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Metamorphic Evolution of the Ogcheon Metamorphic Belt: Review of Recent Studies and Remaining Problems  

조문섭 (서울대학교 자연과학대학 지구환경과학부)
김현철 (서울대학교 자연과학대학 지구환경과학부)
Publication Information
The Journal of the Petrological Society of Korea / v.11, no.3_4, 2002 , pp. 121-137 More about this Journal
Abstract
Metamorphic evolution of the Ogcheon metamorphic belt has been studied by many investigators for the past few decades. P-T conditions of the Ogcheon metamorphic belt were estimated as 4.2-9.4 kbar and $490-630^{\circ}C$, corresponding to the medium-pressure type. In addition, the clockwise P-T-t path suggests a crustal-thickening event in association with the formation of thrust nappes. However, some details on deformation and orogeny of the Ogcheon metamorphic belt have been ambiguous yet. Although the metamorphic age has been also equivocal, recent isotopic studies strongly suggest that the peak metamorphism in the Ogcheon metamorphic belt has occurred at ca. 300-280 Ma between Late Carboniferous and Early Permian. It is thus inferred that the Ogcheon metamorphic belt and the Taebaegsan basin have evolved as separate terranes and that both were sutured at ca. 250-220 Ma. These results are partly in contrast with those of previous workers and require a revised framework for tectonic evolution of the Ogcheon belt. In addition, it is likely that the Ogcheon belt is correlative with the Hida marginal belt and the Hida metamorphic belt.
Keywords
Ogcheon belt; Ogcheon metamorphic belt; orogeny; regional metamorphism; P-T-t path;
Citations & Related Records
Times Cited By KSCI : 4  (Citation Analysis)
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