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- W2035366943 abstract "This paper presents the following matters about the Fe-Ti oxide minerals contained in the 75 tephras, which are about 70% of marker-tephras sedimented on Oiso Hill, 25km east of Hakone Volcano.Examination of the content, occurrence and type of Fe-Ti oxide minerals clarifies the following features:1) There is a positive correlation between the refractive indices of orthopyroxenes and the TiO2 content of titanomagnetite.2) In many cases, the TiO2 content of ferromagnetic minerals enable us to identify each tephra.Then it is shown that the tephras, which can't be identified by similar TiO2 content, can be identified by the combination of the ratios of ferromagnetic minerals, Mn/Fe and V/Ti, V/Mn and Ti/Zn.Moreover others, which can't be identified, can be distiuguished by the content of ferromagnetic minerals, that of β-phase, and the ratio of attached minerals." @default.
- W2035366943 created "2016-06-24" @default.
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- W2035366943 date "1985-01-01" @default.
- W2035366943 modified "2023-09-25" @default.
- W2035366943 title "Characteristics of Fe-Ti oxide minerals in middle and late pleistocene marker-tephras of south Kanto, central Japan." @default.
- W2035366943 cites W2330476109 @default.
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- W2035366943 doi "https://doi.org/10.4116/jaqua.24.31" @default.
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