Petrography of the Donkerhuk granite, photos from the final day of the Granulites & Granulites post-conference excursion. This granite is emplaced along the boundary between Southern and the Central Zones of the Damara Belt, and shows evidence for the sheeted emplacement of small batches of melt
1Donkerhuk granite landscape, stop 1 (W Donkerhuk)
2Pavement outcrop, stop 1 (W Donkerhuk) Donkerhuk granite with narrow aplitic and pegmatitic veins trending NW-SE
3Pavement outcrop, stop 1 (W Donkerhuk) Thicker pegmatitic vein in Donkerhuk granite
9Texture detail, stop 2 Fabric defined by indistinct trails of mafic minerals and weak shape fabric of feldspars
10Texture detail, stop 2 Fine-grained granite
11Stop 2 (Otjimbingwe) Loose blocks of heterogeneous foliated granite with mafic schlieren
12Pavement outcrop, stop 2 Heterogeneous banded Donkerhuk granite. Discordant pegmatite at top of photo
13Texture detail, stop 2 Detail of biotite-rich schlieren with metamorphic texture
14Texture detail, stop 2 Dark band in partly weathered outcrop. Igneous-textured feldspar notable in central leucocratic band
15Texture detail, stop 2 Granite with thin biotite schlieren
16Texture detail, stop 2 Weakly foliated biotite granite with scattered small K-feldspar phenocrysts, from homogeneous leucocratic layer
17Pavement outcrop, stop 2 Discontinuous veined metasedimentary rafts and schlieren
18Pavement outcrop, stop 2 Depression in outcrop reveals steep orientation of banding. View towards SW
19Pavement outcrop, stop 2 Rotated and sheared portion of partly-digested metasedimentary raft
20Pavement outcrop, stop 2 Veined xenolith of psammitic metasediment. Note that at least some of the veining is truncated by the fabric wrapping the xenolith
21Texture detail, stop 2 Late, discordant vein of biotite pegmatite
22Pavement outcrop, stop 2 Lower contact of fine-grained leucogranite forming a late, discordant subhorizontal sheet