BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN
Online ISSN : 2186-490X
Print ISSN : 1346-4272
ISSN-L : 1346-4272
Volume 68 , Issue 5
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Article
  • Toshihiro Yamada, Shota Teduka, Takahiro Kamiya, Yukio Yanagisawa
    2017 Volume 68 Issue 5 Pages 183-221
    Published: December 25, 2017
    Released: March 31, 2018
    JOURNALS FREE ACCESS

    The stratigraphy of the Miocene Saikawa Formation distributed in the southern Kanazawa area, Ishikawa Prefecture, is revised based on litho- and biostratigraphic studies. The previously defined Saikawa Formation is divided here into the Yamashina, Saikawa (redefined), and Koderayama formations in ascending order. The Yamashina Formation consists mainly of mudstone and contains diatoms which indicate ca.15.6–15.4 Ma within the diatom zone NPD4A. The Saikawa Formation is composed mainly of coarse-grained sandstone and the obtained diatoms were considered to be reworked. However, calcareous nannofossils of the zone CN5a (13.6–11.8 Ma) were reported from the Saikawa Formation in a previous study. These data indicate that the Saikawa Formation unconformably overlies the Yamashina Formation. The Koderayama Formation is characterized mainly by fine-grained sandstone with a basal conglomerate bed eroding the upper part of the Saikawa Formation. The Koderayama Formation in turn is eroded by a conglomerate bed of the overlying Pleistocene Omma Formation. The Koderayama Formation includes endocarps of Carya (Juglandaceae) which became extinct in Japan before 3 Ma. Therefore, the Omma Formation should unconformably overlie the Koderayama Formation with a sedimentary hiatus of more than 1.3 million years.

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  • Takahiro Yamamoto
    2017 Volume 68 Issue 5 Pages 223-235
    Published: December 25, 2017
    Released: March 31, 2018
    JOURNALS FREE ACCESS

    The Daisen-Kurayoshi tephra (DKP) is one of significant wide-spreading fallouts along the Japanese islands during the Late Pleistocene time. However, its stratigraphic position had not been fixed in NE Japan, because there was a conflict among previous studies. In this paper, I have analyzed major compositions of volcanic glasses within tephra layers, which were correlated with DKP in NE Japan, and compared dataset from the SG06 varve core (Smith et al., Quaternary Science Reviews, vol.67, p. 121–137, 2013). New results have revealed that the San-in 1 tephra (SAN1) immediately above the Numazawa-Mizunuma tephra (Nm-MZ) was mistaken as DKP around Mt. Bandai. The revised tephrostratigraphy in this region consists of DKP, Nm-MZ and SAN1 in ascending order.

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