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http://dx.doi.org/10.22807/KJMP.2022.35.3.173

Petrological Study on the Mantle Xenolith from Dongsuak Crater, Jeju Island  

Kil, Youngwoo (Department of Energy and Resources Engineering, Chonnam National University)
Hong, Sei Sun (Climate Change Response Research Division, Korea Institute of Geoscience and Mineral Resources)
Lee, Choon Oh (Geologic Hazards Research Division, Korea Institute of Geoscience and Mineral Resources)
Ahn, Ung San (World Heritage Office, Jeju Special Self-Governing Provincial Government)
Publication Information
Korean Journal of Mineralogy and Petrology / v.35, no.3, 2022 , pp. 173-182 More about this Journal
Abstract
Dongsuak crater, located in the mid-mountainous region of Jeju Island, is located at an altitude of about 700 m, and the newly discovered Dongsuak spinel peridotites was enclosed in Dongsuak alkaline basalt. The Dongsuak spinel peridotites are composed of olivine, orthopyroxene, clinopyroxene, and spinel with porphyroclastic texture under the an equilibrium state. The variations of mineral major and trace compositions indicates that the Dongsuak spinel peridotites originate at depth from 66 to 88 km under an equilibrium temperature of about 960℃~1068℃. The Dongsuak spinel peridotites have been undergone about 1~3% fractional melting. The LREE-enriched characteristics indicate that the Dongsuak spinel peridotites have been undergone cryptic metasomatism by silicate melt without new minerals.
Keywords
Dongsuak; Spinel peridotite; Mantle xenolith;
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