On the Nature of Remanence in the 1985 Andesitic Pumice with Self-Reversed Magnetization from Nevado del Ruiz, Colombia
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概要
- 論文の詳細を見る
The magnetic remanence of the andesitic pumice of the Nevado del Ruiz 1985 eruption has the multi-component nature. The major normal component behavior is due to the titanomagnetite phase with variable chemistry. The major reverse component has a peak demagnetization and acquisition range between 200°-225℃ but no such mineral phase could be detected. The titanomagentite phase contributes to the major normal component and has probably no relation to the reverse magnetization.
- 北海道大学 = Hokkaido Universityの論文
著者
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Gautam Pitambar
北海道大学理学部地質学鉱物学教室
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Gautam P
Hokkaido Univ. Sapporo Jpn
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Gautam Pitambar
Coe For Neo-science Of Natural History Graduate School Of Science Hokkaido University
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Gautam Pitambar
Hokkaido Univ.
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Gautam Pitambar
Division Of Earth And Planetary Sciences Graduate School Of Science Hokkaido University
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