Is Southern African Off-craton Lithospheric Mantle Warm Because of Steady State Conduction or a Mesozoic Thermal Disturbance?

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    W[2002AGUFM.T61A1245J]
    LA["Linked Authors (0)"]
    LI["Linked Institutions (1)"]
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ADS bibcode
2002AGUFM.T61A1245J
year
2002
Listed Authors
Janney, P. E.
Bell, D. R.
Schmitz, M.
Shirey, S. B.
Listed Institutions
Department of Geology, The Field Museum of Natural History 1400 S. Lake Shore Dr., Chicago, IL 60605 United States ; The Carnegie Institution of Washington, 5241 Broad Branch Rd., NW, Washington, DC 20015 United States
Departments of Chemistry and Biochemistry, Arizona State University, Tempe, AZ 85287 United States ; The Carnegie Institution of Washington, 5241 Broad Branch Rd., NW, Washington, DC 20015 United States
The Carnegie Institution of Washington, 5241 Broad Branch Rd., NW, Washington, DC 20015 United States
The Carnegie Institution of Washington, 5241 Broad Branch Rd., NW, Washington, DC 20015 United States

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