The Effect of Alumina on Phase Transformations at the 660-Kilometer Discontinuity from Fe-Mg Partitioning Experiments

Author:

Wood B. J.1,Rubie D. C.2

Affiliation:

1. B. J. Wood, Department of Geology, University of Bristol, Bristol BS8 1 RJ, UK.

2. D. C. Rubie, Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference22 articles.

1. SHARPNESS OF UPPER-MANTLE DISCONTINUITIES DETERMINED FROM HIGH-FREQUENCY REFLECTIONS;BENZ H.M.;NATURE,1993

2. THERMODYNAMIC PARAMETERS IN THE EARTH AS DETERMINED FROM SEISMIC PROFILES;BROWN J.M.;GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY,1981

3. STABILITY OF CLINOPYROXENE AT PRESSURE-TEMPERATURE CONDITIONS OF THE TRANSITION REGION;CANIL D;PHYSICS OF THE EARTH AND PLANETARY INTERIORS,1994

4. PRELIMINARY REFERENCE EARTH MODEL;DZIEWONSKI A.M.;PHYSICS OF THE EARTH AND PLANETARY INTERIORS,1981

5. EXPERIMENTAL-DETERMINATION OF ELEMENT PARTITIONING AND CALCULATION OF PHASE-RELATIONS IN THE MGO-FEO-SIO2 SYSTEM AT HIGH-PRESSURE AND HIGH-TEMPERATURE;FEI Y;JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS,1991

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