| タイトル | The Ivrea zone as a model for the distribution of magnetization in the continental crust |
| 著者（英） | Wasilewski, P.; Fountain, D. M. |
| 著者所属（英） | Montana Univ.|NASA Goddard Space Flight Center |
| 発行日 | 1982-04-01 |
| 言語 | eng |
| 内容記述 | Units are identified within the Ivrea zone of northern Italy exhibiting magnetic susceptibilities greater than 0.0005 cgs, saturation magnetization values above 0.009 emu/cu cm, and Curie points as high as 570-580 C. Amphibolites from the granulite-amphibolite facies transition, and the mafic-ultramafic granulite facies lithologies exhibit high values of initial susceptibility and saturation remanence, are laterally continuous, and may be considered as a deep crustal source for long-wavelength anomalies in low-geothermal gradient areas. Evidence is presented which suggests that such mafic-ultramafic bodies as those exposed in the Toce valley were synmetamorphic additions to the base of the crust. |
| NASA分類 | GEOSCIENCES (GENERAL) |
| レポートNO | 82A30799 |
| 権利 | Copyright |
| URI | https://repository.exst.jaxa.jp/dspace/handle/a-is/410899 |
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