Petrophysical data and opaque mineralogy of high-grade and retrogressed lithologies: implications for the interpretation of aeromagnetic anomalies in Northern Vestranden, Central Norway
A regional aeromagnetic anomaly centred around Roan, Northern Vestranden, Western Gneiss Region, Central Norway, is caused by the presence of high-grade orthogneisses and metabasites with 1–2 vol% magnetite. Granulites are surrounded, and partly covered by amphibolite-facies rocks, which consist of...
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Veröffentlicht in: | Tectonophysics 1991-06, Vol.192 (1), p.21-31 |
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Format: | Artikel |
Sprache: | eng |
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