BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN
Online ISSN : 2186-490X
Print ISSN : 1346-4272
ISSN-L : 1346-4272
Volume 68 , Issue 6
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Article
  • Yukio Yanagisawa, Mahito Watanabe
    2017 Volume 68 Issue 6 Pages 259-285
    Published: December 28, 2017
    Released: April 12, 2018
    JOURNALS FREE ACCESS

    A revised lithostratigraphy has been proposed for the Neogene sedimentary sequence distributed in the southern part of the Osado Mountains area, Sado Island. The Neogene sediments of this area unconformably overlie the lower Miocene volcanic rocks, and are divided into seven formations in ascending order: the Orito, Hanyugawa, Nakayama, Nozaka, Kawachi, Kaidate and Shichiba formations. The Orito Formation is redefined in this report, consisting of fluvial sediments in its lower part and muddy fine-grained sandstone of estuary environment in its upper part. The newly proposed Hanyugawa Formation is conformably overlies the Orito Formation with a basal transgressive conglomerate bed and consists of marine calcareous sandstone, gray marine mudstone and glauconite sandstone. The redefined Nakayama Formation is composed of lower hard siliceous mudstone and upper diatomaceous mudstone containing abundant well-preserved marine diatom fossils. The Nozaka Formation is proposed for massive mudstone which overlies the Nakayama Formation with a glauconite bed.

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  • Yukio Yanagisawa, Mahito Watanabe
    2017 Volume 68 Issue 6 Pages 287-339
    Published: December 28, 2017
    Released: April 12, 2018
    JOURNALS FREE ACCESS

    Marine diatom biostratigraphy has been established for the Neogene sedimentary sequence distributed in the southern Osado Mountains area, Sado Island, Niigata Prefecture, Japan. The Neogene and Pleistocene sediments in this area are composed of the Orito, Hanyugawa, Nakayama, Nozaka, Kawachi, Kaidate and Shichiba formations in ascending order. This study examined diatoms in the Nakayama and Nozaka formations. The Nakayama Formation is composed of lower hard siliceous mudstone and upper diatomaceous mudstone, and correlated to the diatom zones NPD5B to NPD6A, ranging in age from 12.3 to 6.5 Ma. The Nozaka Formation overlies the Nakayama Formation with a glauconite bed and consists of marine massive mudstone. This formation is assigned to the subzones NPD7Ba and 7Bb, and its depositional age is estimated from 6.5 to 4.2 Ma. The age of the Orito Formation is determined to be latest Early Miocene between 17.0 and 16.7 Ma on the basis of the occurrence of the widespread Arcid-Potamid-type molluscan assemblage. The depositional age of the Hanyugawa Formation is dated by the ages of underlying Orito and overlying Nakayama formations to be early Middle Miocene ranging from 16.7 to 12.3 Ma, suggesting a long slow depositional time interval of over 4 million years.

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