Abstract

Combined mapping of variations in sedimentary basin fill composition and a structural interpretation is a step towards defining significant crustal scale structures and developing tectonic models in basin dominated terranes. The Bresnahan Group, part of the siliclastic Bresnahan Basin in the Capricorn Orogen was deposited in one such region. New geophysical and remote sensing datasets have been processed to interpret the basin composition and structure. Fieldwork to ground truth the interpretations, including mapping, petrophysical measurements and petrographic examination has also been completed. A northwest-trending fault in the eastern part of the Bresnahan Group has been identified as being in close proximity to compositional changes in basin fill observed on hyperspectral mineral maps. The structure has a similar orientation to a fault that cuts the older Hamersley Basin. A previously interpreted northeast-trending basin-controlling fault mapped in the west has observed differences in radiogenic comp...

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