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corresponds to the northern Chuandian block, display large- scale , pronounced and continuous mid- crustal LVZs (Figs 12b, c and f). These LVZs become less clear towards the Songpan-Ganzi fold belt to the east ...
–relamination stage was followed by crustal - scale Early Carboniferous doming when the lower crustal rocks were exhumed to middle crust levels along vertical deformation zones (Štípská et al., 2004, 2012 ...
to thermochemical mantle plumes (White & McKenzie, 1989; Campbell & Griffiths, 1990; Campbell, 2005). Evidence for uplift and lithospheric extension prior to the onset of volcanism is a common feature of CFBs ...
, causing upwelling of asthenospheric mantle and large- scale crustal melting (Coney & Reynolds, 1977; Humphreys, 1995; Humphreys et al., 2003). Dewatering of the flat-slab may have metasomatized ...
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