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| 1 | Foreword显示文摘The contributions to this Special Issue were called on the occasion of the upcoming birthday anniversary of one of the outstanding scientists in field of mantle rheology and rock deformation, Prof. Zhenmin Jin, China University of Geosciences, to celebrate | Harry W Green II 章军锋 Larissa F Dobrzhinetskaya Tetsuo Irifune | 2010 | Journal of Earth Science2010，21，5： | 2 |
| 2 | Technical Development of Simple Shear Deformation Experiments Using a Deformation-DIA Apparatus显示文摘Technical developments for simple shear deformation experiments at high pressures were made. The newly designed cell assembly can be compressed by deformation-DIA apparatuses with the MA 6-6 system, which consists of six second-stage tungsten carbide anvils (with a truncated edge length of 5 mm) and the anvil guide. Deformation of samples was barely observed during the compression process, showing that the shear strain of the deformed samples can be measured by the rotation of a strain marker. Simple shear deformation experiments on anhydrous and hydrous oli-vine aggregates were conducted under upper mantle conditions (pressures of 5.2–7.6 GPa and tem-peratures of 1 473–1 573 K), and sample deformation with a shear strain of γ=0.8–1.2 was success-fully achieved at a shear strain rate of 4.0×10-5–7.5×10-5 s-1. The present study extended the pressure range of simple shear deformation experiments in the deformation-DIA apparatus from 3 GPa in an early study to 7.6 GPa at high temperatures. | Tomohiro Ohuchi Takaaki Kawazoe Norimasa Nishiyama Yu Nishihara Tetsuo Irifune | 2010 | Journal of Earth Science2010，21，5： | 2 |
| 3 | Pressure and Temperature Dependences of Elastic Properties of Grossular Garnet up to 17 GPa and 1 650 K显示文摘Simultaneous ultrasonic elastic wave velocity and in situ synchrotron X-ray measurements on grossular garnet were carried out up to 17 GPa and 1 650 K. P-and S-wave velocities and bulk and shear modulus showed linear pressure and temperature dependence. These data yielded a pressure derivative of the bulk modulus of 4.42(7) and a shear modulus of 1.27(3), which are in good agreement with those of garnets with variable chemical compositions. Temperature dependence of the bulk modulus of grossular (-1.36×10-2 GPa/K) is also similar to that of other garnets, while the temperature dependence of the shear modulus of grossular (-1.11×10-2 GPa/K) is higher than those of magnesium end-member garnets and pyrolitic garnet. | Yoshio Kono Steeve Gréaux Yuji Higo Hiroaki Ohfuji Tetsuo Irifune | 2010 | Journal of Earth Science2010，21，5： | 2 |
| 4 | Propofol-induced anesthesia in mice is mediated by gamma-aminobutyric acid-A and excitatory amino acid receptors显示文摘 | Irifune M Takarada T Shimizu Y | 2003 | Anesth Analg2003，97，2： | 1 |
| 5 | Nature of the 650 km seismic discontinuity: implications for mantle dynamics and differentiation显示文摘 | Ringwood A E Irifune T | 1988 | Nature1988，331，： | 1 |
| 6 | Docetaxel and eisplatin as second-line chemotherapy for advanced non-small cell lung cancer 显示文摘 | Hamada H Irifune K Ito R | 2007 | Gan To Kaqaku Ryoho2007，34，8： | 1 |
| 7 | Ketamine-induced anesthesia involves the NMDA receptor-channel complex in mice 显示文摘 | Irifune M Shimizu T Nomoto M | 1992 | Brain Res1992，596，12： | 1 |
| 8 | Melting of enstatite from 13 to 18 GPa under hydrous conditions显示文摘 | Yamada A Inoue T Irifune T | 2004 | Phys Earth Planet Int2004，147，： | 1 |
| 9 | Evidence for GABA(A) receptor agonistic properties of ketamine: convulsive and anesthetic behavioral models in mice显示文摘 | Irifune M Sato T Kamata Y | 2000 | Anesth Analg2000，91，： | 1 |
