Metamorphic zones, terranes and lithologic associations provide a subdivision of the lithologically monotonous Otago Schist on a 10 to 50 kilometer scale. In this study, form line maps of schist foliation have been used to construct a provisional structural thickness map of the Otago Schist that allows a more detailed (1-5 km scale) subdivision of the entire schist. The map shows the macroscopic thickness of schist measured orthogonal to dominant foliation, relative to the datum of the Caples-Rakaia terrane boundary. The structural thickness map provides a new spatial reference frame for the Otago Schist that depicts the differing levels of exhumation of penetratively deformed metamorphic rocks. The structural thickness parameter shows a good correlation with metamorphic grade, white mica grain size, and K-Ar and Ar-Ar ages, thus justifying the simplifying assumptions behind the map's construction. The map reveals several hitherto little-highlighted features including along- and across-strike correlations, interference patterns between Mesozoic and Cenozoic macroscopic folds, net displacement across known and inferred major faults, and relative structural position of mesothermal gold deposits.
CITATION STYLE
Mortimer, N. (2003). A provisional structural thickness map of the Otago Schist, New Zealand. American Journal of Science, 303(7), 603–621. https://doi.org/10.2475/ajs.303.7.603
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