Biogenic magnetite as a paleomagnetic recorder of the ferromanganese crust in the West Pacific
DC Field | Value | Language |
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dc.contributor.author | 김원년 | - |
dc.contributor.author | 신지영 | - |
dc.contributor.author | 김종욱 | - |
dc.date.accessioned | 2020-07-15T12:53:52Z | - |
dc.date.available | 2020-07-15T12:53:52Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2017-12-18 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/23503 | - |
dc.description.abstract | Various magnetic measurements were carried out to diagnose magnetic mineralogy of the ferromanganese crust obtained in the Magellan Seamounts, the West Pacific (~20°N). Thermal demagnetization revealed a Curie temperature of ~560oC, corresponding to (titano)magnetite. Component analysis of isothermal remanent magnetization identified a presence of two types of magnetite. Measurements of first order reverse curve showed a dominance of non-interacting single-domain magnetite, which is one of the intrinsic feature of biogenic magnetite.ponding to (titano)magnetite. Component analysis of isothermal remanent magnetization identified a presence of two types of magnetite. Measurements of first order reverse curve showed a dominance of non-interacting single-domain magnetite, which is one of the intrinsic feature of biogenic magnetite. | - |
dc.description.uri | 2 | - |
dc.language | English | - |
dc.publisher | AGU | - |
dc.relation.isPartOf | AGU 2017 | - |
dc.title | Biogenic magnetite as a paleomagnetic recorder of the ferromanganese crust in the West Pacific | - |
dc.type | Conference | - |
dc.citation.conferencePlace | US | - |
dc.citation.endPage | GP23A-0905 | - |
dc.citation.startPage | GP23A-0905 | - |
dc.citation.title | AGU 2017 | - |
dc.contributor.alternativeName | 김원년 | - |
dc.contributor.alternativeName | 신지영 | - |
dc.contributor.alternativeName | 김종욱 | - |
dc.identifier.bibliographicCitation | AGU 2017, pp.GP23A-0905 | - |
dc.description.journalClass | 2 | - |