書誌事項
- タイトル別名
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- Behavior of Magmatic Volatiles in Volcanic Eruptions Based on Glass Inclusion Analysis
- カザン フンカ ニ オケル マグマチュウ ノ キハツセイ ブッシツ ノ キョド
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The role of volatiles in volcanic eruptions was reviewed in view of the measured concentration of volatiles in glass inclusions in phenocrysts. Since the amount of volatiles in a glass inclusion is very small (typically ranging from 10-11 to 10-8 mol), a special attention has to be paid to the extraction techniques and analytical methods. Advantage and disadvantage were discussed for the four extraction/analytical techniques; (1) vacuum heating methods, (2) electron-probe microanalysis, (3) ion-probe microanalysis, and (4) infrared spectrometry. The glass inclusion analyses suggest that (1) the volatile concentration in a magma of an early stage of eruption is significantly higher than that of the later stage, (2) a gas phase (H2O, CO2 and SO2) accumulates in a magma chamber during its residence at a shallow depth, and (3) accumulation of data on volatiles in magmas contributes to the understanding of the effect of volcanic eruptions on the climatic changes and evolution of atmosphere.
収録刊行物
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- 火山.第2集
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火山.第2集 34 (4), 275-293, 1989
特定非営利活動法人 日本火山学会
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詳細情報 詳細情報について
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- CRID
- 1390282681099300608
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- NII論文ID
- 110002996512
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- NII書誌ID
- AN10512786
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- ISSN
- 04534360
- 24330590
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- NDL書誌ID
- 3649762
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可