FN Archimer Export Format
PT J
TI Bottom water throughflows at the Rio de Janeiro and Rio Grande Fracture Zones
BT 
AF MERCIER, Herle
   WEATHERLY, Georges
   ARHAN, Michel
AS 1:1;2:2;3:3;
FF 1:;2:;3:PDG-DRO-DOPS-LPO;
C1 UBO, IFREMER, CNRS, Lab Phys Oceans, Plouzane, France.
   Florida State Univ, Dept Oceanog, Tallahassee, FL USA.
C2 CNRS, FRANCE
   UNIV FLORIDA STATE, USA
   IFREMER, FRANCE
SI BREST
SE PDG-DRO-DOPS-LPO
IN WOS Ifremer jusqu'en 2018
IF 2.719
TC 12
UR https://archimer.ifremer.fr/doc/2000/publication-491.pdf
LA English
DT Article
CR CITHER : CIRCULATION THERMOCLINE
DE ;Fractures and faults;Structural geology;Hydrography;General circulation;Physical oceanography
AB Bottom water throughflows at the Rio de Janeiro Fracture Zone (22 degrees S) and Rio Grande Fracture Zone (26 degrees S) of the Mid-Atlantic Ridge are identified from hydrographic anomalies observed along 9 degrees W in the Angola Basin. The throughflow water is supplied by a meridional band of cold and fresh water lying against the western flank of the Ridge.
PY 2000
PD MAY
SO Geophysical Research Letters
SN 0094-8276
PU American Geophysical Union
VL 27
IS 10
UT 000087062000020
BP 1503
EP 1506
ID 491
ER

EF