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  3. Vol.1 The Academic Pilgrimage to Sustainable Social Development

Petrogenesis of Plutonic Rocks in the Ryukyu Arc, Japan

http://hdl.handle.net/11266/6626
http://hdl.handle.net/11266/6626
51eeb827-8f09-4daf-8d10-6c987ddc370d
名前 / ファイル ライセンス アクション
07_Kawano_p137-169.pdf 07_Kawano_p137-169.pdf (2.8 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2019-05-15
タイトル
タイトル Petrogenesis of Plutonic Rocks in the Ryukyu Arc, Japan
言語 en
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_3248
資源タイプ book part
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
著者 川野, 良信

× 川野, 良信

en Kawano, Yoshinobu

ja 川野, 良信

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内容記述タイプ Abstract
内容記述 The Cretaceous to Neogene plutonic rocks are distributed over the eight
islands of the Ryukyu Arc, namely Amami-O-shima, Kakeroma-jima,
Uke-jima, Tokuno-shima, Okinoerabu-jima, Okinawa-jima, Tonaki-jima,
and Ishigaki-jima. These plutonic rocks can be categorized based on their
petrological characteristics and active periods into four groups: early
Cretaceous (EC), late Cretaceous (LC), Poleogene (PG), and Neogene
(NG). The initial Sr isotopic ratio of the PG and NG groups increased,
whereas the initial Nd isotopic ratio decreased with increasing aluminum
saturation index (ASI), thereby indicating the influence of the upper crustal
material. The LC group also exhibits a high initial Sr isotopic ratio, a low
initial Nd isotopic ratio, and high ASI, presuming that the source magma
reacted with the upper portion of the crustal material. Such reactions with
the upper crustal material were observed to have occurred three times between
Cretaceous and Neogene, and these events may have been caused by
changes in the tectonics of the Ryukyu Arc.
言語 en
書誌情報 en : The Rissho International Journal of Academic Research in Culture and Society

巻 1, p. 137-169, 発行日 2018-03-25
著者版フラグ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
出版者
出版者 Rissho University
言語 en
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