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http://dx.doi.org/10.7854/JPSK.2014.23.4.325

A Petrological Study of the Mudeungsan Tuff Focused on Cheonwangbong and Anyangsan  

Jung, Woochul (Department of Energy and Resources Engineering, Chonnam National University)
Kil, Youngwoo (Department of Energy and Resources Engineering, Chonnam National University)
Huh, Min (Faculty of Earth Systems and Environmental Sciences, Chonnam National University)
Publication Information
The Journal of the Petrological Society of Korea / v.23, no.4, 2014 , pp. 325-336 More about this Journal
Abstract
Even though Mesozoic Mudeungsan tuff, located within Neungju Basin, has been named several rock names, it should be named as Mudeungsan tuff due to several evidences, such as fiamme, welded texture and rock fragments in the Mudeungsan tuff. Volcanic eruption boundary between the Cheonwangbong and Anyangsan areas is not clear, but petrochemical and mineral chemical evidences with different ages indicate clear petrological boundary between Cheonwangbong and Anyangsan. The Mudeungsan tuffs from Cheonwangbong and Anyangsan is welded crystal tuff with dacitic composition and were generated from cogenetic calc-alkaline magma in the volcanic arc environment. Geochemical events indicate that magma beneath Cheonwangbong was seems to have been evolved from the magma beneath Anyangsan due to fractional crystallization dominated by plagioclase.
Keywords
Mudeungsan tuff; welded texture; devitrification; Cheonwangbong; Anyangsan;
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