logo Hiroshima University, Faculty of Science, Department of Earth and Planetary Systems Science
Graduate School of Advanced Science and Engineering, Earth and Planetary Systems Science Program

MENU

Research Group

Earth and Planetary Material Science

The time and space scales of many geological phenomena are beyond those of history and access of mankind. Therefore, we need to study natural rocks and minerals which preserve information of the Earth activities, to understand what happened in past, and to predict geological future events. Members of this group study the natural rocks and minerals using cutting edge research tools such as a sensitive high resolution ion microprobe, X-ray fluorescence/Raman spectrometers, transmission/scanning electron microscopes, X-ray diffractometer and others, in addition to field survey. Our main topics include 1) evolution of continental crusts, 2) rock flow mechanism, 3) process of fault motion, 4) formation process of ore, 5) rock-fluid interaction and 6) crystallographic characteristics of minerals and their applications.

ANDO, Jun-ichi (Professor)
KATAYAMA, Ikuo (Professor)
DAS, Kaushik (Professor)
OKAZAKI, Keishi (Associate Professor)
OHKAWA, Makio (Assistant Professor)

  • Rock rheology (fracture, plastic deformation)
  • Fault dynamics and earthquake generation
  • Subsurface fluid migration
  • Tectonics of Japanese Island and East Asia​
  • Precambrian plate tectonics
  • Ore formation process
  • Rock-fluid interaction
  • Crystal chemistry of minerals
Thin section of upper-mantle rock (microscopic image under cross-polarized light). Inset: dislocations in olivine (transmission electron microscopic image).
高温高圧変形透水試験機
長崎県野母半島での蛇紋岩調査
Deformed gneiss in India (field survey in 2010)
Ilmenite lamellae in magnetite in Yamaguchi Prefecture, Japan (backscattered electron image by scanning electron microscopy)

(enlarged image with brief explanation on mouseover)

Earth and Planetary Chemistry

Earth and Planetary Chemistry group is working on cosmochemistry for exterritorial materials (meteorite and cosmic dust), geochemistry for magma dynamics, chemical evolution experiments for biochemical precursor, experimental paleontology for fossil, sedimentary rock, and microbe to understand the evolution for the solar system, the Earth, and life for 4.6 Ga. We use a Thermal Ionization Mass Spectrometer (TIMS), Inductively Coupled Plasma-Mass Spectrometer (ICP-MS), pyrolysis Gas Chromatography-Mass spectrometer (GCMS), electron microscope (e.g., SEM, TEM, EDS, and EBSD), and Synchrotron Radiation (e.g., XRD and STXM) to achieve our goal.

SHIBATA, Tomoyuki (Professor)
SHIRAISHI, Fumito (Associate Professor)
YABUTA, Hikaru (Professor)
AKIZAWA, Norikatsu (Associate Professor)
KOIKE, Mizuho (Assistant Professor)
MIYAHARA, Masaaki (Associate Professor)
YOSHIKAWA, Masako (Professor (Special Appointment))
DEY, Bidisha (Assistant Professor (Special Appointment))
HIRAYAMA, Takehiro (Assistant Professor (Special Appointment))

  • Magma geochemistry
  • Astrobiology
  • Analysis of cosmic dusts
  • Shock events recorded in shocked meteorites​
  • Water-rock interaction on the Mars
  • Geomicrobiology
Stromatolite in the Western Australia
Field survey at the Sanbe hot spring in Shimane Prefecture, Japan
Shock-induced glass (blue) in plagioclase (red) caused by meteorite impact
High-pressure mineral (stishovite, SiO2) in shocked meteorite (transmission electron microscopic image)
Mass spectrometer

(enlarged image with brief explanation on mouseover)

Earth and Planetary Physics

Present internal structures of the Earth and planets are the results of long-term deformation and fractionation of internal component materials since their births. To study internal structure leads us to know internal material properties and transport mechanisms. And, conversely, to study material properties and transport mechanisms takes us into understanding how present internal structures were created. In this group, we study internal structures, material properties and their transport mechanisms in the Earth and other planets from analyses of seismic waves, friction experiments, high-temperature and high-pressure experiments, and numerical simulations.

INOUE, Toru (Professor)
SUDA, Naoki (Professor)
KAWAZOE, Takaaki (Associate Professor)
NAKAKUKI, Tomoeki (Associate Professor (Special Recognition))
TAKAICHI Gouru (Assistant Professor (Special Appointment))
Takashi Nakagawa (Visiting Associate Professor)

  • Slow earthquakes
  • Free oscillations of the Earth
  • Structure and properties of the Earth’s interior
  • Water circulation in the Earth’s interior
  • Deep magma
  • Mantle convection
非火山性長周期微動の震源分布。色は時間変化を表す。
マルチアンビル型高温高圧発生装置。28万気圧、1800℃までの極限状態を作り出せる。
マントルの造岩鉱物
高温高圧実験の回収試料の反射電子像。試料の右上は、溶けていた組織を示している。
スタグナントスラブ形成および下部マントへの落下の数値シミュレーション。 Case 1, 2, 3は、スラブの流動則、および相変化のパラメータが異なるモデル である。物理パラメータに依存して作られるスラブの形状が変化することを 示している。上はプレートの運動速度(センチメートル/年)、下の色は温度 (青が低温・赤が高温)、点線は相境界を表す。時間は上から下へ流れる。 42.6 Myrという数字が沈み込みが始まってからの年代で、42.6百万年(4,260万年) を表す。

(enlarged image with brief explanation on mouseover)

Integrated Earth and Ocean Sciences (Institute for Interdisciplinary Science)

We study issues of geosciences, such as earthquakes and global environmental changes, by analyzing drill core samples and related materials recovered from a wide range of locations from continents to deep-sea floor with an interdisciplinary approach.

ISHIKAWA, Tsuyoshi (Visiting Professor)
TOMIOKA, Naotaka (Visiting Professor)
HIROSE, Takehiro (Visiting Professor)
HOSHINO, Tatsuhiko (Visiting Professor)
MORONO, Yuki (Visiting Professor)
NAKADA, Ryoichi (Visiting Associate Professor)

  • Geochemical cycle and enviromental change recorded in sediments and rocks
  • Microbiological and geochemical exploration of subseafloor biosphere
  • Mechanics of earthquake and faulting
  • Geomicrobiology
  • Development of analytical techniques of isotopes and trace elements in core samples