The Source of Fine-Grained ‘Magnetite’ in Sediments
Dados Bibliográficos
| ID | 12265643 |
|---|---|
| Autores | Frank Oldfield (0000-0002-3060-2411, University of Liverpool, autor correspondente) |
| Ano | 1992 |
| Volume | 2 |
| Fascículo | 2 |
| Páginas | 180-182 |
| Data de publicação | 1992-07-01 |
| Peer Reviewed | Sim |
| Open Access | Sim |
| Tipo | ARTICLE |
| Periódico | The Holocene (JOURNAL) |
| Identificadores do periódico | ISSN: 0959-6836 • E-ISSN: 1477-0911 |
| Editora | SAGE Publishing (PUBLISHER • US) |
| DOI | 10.1177/095968369200200209 |
| OpenAlex | W1878737002 |
| Idioma | EN |
| Citações recebidas | 4 |
| Referências citadas | 29 |
Extensive study of the magnetic properties of soils and sediments by both earth scientists and biomagnetists has failed to establish the extent to which fine-grained magnetic components in the sediments' are dominated by detrital or by authigenic bacterial contributions. The question is of considerable importance to workers in a wide range of research fields. This article aims to encourage a balanced and explicit debate between biomagnetists and ‘environmental’ magnetists since, at present, they are tending to interpret their results within mutually exclusive frames of reference
Authigenic · Earth science · Environmental magnetism · Geochemistry · Magnetite · Range (aeronautics · Sediment · Geology and Paleoclimatology Research · Geomagnetism and Paleomagnetism Studies · Magnetic and Electromagnetic Effects · Geology · Paleontology
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Partly pedogenic origin of magnetic variations in Chinese loess
Formation of ultrafine-grained magnetite in soils
Occurrence of magnetic bacteria in soil
Characterisation of soils by mineral magnetic measurements
The record of land use change and soil erosion in the late Holocene sediments of the Petit Lac d'Annecy, eastern France
| Obras citantes distintas | 4 |
|---|---|
| Citações por ano | 0,21 |
| Intervalo de citações | 2007 - 2015 (9) |
| Velocidade de citação | historical |
| Altamente citado | Não |
| Tipos de citação | Neutras: 4 |