U–Pb geochronology of columbite-group mineral
A swarm of pegmatite dykes generally strike NW, NE, and nearly N–S (Fig. 2), with a dipping angle of 10°–85°, which formed sharp contacts with the surrounding wall-rocks.The rare-metal pegmatites belong to the beryl-type (e.g., beryl–columbite subtype) and complex-type (e.g., spodumene subtype and lepidolite subtype; Zhou et al., 2019) …
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