FN Archimer Export Format
PT J
TI Correction to “A geomagnetic record over the last 3.5 million years from deep-tow magnetic anomaly profiles across the Central Indian Ridge” by Gaud Pouliquen, Yves Gallet, Jérôme Dyment, Philippe Patriat, and Chiori Tamura
BT 
AF POULIQUEN, G
   GALLET, Y
   DYMENT, J
   PATRIAT, P
   TAMURA, C
AS 1:1;2:1;3:2;4:1;5:3;
FF 1:;2:;3:;4:;5:;
C1 Institut de Physique du Globe de Paris, UMR 7577, Paris, France
   Université de Bretagne Occidentale, UMR 6538,Institut Universitaire Européen de la Mer, Plouzané, France
   University of Tokyo, Ocean Research Institute,Tokyo, Japan
C2 IPGP, FRANCE
   UBO, FRANCE
   UNIV TOKYO, JAPAN
TC 4
UR https://archimer.ifremer.fr/doc/00223/33379/31815.pdf
LA English
DT Article
CR MAGOFOND2-MD112
BO Marion Dufresne
AB High-resolution records of the geomagnetic field intensity over the last 3.5 Myr provided by paleomagnetic analyses of marine sediments and volcanics have shown the occurrence of short-lived low field intensity features associated with excursions or short polarity intervals. In order to evaluate the ability of marine magnetic anomalies to record the same geomagnetic events, we have collected six deep-tow (similar to500 m above the seafloor) and several sea surface magnetic anomaly profiles from the Central Indian Ridge across the Brunhes, Matuyama, and Gauss chrons (i.e., from the ridge axis to anomaly 2A). After removal of topography, latitude, and azimuth effects, we converted distances into time sequences using well-dated polarity reversal anomalies as tie points. We calculated the average signal to test the robustness of the short-wavelength anomalies. The resulting stacked profile is very similar to stacked sea surface and downward continued profiles from the Central Indian Ridge, the East Pacific Rise, and the Pacific-Antarctic Ridge. Our results suggest that in addition to polarity reversals, geomagnetic field intensity variations represent the major contributor to the detailed shape of recent marine magnetic anomalies in investigated areas. We observe a dense succession of microanomalies that are correlated to previously suggested geomagnetic events (subchrons or excursions) within the Brunhes and Matuyama chrons. A new small-scale magnetic anomaly, likely generated by several closely spaced excursions (Ontong Java 1 and 2, and Gilsa), is found after the Olduvai chron. The near-bottom results support the existence of three geomagnetic features between the Gauss-Matuyama boundary and Olduvai. They also suggest three geomagnetic events during the C2A. In subchron within the Gauss chron. This study emphasizes the potential of deep-tow magnetic surveys in detecting fluctuations in geomagnetic field intensity and, in particular, short-lived excursions, a poorly constrained part of the geomagnetic field temporal variation spectrum.
PY 2001
PD DEC
SO Journal Of Geophysical Research-solid Earth
SN 0148-0027
PU Amer Geophysical Union
VL 106
IS B12
UT 000173320800007
BP 30549
EP 30549
DI 10.1029/2001JB001637
ID 33379
ER

EF