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How easy is it to determine paleocurrent directions
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How, When and Where Do Ocean Currents Control Sedimentation in Deep-Water Environments?
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- 1 Introduction
- 2 deep sea
- 3 countries
- 4 rifts
- 5 detached drifts
- 6 controlled terraces
- 7 eroded surfaces
- 8 distribution of currents
- 9 early studies
- 10 Argentina margins
- 11 Vessel mounted adcp measurements
- 12 Average speed from reanalysis
- 13 Summary
- 14 When arechondrites forming
- 15 Types of currents
- 16 Model outputs
- 17 Seasonality
- 18 High variability
- 19 Interpretation
- 20 Southern Greenland
- 21 Argentina
- 22 Anticyclone
- 23 Positive feedback
- 24 Takehome message
- 25 Currents
- 26 Thank you
- 27 Very much
- 28 Questions
- 29 Induced by currents
- 30 How easy is it to determine paleocurrent directions
- 31 How can we constrain sediment supply
- 32 Inversion of bottom currents
- 33 Drift locations
- 34 Mineralogical analysis