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http://dx.doi.org/10.5467/JKESS.2013.34.2.109

Petrochemical Characteristics of the Duibaejae Volcanic Rocks from Goseong, Gangwon-do, Korea  

Kim, Hwa Sung (Taebaek Mechanical Technical High School)
Kil, Youngwoo (Department of Energy and Resources Engineering, Chonnam National University)
Lee, Moon Won (Division of Science Education, Kangwon National University)
Publication Information
Journal of the Korean earth science society / v.34, no.2, 2013 , pp. 109-119 More about this Journal
Abstract
Duibaejae basalts from Goseong, Gangwon-do, are divided into the lower basalt and the upper basalt depending on the properties, such as occurrence, mineral compositions, and major and trace compositions of the basalts. The lower basalts have characteristics of agglomerate rocks as well as contain, crustal and mantle xenoliths, and olivine, pyroxene, and plagioclase xenocrysts. The upper basalts with columnar joints contain relatively more mantle xenolith and olivine xenocryst than the lower basalts. The major and trace element compositions suggest that the composition of the upper basalts is close to primary magma composition. Enrichment and depletion patterns of the trace and the rare-earth elements of the lower basalts are similar to those of the upper basalts, whereas the lower basalts are more LREE enriched than the upper basalts. The source magmas of the lower and upper basalts from Duibaejae volcanic edifice were generated from about 0.8-1.2% and 3.7-4.0% batch melting of garnet peridotite, respectively. The abundance of granite xenolith, and plagioclase and quartz xenocrysts with reaction rim indicates that the lower basalts, compared with upper basalts, might have been assimilated with the crustal materials during ascending to surface.
Keywords
Duibaejae volcanic edifice; garnet peridotite; batch melting; magma;
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Times Cited By KSCI : 4  (Citation Analysis)
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