Geochemical characteristics of ridge-subduction-related granitoids
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- Kon Yoshiaki
- AIST
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- Komiya Tsuyoshi
- University of Tokyo
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- Anma Ryo
- University of Tsukuba
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- Hirata Takafumi
- Kyoto University
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- Maruyama Shigenori
- Tokyo Institute of Technology
Bibliographic Information
- Other Title
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- 中央海嶺沈み込みに伴う花崗岩の地球科学的特徴
Description
The Taitao Peninsula is the youngest site of ridge subduction in the world, where a young oceanic plate subducts, probably equivalent to the Archean subduction zone. Based on geological evidence and age and composition of the granite, we conclude that the granitic magma was generated over 10 km depth below a fore-arc region, and imply that ridge subduction played an important role in the igneous activity as a heat source. Moreover, REE patterns of granitoid are not necessary good signature of slab melting.
Journal
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- Abstracts of Annual Meeting of the Geochemical Society of Japan
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Abstracts of Annual Meeting of the Geochemical Society of Japan 57 (0), 158-158, 2010
GEOCHEMICAL SOCIETY OF JAPAN
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Keywords
Details 詳細情報について
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- CRID
- 1390001205731819648
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- NII Article ID
- 130004593256
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- Data Source
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- JaLC
- CiNii Articles
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- Abstract License Flag
- Disallowed