Palaeomagnetic remanences in high‐grade metamorphic rocks of the Everest region: indication for Late Miocene crustal doming
SUMMARY High‐grade metamorphic rocks of the upper amphibolite to granulite facies in the Higher Himalayan crystalline (HHC) were studied for their appropriateness for palaeomagnetic investigations. Sampling and fieldwork was accomplished on a south–north transect at ∼87°E in the Khumbu region south...
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Veröffentlicht in: | Geophysical journal international 2011-08, Vol.186 (2), p.551-566 |
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Sprache: | eng |
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