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The Ogcheon metamorphic belt in central Korea has been interpreted to be the eastward extension of the Nanhua Basin (aulacogen) of southeast China. In this paper, comparisons are made between the two regions based on stratigraphic, thermal-tectonic and other considerations. From this comparison, correlation of geological events between the Nanhua Basin and Ogcheon metamorphic belt are at best equivocal...
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