| 10 | The phase boundary between wadsleyite and ringwoodite in Mg2SiO4 determined by in situ X-ray diffraction显示文摘 | Inoue T Irifune T Higo Y | 2006 | Physics and Chemistry of Minerals2006，33，： | 1 |
| 11 | Phase transformation in di- opside CaMgSi206 at pressures up to 25 GPa显示文摘 | Irifune T Susaki J I Yagi T | 1989 | Geophysical Research Letters1989，16，： | 1 |
| 12 | The postspinel phase boundary in Mg2SiO4 determined by in situ X-ray diffraetion显示文摘 | IRIFUNE T NISHIYAMA N KURODA K | 1998 | Science1998，279，： | 1 |
| 13 | Formation of diamond powders from melamine under high pressure and high temperature显示文摘High pressure pyrolysis of melamine has been attracting great interest recently, due to it being considered as a suitable precursor to realize the g-C3N4 and even superhard C3N4 . In this work, we studied the detailed pyrolysis behavior of melamine at 22 GPa. Melamine was stable at 800 , and decomposed to diamond in the form of powder at 1500-2000 under this pressure condition. At 2000 , the pure cubic diamond powders with 0.1-0.5 μm grain size were obtained. The diamond particles exhibited euhedral forms and dispersed to each other, we proposed that these novel features were caused by the presence of liquid N2 and NH3 during diamond formation. The high pressure pyrolysis of melamine may provide a new means of producing micrometer-sized diamond powders. | 房雷鸣 陈喜平 H. Ohfuji T. Irifune 孙光爱 陈波 彭述明 | 2013 | Chinese Physics C2013，37，8： | 1 |
| 14 | Determination of the phase boundary between ilmenite and perovskite in MgSiO3 by in situ X-ray diffraction and quench experiments显示文摘 | KURODA K IRIFUNE T INOUE T | 2000 | Phys Chem Miner2000，27，： | 1 |
| 15 | Application of synchrotron radiation and Kawai-type apparatus to various studies in high-pressure mineral physics显示文摘 | IRIFUNE T | 2002 | Mineral Mag2002，66，： | 1 |
| 16 | Seven cases of tuberculous otitis media 显示文摘 | Nishiike S Irifune M Kubo T | 2000 | Nippon Jibiinkoka Gakkai Kaiho2000，103，12： | 1 |
| 17 | Laryngeal tuberculo- sis: a report of 15 cases显示文摘 | Nishiike S Irifune M Doi K | 2002 | Ann Otol Rhinol Laryngeal2002，111，10： | 1 |
| 18 | Laryngeal tuberculo- sis:a report of 15 cases 显示文摘 | Nishiike S Irifune M Doi K | 2002 | Ann Otol Rhinol Laryngeal2002，111，10： | 1 |
| 19 | Total Synthesis of (±)-Kainic acid: A photochemical C-H carbamoylation approach显示文摘 | Kamon T Irifune Y Tanaka T | 2011 | Organic Letters2011，13，10： | 1 |
| 20 | Preliminary Deformation Experiment of Ringwoodite at 20 GPa and 1 700 K Using a D-DIA Apparatus显示文摘A deformation experiment of ringwoodite with a strain of 9% was achieved at 20 GPa and 1 700 K and at a strain rate of 3×10-5 s-1 using a deformation-DIA (D-DIA) apparatus and a multi-anvil 6-6 (MA 6-6) assembly. The crystallographic orientations of the deformed sample were suc-cessfully analyzed by the electron backscatter diffraction (EBSD) method, although any notable lattice-preferred orientation (LPO) was not observed presumably due to the insufficient strain in the present experiment. In this study, the deformation experiment on ringwoodite succeeded at P-T conditions con-sistent with the lower part of the mantle transition zone and at a controlled strain rate for the first time. The present study extended the pressure range of deformation experiments in the D-DIA apparatus from 16 GPa in our earlier study to 20 GPa at 1 700 K. The successful extension of the pressure range demonstrates potential importance of the D-DIA apparatus in studying rheological properties of min-erals under the P-T conditions of the whole mantle transition zone. | Takaaki Kawazoe Tomohiro Ohuchi Norimasa Nishiyama Yu Nishihara Tetsuo Irifune | 2010 | Journal of Earth Science2010，21，5： | 1 |
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