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2. Multiple seismic discontinuities near the base of the transition zone in the Earth's mantle. Simmons NA, Gurrola H. Nature; 2000 Jun 01; 405(6786):559-62. PubMed ID: 10850712 [Abstract] [Full Text] [Related]
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5. Phase changes in the upper mantle. Anderson DL. Science; 1967 Sep 08; 157(3793):1165-73. PubMed ID: 17795496 [Abstract] [Full Text] [Related]
7. High-pressure polymorphs of olivine and the 660-km seismic discontinuity. Chudinovskikh L, Boehler R. Nature; 2001 May 31; 411(6837):574-7. PubMed ID: 11385569 [Abstract] [Full Text] [Related]
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10. Pressure sensitivity of olivine slip systems and seismic anisotropy of Earth's upper mantle. Mainprice D, Tommasi A, Couvy H, Cordier P, Frost DJ. Nature; 2005 Feb 17; 433(7027):731-3. PubMed ID: 15716950 [Abstract] [Full Text] [Related]
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12. 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]
13. Low-velocity zone atop the 410-km seismic discontinuity in the northwestern United States. Song TR, Helmberger DV, Grand SP. Nature; 2004 Feb 05; 427(6974):530-3. PubMed ID: 14765192 [Abstract] [Full Text] [Related]
14. Elastic properties of Fe-bearing Akimotoite at mantle conditions: Implications for composition and temperature in lower mantle transition zone. Zhao Y, Wu Z, Hao S, Wang W, Deng X, Song J. Fundam Res; 2022 Jul 05; 2(4):570-577. PubMed ID: 38934001 [Abstract] [Full Text] [Related]
15. 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]
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