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...

Full description

Saved in:
Bibliographic Details
Main Authors: Zuev Oleg, Seliverstova Anna M.
Format: Article
Language:English
Published: Russian Academy of Sciences, The Geophysical Center 2024-11-01
Series:Russian Journal of Earth Sciences
Subjects:
Online Access:http://doi.org/10.2205/2024ES000945
Tags: Add Tag
No Tags, Be the first to tag this record!