U–Pb ages of granitoids around the Kofu basin: Implications for the Neogene geotectonic evolution of the South Fossa Magna region, central Japan

Author:

Sawaki Yusuke1ORCID,Asanuma Hisashi2,Abe Mariko3,Hirata Takafumi2ORCID

Affiliation:

1. Department of Earth Science and Astronomy The University of Tokyo Tokyo Japan

2. Geochemistry Research Center The University of Tokyo Tokyo Japan

3. Institute for Extra‐cutting‐edge Science and Technology Avant‐garde Research (X‐star) Japan Agency for Marine‐earth Science and Technology (JAMSTEC) Yokosuka‐City Japan

Funder

Japan Society for the Promotion of Science

Publisher

Wiley

Subject

Geology

Reference81 articles.

1. Geological age and paleobathymetry of the Koma Group, Yamanashi Prefecture, Central Japan;Akimoto K.;Bulletin of the Earthquake Research Institute,1990

2. Multiple collision tectonics of the South Fossa Magna in central Japan;Amano K.;Modern Geology,1991

3. Aoike K.(1998).Collisional accretionary block of the Eo‐Oligocene paleo‐Izu‐Bonin Arc in the Koma massif the Izu Collision Zone (preliminary report). Paper presented at the The 105th anuual meeting of the Geological Society of Japan (Matsumoto) 39.

4. Tectonic evolution of the Izu collision zone. Research report of the Kanagawa prefectural museum;Aoike K.;Natural History,1999

5. I- and S-type granites in the Lachlan Fold Belt

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