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Solander Trough is located offshore and south of Fiordland, New Zealand, adjacent to the geologically young Pacific-Australian plate boundary. Petroleum industry exploration was restricted to the near-shore. This thesis presents the first stratigraphic analysis of Solander Trough south of ~46.5°S, using 2D seismic reflection data acquired and processed onboard the R/V Marcus G. Langseth in 2018 (voyage MGL1803). The only pre-existing high-quality line, which was acquired onboard the R/V Maurice Ewing during voyage EW9601a in 1996, was reprocessed.  The study area is divided into northern and southern sub-basins by Tauru High. Four megasequences and eight sequences are identified in the northern sub-basin (SLN). In the southern sub-basin (SLS), three megasequences and seven sequences are mapped. Biostratigraphy from the Parara-1 exploration well enabled age determination in the northern sub-basin. High resolution (~10 m) swath bathymetry data collected along seismic reflection lines provide insight into modern sedimentary processes.  Solander Trough formed in the Eocene, but most sediment is young (

A seismic stratigraphic model for understanding the sedimentary and tectonic evolution of Solander Trough, offshore Fiordland, New Zealand