Development of oceanic detachment and asymmetric spreading at the Australian-Antarctic Discordance-Reference-Cited by-同舟云学术

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Development of oceanic detachment and asymmetric spreading at the Australian-Antarctic Discordance

Published:2004-12 Issue:12 Volume:5 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Okino Kyoko¹,Matsuda Kohei,Christie David M.²,Nogi Yoshifumi³,Koizumi Kin-ichiro¹

Affiliation:

1. Ocean Research Institute; University of Tokyo; 1-15-1 Minamidai, Nakano,; Tokyo; 164-8639; Japan

2. College of Oceanic and Atmospheric Sciences; Oregon State University; 104 Ocean Administration Building,; Corvallis; Oregon; 97331-5503; USA

3. National Institute of Polar Research; 1-9-10 Kaga, Itabashi,; Tokyo; 173-8515; Japan

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference72 articles.

1. Extremely asymmetric magmatic accretion of oceanic crust at the ends of slow-spreading ridge segments;Allerton;Geology,2000

2. The interrelation between variations in magnetic anomaly amplitudes and basalt magnetization and chemistry along the Southeast Indian Ridge;Anderson;J. Geophys. Res.,1980

3. Origin of extensional core complexes: Evidence from the Mid-Atlantic Ridge at Atlantis Fracture Zone;Blackman;J. Geophys. Res.,1998

4. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic;Cande;J. Geophys. Res.,1995

5. A revised identification of the oldest sea-floor spreading anomalies between Australia and Antarctica;Cande;Earth Planet. Sci. Lett.,1982

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