Conodont fossils from the Kiryu and Ashikaga District (Quadrangle series 1:50,000),central Japan with emphasis on the reexamination of “Carboniferous” conodonts from the Ashio Belt-Reference-Cited by-同舟云学术

Conodont fossils from the Kiryu and Ashikaga District (Quadrangle series 1:50,000),central Japan with emphasis on the reexamination of “Carboniferous” conodonts from the Ashio Belt

Published:2021-10-13 Issue:4 Volume:72 Page:325-344
ISSN:1346-4272
Container-title:BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN
language:en
Short-container-title:Bull. Geol. Surv. Japan

Author:

MUTO Shun¹,ITO Tsuyoshi¹

Affiliation:

1. AIST, Geological Survey of Japan, Research Institute of Geology and Geoinformation

Publisher

National Institute of Advanced Industrial Science

Subject

General Medicine

Link

https://www.jstage.jst.go.jp/article/bullgsj/72/4/72_325/_pdf

Reference63 articles.

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2. Aono, H. (1985) Geologic structure of the Ashio and Yamizo Mountains with special reference to its tectonic evolution. Science reports of the Institute of Geoscience, University of Tsukuba. Section B, Geological Sciences, 6, 21–57.

3. Chen, Y., Krystyn, L., Orchard, M. J., Lai, X. L. and Richoz, S.(2016) A review of the evolution, biostratigraphy, provincialism and diversity of Middle and early Late Triassic conodonts. Papers in Palaeontology, 2, 235–263.

4. Clark, D. L. and Mosher, L. C. (1966) Stratigraphic, geographic, and evolutionary development of the conodont genus Gondolella. Journal of Paleontology,40, 376–394.

5. Conodont Research Group (1972) Conodonts at the Permian-Triassic boundary in Japan—Conodonts from the basal part of the Adoyama Formation—. Journal of the Geological Society of Japan, 78, 355–368 (in Japanese with English abstract). 10.5575/geosoc.78.355

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