Lava flows of the intraplate Miocene Akaroa Volcanic Complex (AVC), Banks Peninsula, New Zealand, display a cyclical geochemical trend from picrite to benmoreite. When observed within a single stratigraphic section, flows reveal repeating patterns, or batches, of primitive to evolved magmas. Primitive flows are generally porphyritic, while the more evolved flows are consistently aphyric. Previous studies have led to a model for the AVC in which a deep reservoir (lithospheric detachment sourced) fed and replenished multiple shallow magma chambers, which then fractionated individually to produce several independently evolving magma batches. The purpose of this research is to test that model and extend it spatially across the eastern flanks of the AVC, as well as to characterize magma chamber dynamics using geochemistry and petrography. Sixty-nine samples were taken from six stratigraphically controlled transects across the eastern AVC for XRF analysis. Based on rock type and composition, samples were separated into individual batches within their respective transects. Distinct geochemical variations were observed in samples ranging from 43-59 wt. % SiO2, 0.5-7 wt. % MgO, 1-4 wt. % TiO2, and 0-270ppm V. The distinction between batches were drawn where element concentrations varied significantly within stratigraphy, further supported by petrographic distinctions (plagioclase resorbtion and sieved cores, and skeletal textures). Eleven of the sixty-nine original samples were selected for microprobe analysis of individual plagioclase, clinopyroxene, and olivine crystals. Anorthite composition in plagioclase ranged from 0.15-0.77, with both reverse and normal zoning patterns observed from core to rim. By correlating the crystallinity and textures of each flow with the bulk-rock geochemistry, this study argues that the shallow magma chambers underlying the AVC experienced cycles of magma evolution punctuated by magmatic recharge from depth. As each batch evolved, the hawaiite, benmoreite, and mugearite flows would experience crystal separation in the chamber forming a crystal mush while the residual liquid erupted aphyrically. The more primitive picrite flows, however, erupted with their phenocrysts without experiencing crystal separation, resulting in the initial, most primitive flow(s) of each cycle containing the greatest degree of crystallinity. Reverse zoning patterns coupled with resorbtion and sieve textures in the plagioclase phenocrysts within the picrite flows suggest that either the erupted flow experienced several recharge events prior to eruption, or incorporated pieces of the previous batch’s crystal mush. As such, the phenocrysts contained within the picrite flows record complex geochemical process occurring in the shallow magma chambers below the AVC.