Abstract
The Inzie Head gneisses of the NE Dalradian are syntectonic metapelitic schollen migmatites containing numerous sill-like bodies of granite and diorite. Leucosomes with clear evidence of melt-present crystallization exhibit a wide variety of segregation structures. Initial in situ melting occurred within, or at the margins of, fertile metasedimentary horizons and was strongly controlled by variations in bulk-composition. Intergranular melt-pockets coalesced into thin (
Original language | English |
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Pages (from-to) | 59-72 |
Number of pages | 13 |
Journal | Scottish Journal of Geology |
Volume | 37 |
Issue number | 2 |
DOIs | |
Publication status | Published - 2001 |