F. J. Turner
Abstract
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Isolated blocky outcrops of schist in central Otago, New Zealand, are elongated and aligned in a northwest direction which parallels the lineation of the schist, and are thought to reflect the effect of differential weathering controlled by the rock fabric.
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Isolated blocky outcrops of schist in central Otago, New Zealand, are elongated and aligned in a northwest direction which parallels the lineation of the schist, and are thought to reflect the effect of differential weathering controlled by the rock fabric.
Key concepts: Schist, Lineation, Geology, Outcrop, Geochemistry, Paleontology, Metamorphic rock, Tectonics