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Results of analyses from the tuffs in the Pliocene Mukaiyama Formation, Sendai area, Japan.

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posted on 2023-08-08, 11:32 authored by Haruka Kusakawa, Reishi Takashima

Table S1. Heavy mineral occurrences and abundances in the studied tuffs from the Mukaiyama Formation. ◎:abundant, 〇: common, △: rare, ×: absent. Red symbols for zircon indicate that most zircon grains are bright red in color.

Table S2. Results of LA–ICP–MS U–Pb analyses of zircon grains from the studied tuffs. Each analysis was performed on a different grain.

Table S3. Major and trace element compositions of apatite from the studied tuffs, analyzed using wavelength disper  sive spectrometry on an electron probe microanalyser (JEOL 8530F). Each analysis was performed on a different grain.

History

Corresponding author email address

reishi.takashima.a7@tohoku.ac.jp

Manuscript title (in Japanese)

アパタイト微量元素組成を用いた仙台地域の鮮新統・向山層の層序と凝灰岩 の対比

Authors (in Japanese)

草川 遥,髙嶋礼詩

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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