl
and 35
more
Gerhard Kühn
Steven M. Bohaty
Jürgen Titschack
Juliane Müller
Thomas Frederichs
Thorsten Bauersachs
Werner Ehrmann
Tina van de Flierdt
Patric Simões Pereira
Robert D Larter
Gerrit Lohmann
Igor Niezgodzki
Gabriele Uenzelmann‐Neben
Maximilian Zundel
Cornelia Spiegel
Chris Mark
David Chew
Jane E. Francis
Gernot Nehrke
Florian Schwarz
James A Smith
Tim Freudenthal
Oliver Esper
Heiko Pälike
Thomas A. Ronge
Ricarda Dziadek
V. Afanasyeva
Jan Erik Arndt
Benjamin Ebermann
Catalina Gebhardt
Katharina Hochmuth
Kevin Küssner
Yani Najman
Florian Riefstahl
Mirko Scheinert
10.1038/s41586-020-2148-5
article
EN
Nature
2020-04-01
Gabriele Uenzelmann‐Neben
Karsten Gohl
Katharina Hochmuth
Ulrich Salzmann
Robert D Larter
and 25
more
Claus‐Dieter Hillenbrand
Johann Philipp Klages
V. Afanasyeva
Jan Erik Arndt
Torsten Bickert
Steven M. Bohaty
Ricarda Dziadek
Benjamin Ebermann
Werner Ehrmann
Oliver Esper
Thomas Frederichs
Tim Freudenthal
Catalina Gebhardt
Kevin Küssner
Gerhard Kühn
Yani Najman
Heiko Pälike
Florian Riefstahl
T.A. Ronge
Mirko Scheinert
Patric Simões Pereira
J. A. Smith
Cornelia Spiegel
Tina van de Flierdt
Maximilian Zundel
Abstract The stability of the West Antarctic Ice Sheet is threatened by incursion warm Circumpolar Deepwater which flows southwards via cross-shelf troughs towards coast there melting ice shelves. However, onset this oceanic forcing on development and evolution remains poorly understood. Here, we use single- multichannel seismic reflection profiles to investigate architecture a sediment body shelf Amundsen Sea Embayment. We estimate formation age be around Eocene-Oligocene Transition find...
10.1038/s43247-022-00369-x
article
EN
cc-by
Communications Earth & Environment
2022-02-21
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