The Cheslatta Lake Suite: Miocene Mafic, Alkaline Magmatism in Central British Columbia1
Color profile: Disabled Composite Default screen 697 The Cheslatta Lake suite: Miocene mafic, alkaline magmatism in central British Columbia1 Robert G. Anderson, Jonah Resnick, James K. Russell, G.J. Woodsworth, Michael E. Villeneuve, and Nancy C. Grainger Abstract: New mapping, mineralogical, and geochemical studies help characterize late Tertiary primitive, alkaline, sodic basanite, alkali olivine basalt, transitional basalt, and diabase in the Nechako River, Whitesail Lake, and McLeod Lake map areas of central British Columbia and distinguish the Miocene Cheslatta Lake suite. The suite encompasses scattered erosional remnants of topographically distinct, columnar-jointed, olivine-phyric basalt and diabase volcanic necks, dykes, and associated lava flows north of the Anahim volcanic belt and west of the Pinchi Fault. Volcanic cen- tres at Alasla Mountain and at Cutoff Creek, near Cheslatta Lake, are proposed as type areas. Olivine, plagioclase, and pyroxene phenocrysts, megacrysts, and (or) xenocrysts; common ultramafic xenoliths; and rare but significant plutonic and metamorphic xenoliths are characteristic. Basanite, transitional basalt, and alkali olivine basalt groundmass contain plagioclase, clinopyroxene, Fe-Ti oxides, feldspathoid, olivine, and apatite. The Cheslatta Lake suite is characterized by its alkaline character, olivine-rich (>10 wt.%) normative mineralogy, and silica-undersaturated nature (>1 wt.% norma- tive nepheline; hypersthene-normative rocks are uncommon). Mg numbers vary between 72–42. Some samples encom- pass
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