Transient hot channels: Perpetrating and regurgitating ultrahigh-pressure, high-temperature crust–mantle associations in collision belts

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Magmatic implications of mantle wedge plumes: Experimental study (2008, background): “2) (Gerya and Stöckhert, 2006) and continental collision zones (Gerya et al., 2008-this volume).”
Subduction styles in the Precambrian: Insight from numerical experiments (2009, methodology): “At this point, the oceanic slab starts to sink into the mantle in a “two-sided subduction”mode; both the oceanic plate and the buckled continental lithospheric mantle subduct together in an asymmetric manner (cf. Gerya et al., 2008a).”
HP-UHP exhumation during slow continental subduction: Self-consistent thermodynamically and thermomechanically coupled model with application to the Western Alps (2008, background): “The real contribution of these sources at depth is unknown and one can be only confident in that ±100–150 °Cmaximal discrepancy with the data can be easily compensated in many ways (Gerya et al., 2007; Faccenda et al., 2007).”