Spatial Variability of the Hydrochemical Structure in Bottom Gravity Current in the Vema Fracture Zone
The Vema Fracture Zone is located in the North Atlantic Ridge and extends along 11°N from 38 to 46°W. It is the main pathway for the spreading of Antarctic Bottom Water to the Northeast Atlantic. Due to its location and structure, the Vema Fracture Zone is an excellent object for studying the proper...
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| Hlavní autoři: | , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Russian Academy of Sciences, The Geophysical Center
2024-11-01
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| Edice: | Russian Journal of Earth Sciences |
| Témata: | |
| On-line přístup: | http://doi.org/10.2205/2024ES000945 |
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