J-GLOBAL ID:201801016607064166   Update date: Jun. 09, 2024


Affiliation and department:
Research field  (1): Solid earth science
Research theme for competitive and other funds  (4):
  • 2019 - 2022 Oceanic plateau-origin rocks in orogenic belts: Towards understanding the genesis of oceanic LIP
  • 2016 - 2019 Metasomatic process of the mantle wedge recorded in basal peridotites from the Oman ophiolite
  • 2011 - 2012 Carbon cycling in the subduction zones deduced from in-situ Carbon isotope analyses
  • 2006 - 2008 Formation of crust-mantle boundary in the mid-ocean ridge
Papers (165):
  • Yuji Ichiyama, Hisatoshi Ito, Akihiro Tamura, Tomoaki Morishita. Mafic veins in the mantle section of the Oman ophiolite: Petrological and geochronological insights from the Oman Drilling Project cores. Lithos. 2024. 478-479
  • Kazuto Mikuni, Naoto Hirano, Shiki MacHida, Hirochika Sumino, Norikatsu Akizawa, Akihiro Tamura, Tomoaki Morishita, Yasuhiro Kato. Contribution of carbonatite and recycled oceanic crust to petit-spot lavas on the western Pacific Plate. Solid Earth. 2024. 15. 2. 167-196
  • Shoji Arai, Terumi Ejima, Akihiro Tamura, Emi Wako, Tomoaki Morishita, Satoko Ishimaru. Characteristics of serpentinite cobbles from Takase and Kashima Rivers, central Japan, and their geologic implications: an example of the importance of river cobble petrology. The Journal of the Geological Society of Japan. 2023. 129. 1. 643-654
  • Kazuto Mikuni, Naoto Hirano, Shiki Machida, Hirochika Sumino, Norikatsu Akizawa, Akihiro Tamura, Tomoaki Morishita, Yasuhiro Kato. Carbonatite-induced petit-spot melts squeezed upward from the asthenosphere beneath the Jurassic Pacific Plate. 2023
  • Sherif Mansour, Noriko Hasebe, Mohamed Zaki Khedr, Akihiro Tamura, Amer A. Shehata. Tectonic-Thermal Evolution of the Wadi El-Dahal Area, North Eastern Desert, Egypt: Constraints on the Suez Rift Development. Minerals. 2023. 13. 8. 1021-1021
MISC (72):
※ Researcher’s information displayed in J-GLOBAL is based on the information registered in researchmap. For details, see here.

Return to Previous Page