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Detailed Reference Information |
Mandal, N., Chakravarty, K.H., Borah, K. and Rai, S.S. (2012). Is a cation ordering transition of the Mg-Fe olivine phase in the mantle responsible for the shallow mantle seismic discontinuity beneath the Indian Craton?. Journal of Geophysical Research 117: doi: 10.1029/2012JB009225. issn: 0148-0227. |
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Keywords
Mineral Physics, High-pressure behavior, Seismology, Body waves, Seismology, Mantle (1212, 1213, 8124) |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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