From plutons to magma chambers: Thermal constraints on the accumulation of eruptible silicic magma in the upper crust

By C. Annen. 2009

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Lifetime and size of shallow magma bodies controlled by crustal-scale magmatism (2017, neutral): “Upper crustal magma flux (km(3)/km(2) per year) 10 10 10 Thermally mature crust Undisturbed geotherm Annen (2009)”
Vertically extensive and unstable magmatic systems: A unified view of igneous processes (2017, neutral): “Efficient melt extraction in these systems, however, requires either maintenance of upper crustal mush zones at high temperatures (high magma influx rates) and/or sufficiently low melt viscosities (high dissolved volatile contents; ( 83, 103 )).”
Physical controls and depth of emplacement of igneous bodies: A review (2011, background): “These different growth sequences will lead to radically different thermal evolutions, and thus to extremely different relative amounts of residual melt from incomplete crystallization of the pulses and of partial crustal melt (Annen et al., 2008; Annen, 2009b, this issue).”
Multiscale magmatic cyclicity, duration of pluton construction, and the paradoxical relationship between tectonism and plutonism in continental arcs (2011, background): “…Costa, 2007; Michel et al., 2008; Costa, 2008), the new data initiated vigorous debate on upper crustal plutonic systems, the relation between magma chamber and pluton dynamics, and the relation between plutonism and volcanism (Glazner et al., 2004; Bachmann et al., 2007; Annen, 2009; Annen, 2011).”