Stratigraphy of the Paleozoic rocks in the Akiyoshi Terrane of the central Chugoku Massif

H. Sano; Y. Iijima; H. Hattori

doi:10.5575/geosoc.93.865

Stratigraphy of the Paleozoic rocks in the Akiyoshi Terrane of the central Chugoku Massif

H. Sano, Y. Iijima, H. Hattori

Dynamics, Structure and Evolution of the Earth and Planets

Research output: Contribution to journal › Article › peer-review

7 Citations (Scopus)

Abstract

The rocks of the area are lithostratigraphically grouped into four rock-units, the Koyama and Yoshii Groups, and the Sugeno Chert and Uji Formations. Spicular chert was deposited on the lower flank to foot of a seamount capped by a limestone build-up in an open-ocean setting, and radiolarians-bearing chert formed on the foot to ocean floor surrounding the seamount. -from English summary

Original language	English
Pages (from-to)	865-880
Number of pages	16
Journal	Journal - Geological Society of Japan
Volume	93
Issue number	12
DOIs	https://doi.org/10.5575/geosoc.93.865
Publication status	Published - 1987

All Science Journal Classification (ASJC) codes

Environmental Science(all)
Engineering(all)
Earth and Planetary Sciences(all)

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10.5575/geosoc.93.865

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abstract = "The rocks of the area are lithostratigraphically grouped into four rock-units, the Koyama and Yoshii Groups, and the Sugeno Chert and Uji Formations. Spicular chert was deposited on the lower flank to foot of a seamount capped by a limestone build-up in an open-ocean setting, and radiolarians-bearing chert formed on the foot to ocean floor surrounding the seamount. -from English summary",

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AU - Sano, H.

AU - Iijima, Y.

AU - Hattori, H.

PY - 1987

Y1 - 1987

N2 - The rocks of the area are lithostratigraphically grouped into four rock-units, the Koyama and Yoshii Groups, and the Sugeno Chert and Uji Formations. Spicular chert was deposited on the lower flank to foot of a seamount capped by a limestone build-up in an open-ocean setting, and radiolarians-bearing chert formed on the foot to ocean floor surrounding the seamount. -from English summary

AB - The rocks of the area are lithostratigraphically grouped into four rock-units, the Koyama and Yoshii Groups, and the Sugeno Chert and Uji Formations. Spicular chert was deposited on the lower flank to foot of a seamount capped by a limestone build-up in an open-ocean setting, and radiolarians-bearing chert formed on the foot to ocean floor surrounding the seamount. -from English summary

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Stratigraphy of the Paleozoic rocks in the Akiyoshi Terrane of the central Chugoku Massif

Abstract

All Science Journal Classification (ASJC) codes

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