Geochronology of Ashidani Formation in the Hida Gaien Belt at Kuzuryu, Central Japan

Author:

MATSUMOTO Takayuki1

Affiliation:

1. ASCO-Daito Co., Ltd.

Publisher

Tokyo Geographical Society

Subject

Earth-Surface Processes,Geology,Geophysics,Geography, Planning and Development,Global and Planetary Change

Reference56 articles.

1. Bhatia, M.R. (1983): Plate tectonics and geochemical composition of sandstones. Journal of Geology, 91, 611-649.

2. Black, L.P., Kamo, S.L., Allen, C.M., Aleinikoff, J.N., Davis, D.W., Korsch, R.J. and Foudoulis, C. (2003): TEMORA 1: A new zircon standard for U–Pb geochronology. Chemical Geology, 200, 155-170.

3. Hashimoto, M. (1972): Mineral facies of the Sangun metamorphic rocks of the Chugoku Province. Bulletin of National Museum of Nature and Science, 15, 767-775.

4. Hayasaka, Y. (1986): Discovery of Triassic conodonts and Jurassic type radiolarians from the Hattou Formation of the “Sangun metamorphic rocks”. Abstracts, The 93th Annual Meeting of Geological Society of Japan, 465.*

5. Hayasaka, Y. (1987): Study on the late paleozoic-early mesozoic tectonic development of western half of the Inner Zone of Southwest Japan. Geological Report of Hiroshima University, 27, 119-204.

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