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2. Iron-silica interaction at extreme conditions and the electrically conducting layer at the base of Earth's mantle. Dubrovinsky L; Dubrovinskaia N; Langenhorst F; Dobson D; Rubie D; Gessmann C; Abrikosov IA; Johansson B; Baykov VI; Vitos L; Le Bihan T; Crichton WA; Dmitriev V; Weber HP Nature; 2003 Mar; 422(6927):58-61. PubMed ID: 12621431 [TBL] [Abstract][Full Text] [Related]
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5. Densities of liquid silicates at high pressures. Rigden SM; Ahrens TJ; Stolper EM Science; 1984 Nov; 226(4678):1071-4. PubMed ID: 17839996 [TBL] [Abstract][Full Text] [Related]
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8. Geology of the Crust and Mantle, Western United States: Geophysical data reveal a thin crust and anomalous upper mantle characteristic of active regions. Thompson GA; Talwani M Science; 1964 Dec; 146(3651):1539-49. PubMed ID: 17775979 [TBL] [Abstract][Full Text] [Related]
9. The Melting Curve of Iron to 250 Gigapascals: A Constraint on the Temperature at Earth's Center. Williams Q; Jeanloz R; Bass J; Svendsen B; Ahrens TJ Science; 1987 Apr; 236(4798):181-2. PubMed ID: 17789782 [TBL] [Abstract][Full Text] [Related]
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13. Geological Aspects of High-Pressure Research: High-pressure experimentation is providing a new look at problems in geophysics and petrology. Boyd FR Science; 1964 Jul; 145(3627):13-20. PubMed ID: 17769134 [TBL] [Abstract][Full Text] [Related]
14. Density distribution in Earth. Press F Science; 1968 Jun; 160(3833):1218-21. PubMed ID: 17818740 [TBL] [Abstract][Full Text] [Related]
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