Sr-Nd-Pb-Hf Isotope Results from ODP Leg 187: Evidence for Mantle Dynamics of the Australian-Antarctic Discordance and Origin of the Indian MORB Source

Author:

Kempton Pamela D.1,Pearce Julian A.2,Barry Tiffany L.1,Fitton J. Godfrey3,Langmuir Charles4,Christie David M.5

Affiliation:

1. NERC Isotope Geosciences Laboratory; Kingsley Dunham Centre; Keyworth UK, NG12 5GG,

2. Department of Earth Sciences; University of Cardiff; UK, CF10 3YE,

3. Grant Institute; University of Edinburgh; Edinburgh UK, EH9 3JW,

4. Lamont-Doherty Geological Observatory and Department of Geological Sciences of Columbia University; Palisades New York 10964 USA

5. College of Oceanic and Atmospheric Sciences; Oregon State University; Oceanography Administration Building 104, Corvallis Oregon 97331 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference76 articles.

1. Geological evidence for the plate driving mechanism: The continental undertow hypothesis and the Australian-Antarctic Discordance;Alvarez;Tectonics,1990

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 the continental crust;Arculus;J. Proc. R. Soc. New South Wales,1999

4. Geochemistry of Heard Island (Southern Indian Ocean)-Characterization of an enriched mantle component and implications for enrichment of the sub-Indian-Ocean mantle;Barling;J. Petrol.,1994

5. The geochemistry of marine sediments, island arc magma genesis and crust-mantle recycling;Ben Othman;Earth Planet. Sci. Lett.,1989

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