(Table 2) Sedimentation and accumulation rates of DSDP Holes 38-337 and 38-338
The modern depositional environment of the deep Norwegian-Greenland Sea is highly asymmetric in an E–W direction because of the hydrography of the surface water masses and because of the more or less permanent pack ice cover of the East Greenland Current regime along the Greenland continental margin...
Main Authors: | , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1986
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.761096 https://doi.org/10.1594/PANGAEA.761096 |