How, When and Where Do Ocean Currents Control Sedimentation in Deep-Water Environments?
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Overview
Syllabus
Introduction
deep sea
countries
rifts
detached drifts
controlled terraces
eroded surfaces
distribution of currents
early studies
Argentina margins
Vessel mounted adcp measurements
Average speed from reanalysis
Summary
When arechondrites forming
Types of currents
Model outputs
Seasonality
High variability
Interpretation
Southern Greenland
Argentina
Anticyclone
Positive feedback
Takehome message
Currents
Thank you
Very much
Questions
Induced by currents
How easy is it to determine paleocurrent directions
How can we constrain sediment supply
Inversion of bottom currents
Drift locations
Mineralogical analysis
Taught by
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