| Автор | Johnson, A. C. |
| Автор | Swain, C. J. |
| Дата выпуска | 1995 |
| dc.description | Aeromagnetic anomaly data collected between 67°S and 70°S crossing the Antarctic Peninsula and adjacent offshore areas show a prominent NW‐SE trend in the magnetic fabric. Apparent lateral offsets, previously recognized in the Pacific Margin Anomaly, have been mapped in detail and are shown to be much smaller than previously suggested. A 35 km wide zone of subdued magnetic anomalies at the Western edge of the Pacific Margin Anomaly, bounded by these apparent offsets, is interpreted as a downfaulted block of the mafic‐intermediate batholith thought to be responsible for the Pacific Margin Anomaly. The trends of both fracture zones and magnetic lineaments strongly support the link between faulting in the Antarctic Peninsula magmatic arc and offshore tectonics. |
| Формат | application.pdf |
| Копирайт | Copyright 1995 by the American Geophysical Union. |
| Тема | Geomagnetism and Paleomagnetism |
| Тема | Geomagnetism and Paleomagnetism: Spatial variations (all harmonics and anomalies) |
| Тема | Structural Geology |
| Тема | Structural Geology: Remote sensing |
| Тема | Tectonophysics |
| Тема | Tectonophysics: Plate boundary—general |
| Тема | Geographic Location |
| Тема | Information Related to Geographic Region: Antarctica |
| Название | Further evidence of fracture‐zone induced tectonic segmentation of the Antarctic Peninsula from detailed aeromagnetic anomalies |
| Тип | article |
| DOI | 10.1029/95GL00812 |
| Electronic ISSN | 1944-8007 |
| Print ISSN | 0094-8276 |
| Журнал | Geophysical Research Letters |
| Том | 22 |
| Первая страница | 1917 |
| Последняя страница | 1920 |
| Аффилиация | Johnson, A. C.; British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK |
| Аффилиация | Swain, C. J.; British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK |
| Выпуск | 14 |
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