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Graduate School of Advanced Science and Engineering, Earth and Planetary Systems Science Program

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Research Group

Earth and Planetary Material Science

Rocks and minerals that record the history of the Earth from about 4 billion years ago to the present are exposed on the Earth’s surface, as well as rocks and minerals that have come from the Earth’s interior at depths of 400 to 670 km. The Earth and Planetary Materials Science Group collects such rocks and minerals from all over the world and performs chemical composition analysis, dating, deformation texture analysis, structural analysis, deformation experiments, friction experiments, etc. to elucidate the formation history of the continents and the Japan Islands, elucidate the mechanisms of dynamic deformation phenomena occurring on Earth, and conduct research into the crystallographic properties of minerals.

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

  • Rock rheology (properties related to fracture and flow)
  • Fault dynamics and earthquake generation
  • Movement and circulation of fluid in the Earth’s interior
  • Precambrian plate tectonics (mainly on the Indian subcontinent)​
  • Formation history of continental and island arc crusts in East Asia and the Japan
  • Reconstruction of the paleo-Pacific crust from ophiolites
  • Physical and chemical properties of minerals based on crystallography
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)

Earth and Planetary Chemistry

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

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

  • Magma geochemistry and its application to material cycle between the crust and mantle
  • Space dust collected from Antarctica and the International Space Station
  • Synthesis and nano-observation of primitive cellular functional materials leading to the origin of life
  • Water-rock reactions that occurred on the surface of Mars​
  • Shock metamorphic history recorded in meteorites
  • Environmental changes from microbial mineralization
  • Studying sedimentary rocks using paleontological and geochemical methods
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

Earth and Planetary Physics

The interiors of the Earth and planets have been moving for a long time since their formation, and have differentiated into their current structure. Investigating the current internal structure leads to understanding the properties of materials and their internal movements, and conversely, investigating the properties and movements of materials allows us to understand the process by which the current internal structure was formed. The Earth and Planetary Physics Group is conducting research into the mechanisms of movement of the solid parts of the Earth and planets and their internal structures using methods such as seismic wave analysis, high-temperature and high-pressure experiments, and numerical simulations.

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

  • Slow earthquakes
  • Internal structure of the Earth
  • Phase changes and flow of planetary materials under high temperature and pressure
  • Properties of magma in the Earth’s interior
  • Mantle convection and fluid movement
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。

Integrated Earth and Ocean Sciences / Center for Developing Pioneers in Science, JAMSTEC Kochi Institute for Core Sample Research

Core samples drilled from various regions on the ocean floor and land record various geological phenomena, environmental changes, and material cycles occurring on the Earth’s surface and interior. By systematically analyzing these samples, we can gain knowledge about the Earth’s past, present, and future. From this perspective, we are working on the following research themes.

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)

  • Environmental changes and material cycles on the Earth’s surface through the analysis of sediments and rocks
  • Biogeochemical material cycles on the ocean floor
  • Rheology of fault zones and the mechanism of earthquake occurrence
  • Development of analytical techniques of isotopes and trace elements in core samples