POSTSPINEL TRANSFORMATIONS AND THE WIDTH OF THE 670-KM DISCONTINUITY - A COMMENT ON POSTSPINEL TRANSFORMATIONS IN THE SYSTEM MG2SIO4-FE2SIO4 AND SOME GEOPHYSICAL IMPLICATIONS BY ITO,E. AND TAKAHASHI,E.

Những quyển sách tương tự

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  Được phát hành: (1990)
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• MANTLE GEOPHYSICS - MINERALOGICAL PHASE-CHANGE AT THE 670-KM DISCONTINUITY
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• The nature of the olivine - spinel transition in the Mg2SiO4-Fe2SiO4 system and its geophysical implications.
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