| Ultrahard polycrystalline diamond from graphite T Irifune, A Kurio, S Sakamoto, T Inoue, H Sumiya Nature 421 (6923), 599-600, 2003 | 938 | 2003 |
| Phase transformations in subducted oceanic crust and buoyancy relationships at depths of 600–800 km in the mantle T Irifune, AE Ringwood Earth and Planetary Science Letters 117 (1-2), 101-110, 1993 | 531 | 1993 |
| Absence of an aluminous phase in the upper part of the Earth's lower mantle T Irifune Nature 370 (6485), 131-133, 1994 | 377 | 1994 |
| Nature of the 650–km seismic discontinuity: implications for mantle dynamics and differentiation AE Ringwood, T Irifune Nature 331 (6152), 131-136, 1988 | 367 | 1988 |
| An experimental investigation of the pyroxene-garnet transformation in a pyrolite composition and its bearing on the constitution of the mantle T Irifune Physics of the Earth and Planetary Interiors 45 (4), 324-336, 1987 | 341 | 1987 |
| Stability of magnesite and its high-pressure form in the lowermost mantle M Isshiki, T Irifune, K Hirose, S Ono, Y Ohishi, T Watanuki, E Nishibori, ... Nature 427 (6969), 60-63, 2004 | 331 | 2004 |
| The postspinel phase boundary in Mg2SiO4 determined by in situ X-ray diffraction T Irifune, N Nishiyama, K Kuroda, T Inoue, M Isshiki, W Utsumi, ... Science 279 (5357), 1698-1700, 1998 | 318 | 1998 |
| Subduction of continental crust and terrigenous and pelagic sediments: an experimental study T Irifune, AE Ringwood, WO Hibberson Earth and Planetary Science Letters 126 (4), 351-368, 1994 | 318 | 1994 |
| Phase transformations in primitive MORB and pyrolite compositions to 25 GPa and some geophysical implications T Irifunea, AE Ringwood High‐Pressure Research in Mineral Physics: A Volume in Honor of Syun‐iti …, 1987 | 300 | 1987 |
| Experimental determination of element partitioning between silicate perovskites, garnets and liquids: constraints on early differentiation of the mantle T Kato, AE Ringwood, T Irifune Earth and Planetary Science Letters 89 (1), 123-145, 1988 | 297 | 1988 |
| Phase transformations in a harzburgite composition to 26 GPa: implications for dynamical behaviour of the subducting slab T Irifune, AE Ringwood Earth and Planetary Science Letters 86 (2-4), 365-376, 1987 | 285 | 1987 |
| Iron partitioning and density changes of pyrolite in Earth’s lower mantle T Irifune, T Shinmei, CA McCammon, N Miyajima, DC Rubie, DJ Frost Science 327 (5962), 193-195, 2010 | 270 | 2010 |
| Stability of hydrous silicate at high pressures and water transport to the deep lower mantle M Nishi, T Irifune, J Tsuchiya, Y Tange, Y Nishihara, K Fujino, Y Higo Nature Geoscience 7 (3), 224-227, 2014 | 261 | 2014 |
| A new high-pressure form of MgAl2O4 T Irifune, K Fujino, E Ohtani Nature 349 (6308), 409-411, 1991 | 260 | 1991 |
| Phase relations and volume changes of hafnia under high pressure and high temperature O Ohtaka, H Fukui, T Kunisada, T Fujisawa, K Funakoshi, W Utsumi, ... Journal of the American Ceramic Society 84 (6), 1369-1373, 2001 | 250 | 2001 |
| The eclogite-garnetite transformation at high pressure and some geophysical implications T Irifune, T Sekine, AE Ringwood, WO Hibberson Earth and Planetary Science Letters 77 (2), 245-256, 1986 | 245 | 1986 |
| Hardness and deformation microstructures of nano-polycrystalline diamonds synthesized from various carbons under high pressure and high temperature H Sumiya, T Irifune Journal of materials research 22 (8), 2345-2351, 2007 | 226 | 2007 |
| An experimental study of the garnet-perovskite transformation in the system MgSiO3 Mg3Al2Si3O12 T Irifune, T Koizumi, J Ando Physics of the Earth and Planetary Interiors 96 (2-3), 147-157, 1996 | 206 | 1996 |
| Phase relations and equations of state of under high temperature and high pressure O Ohtaka, H Fukui, T Kunisada, T Fujisawa, K Funakoshi, W Utsumi, ... Physical Review B 63 (17), 174108, 2001 | 202 | 2001 |
| Sound velocities of majorite garnet and the composition of the mantle transition region T Irifune, Y Higo, T Inoue, Y Kono, H Ohfuji, K Funakoshi Nature 451 (7180), 814-817, 2008 | 177 | 2008 |
Toru InoueHiroshima UniversityE-mailová adresa ověřena na: hiroshima-u.ac.jp
