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Format

EDI

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file-only

Publisher-reported update

2017-01-26

Results of a ground geophysical survey near the eastern limit of the Shield to Selwyn transect extends our knowledge of the spatial distribution of Paleozoic and Proterozoic sequences. Subsurface faulting in the center of the transect, just east of a large gravity anomaly, has created a large deformation zone traceable to mid-crustal depths.

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