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Journal Abstract Search
127 related items for PubMed ID: 17744263
1. Ultradeep (>300 kilometers) ultramafic xenoliths: petrological evidence from the transition zone. Sautter V, Haggerty SE, Field S. Science; 1991 May 10; 252(5007):827-30. PubMed ID: 17744263 [Abstract] [Full Text] [Related]
2. Ultradeep (greater than 300 kilometers), ultramafic upper mantle xenoliths. Haggerty SE, Sautter V. Science; 1990 May 25; 248(4958):993-6. PubMed ID: 17745405 [Abstract] [Full Text] [Related]
3. Sound velocities of majorite garnet and the composition of the mantle transition region. Irifune T, Higo Y, Inoue T, Kono Y, Ohfuji H, Funakoshi K. Nature; 2008 Feb 14; 451(7180):814-7. PubMed ID: 18273016 [Abstract] [Full Text] [Related]
5. 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 03; 145(3627):13-20. PubMed ID: 17769134 [Abstract] [Full Text] [Related]
8. Seismic observations of splitting of the mid-transition zone discontinuity in Earth's mantle. Deuss A, Woodhouse J. Science; 2001 Oct 12; 294(5541):354-7. PubMed ID: 11598296 [Abstract] [Full Text] [Related]
12. Dislocations in spinel and garnet high-pressure polymorphs of olivine and pyroxene: implications for mantle rheology. Madon M, Poirier JP. Science; 1980 Jan 04; 207(4426):66-8. PubMed ID: 17730816 [Abstract] [Full Text] [Related]
19. An inverted double seismic zone in chile: evidence of phase transformation in the subducted slab. Comte D, Suárez G. Science; 1994 Jan 14; 263(5144):212-5. PubMed ID: 17839180 [Abstract] [Full Text] [Related]
20. Spin transition zone in Earth's lower mantle. Lin JF, Vankó G, Jacobsen SD, Iota V, Struzhkin VV, Prakapenka VB, Kuznetsov A, Yoo CS. Science; 2007 Sep 21; 317(5845):1740-3. PubMed ID: 17885134 [Abstract] [Full Text] [Related] Page: [Next] [New Search]