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Results of X-ray fluorescence analyses of major elements for concretions, whale bones, calcite vein, and matrix , and Carbon and oxygen stable isotope ratios for the studied samples in Unosaki coast, Oga peninsula, Japan.

Version 2 2023-03-08, 02:34
Version 1 2023-02-21, 00:37
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posted on 2023-03-08, 02:34 authored by Ryusei Kuma, Shoji Nishimoto, Yusuke Muramiya, Hidekazu Yoshida

Table S1. Results of X-ray fluorescence analyses of major elements for concretions (con.), whale bones (bone), calcite vein, and matrix (wt.%). Samples of concretions and whale bone were collected from concretions 23 and 47 of Watanabe et al. (2017). LOI: loss of ignition. The low total values could be due to insufficient heating of the carbonate.


Table S2. Carbon and oxygen stable isotope ratios for the studied samples.


Funding

Development of long-term self-sealing technology of ground water pathways by learning of natural carbonate concretions

Japan Society for the Promotion of Science

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Elucidation of the early diagenetic mechanism of biogenic carbonate concretions

Japan Society for the Promotion of Science

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History

Corresponding author email address

kuma.ryusei.p8@f.mail.nagoya-u.ac.jp

Translated manuscript title

男鹿半島鵜ノ崎海岸の中新統西黒沢層・女川層中に見られる巨大鯨骨ドロマ イトコンクリーション群の形成条件

Translated authors

隈 隆成,西本昌司,村宮悠介,吉田英一

Copyright

©︎2023 The Geological Society of Japan

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    地質学雑誌/The Journal of The Geological Society of Japan

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