Ocean Island Basalts in Polynesia, South Pacific
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- KOGISO Tetsu
- Department of Interdisciplinary Environment, Graduate School of Human and Environmental Studies, Kyoto University
Bibliographic Information
- Other Title
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- 南太平洋,ポリネシアの海洋島玄武岩
- The 100s : Significant Exposures of the World(No. 9)Ocean Island Basalts in Polynesia, South Pacific : Products of Magmatism Caused by Superplume Activity
- Products of Magmatism Caused by Superplume Activity
- ―スーパープルームによって引き起こされた火成活動の産物―
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Abstract
Polynesia in the South Pacific is the location of a cluster of hotspots associated with a superswell. A large-scale seismic low-velocity anomaly found in the mantle beneath Polynesia indicates the existence of a superplume, which is responsible for the formation of the hotspot cluster and superswell. Basaltic lavas that erupted at volcanic islands in Polynesia are characterized by a large diversity of radiogenic isotopic ratios. The geochemical characteristics of Polynesian basalts are consistent with the involvement of subducted crustal material in the source mantle, suggesting that Polynesian basalts are products of the large-scale recycling of subducted crustal material facilitated by superplume activity.
Journal
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- Journal of Geography (Chigaku Zasshi)
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Journal of Geography (Chigaku Zasshi) 122 (3), 539-545, 2013
Tokyo Geographical Society
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Details 詳細情報について
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- CRID
- 1390282679215270912
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- NII Article ID
- 130003373654
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- NII Book ID
- AN00322536
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- ISSN
- 18840884
- 0022135X
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- NDL BIB ID
- 024773177
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- Text Lang
- ja
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed