Environmental Engineering Reference
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FIGURE 4 Ichnological characterization of a submarine canyon margin, Early Miocence strata of
Northland, New Zealand. (A) General exposure of the canyon margin sequence boundary (yellow
arrows) at Tirikohua Point. (B) Firmground Rhizocorallium ( Rh ) attributable to the Glossifungites
Ichnofacies. The omission suite is associated with the sequence boundary shown in (A) excavated
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