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Newly found granulites from the western part of Sefuri Mountains, North Kyushu
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- Owada Masaaki
- Department of Earth Sciences, Yamaguchi University
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- Hada Ryoichi
- Department of Earth Sciences, Yamaguchi University
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- Yada Jun
- Department of Earth Sciences, Yamaguchi University Present address: Kaminaga Co. Ltd.
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- Nakamura Mai
- Department of Earth Sciences, Yamaguchi University
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- Osanai Yasuhito
- Department of Evolution of Earth Environments, Kyushu University
Bibliographic Information
- Other Title
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- 新たに見い出された北部九州,脊振山地西部のグラニュライト相変成岩類
- アラタ ニ ミイ ダサレタ ホクブ キュウシュウ セフリ サンチ セイブ ノ グラニュライトソウ ヘンセイガンルイ
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Description
Newly found metamorphic block (c. 3 km × 1 km) within the Cretaceous granitic rocks in the Mt. Uki-dake area, northwest Kyushu, consists of two-pyroxene rock, garnet-orthopyroxene-cordierite gneiss and orthopyroxene tonalite being associated with layers or lenses of calcsilicate and ultramafic rocks. Geothermobarometries yield granulite-facies metamorphic conditions, approximately at 800 to 900°C and 400 to 500 MPa. On the basis of the similarity of the lithology and the metamorphic conditions, we propose that the present granulite-facies block and the neighboring amphibolite-facies block at the western part of Sefuri Mountains can be correlated to the high-grade sequence of the Higo metamorphic terrain in west-central Kyushu.<br>
Journal
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- The Journal of the Geological Society of Japan
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The Journal of the Geological Society of Japan 111 (1), 50-53, 2005
The Geological Society of Japan
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Keywords
Details 詳細情報について
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- CRID
- 1390001206237469056
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- NII Article ID
- 110003024633
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- NII Book ID
- AN00141768
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- ISSN
- 13499963
- 00167630
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- NDL BIB ID
- 7234628
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- Text Lang
- ja
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- Data Source
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- JaLC
- NDL Search
- Crossref
- CiNii Articles
- OpenAIRE
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- Abstract License Flag
- Disallowed