Tectonics and Source Regions. <br>Comparison of Proterozoic and Phanerozoic rift-related basaltic-granitic magmatism (I. Haapala, O. Tapani Rämö, S. Frindt). <br>TTGs and adakites: are they both slab melts? (K.C. Condie). <br>Ilmenite, magnetite, and peraluminous Mesoproterozoic anorogenic granites of Laurentia and Baltica (J. Lawford Anderson, J. Morrison). <br>Source regions of granites and their links to tectonic environment: examples from the western United States (E.Y. Anthony).<br>Source contributions to Devonian granite magmatism near the Laurentian border, New Hampshire and Western Maine, USA (P.B. Tomascak et al.). <br>Petrogenesis of the Paleoproterozoic rapakivi A-type granites of the Archean Carajás metallogenic province, Brazil (R. Dall'Agnol). <br>The granite-upper mantle connection in terrestrial planetary bodies: an anomaly to the current granite paradigm? (B. Bonin, J. Bébien). <br>Continental rift systems and anorogenic magmatism (J.W. Sears, G.M. St. George, J.C. Winne). <br>Petrologic Processes. <br>Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith, California: nature, origin, and relations with the hosts (B. Barbarin). <br>Pervasive assimilation of carbonate and silicate rocks in the Hortavær igneous complex, north-central Norway (C.G. Barnes et al.). <br>Quartz and feldspar zoning in the eastern Erzgebirge volcano-plutonic complex (Germany, Czech Republic): evidence of multiple magma mixing (A. Müller et al.). <br>Prolonged postcollisional shoshonitic magmatism in the southern Svecofennian domain – a case study of the Åva granite–lamprophyre ring complex (O. Eklund, A. Shebanov). <br>Origin of chemically distinct granites in a composite intrusion in east-central Sweden: geochemical and geothermal constraints (A. Lindh). <br>The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts (R.L. Linnen). <br>Fractionated Granites and Pegmatites. <br>Granitic pegmatites: an assessment of current concepts and directions for the future (D. London).<br>The Greer Lake leucogranite, Manitoba, and the origin of lepidolite-subtype granitic pegmatites (P. Cerný et al.).<br>Textural and chemical evolution of a fractionated granitic system: the Podlesí stock, Czech Republic (K. Breiter et al.). <br>Petrological and geochemical evolution of the Kymi stock, a topaz granite cupola within the Wiborg rapakivi batholith, Finland (I. Haapala, S. Lukkari). <br>Sn-polymetallic greisen-type deposits associated with late-stage rapakivi granites, Brazil: fluid inclusion and stable isotope characteristics (J.S. Bettencourt et al.).<br>Solubility of cassiterite in evolved granitic melts: effect of T, fO<INF>2</INF>, and additional volatiles (P. Bhalla et al.).