Motoko Yoshizaki

发表

High-temperature water–rock interactions and hydrothermal environments in the chondrite-like core of Enceladus

F. Postberg, S. Tachibana, T. Kuwatani, 2015, Nature Communications.

Reactions between basalt and CO2-rich seawater at 250 and 350°C, 500bars: Implications for the CO2 sequestration into the modern oceanic crust and the composition of hydrothermal vent fluid in the CO2-rich early ocean

Ken Takai, Michael J. Russell, Yuka Masaki, 2013 .

Hydrogen-rich hydrothermal environments in the Hadean ocean inferred from serpentinization of komatiites at 300 °C and 500 bar

Kentaro Nakamura, H. Tsunakawa, K. Takai, 2015, Progress in Earth and Planetary Science.

Experimental Hydrogen Production in Hydrothermal and Fault Systems: Significance for Habitability of Subseafloor H2 Chemoautotroph Microbial Ecosystems

T. Hirose, Katsuhiko Suzuki, T. Shibuya, 2015 .

Origin of methane in serpentinite-hosted hydrothermal systems: The CH4–H2–H2O hydrogen isotope systematics of the Hakuba Happo hot spring

K. Kurokawa, Keita Yamada, N. Yoshida, 2014 .

H2 generation by experimental hydrothermal alteration of komatiitic glass at 300°C and 500 bars: A preliminary result from on-going experiment

Kenji Shimizu, Ken Takai, Shigenori Maruyama, 2009 .

Diversity of fluid geochemistry affected by processes during fluid upwelling in active hydrothermal fields in the Izena Hole, the middle Okinawa Trough back-arc basin

Ken Takai, Yoshio Takahashi, Fumio Inagaki, 2014 .

High-temperature water–rock interactions and hydrothermal environments in the chondrite-like core of Enceladus

F. Postberg, S. Tachibana, T. Kuwatani, 2015, Nature Communications.

Development of hydrothermal and frictional experimental systems to simulate sub-seafloor water–rock–microbe interactions

Kensei Kobayashi, Kentaro Nakamura, Shingo Kato, 2015 .