Mangerite magmatism associated with a probable Late-Permian to Triassic Hongseong–Odesan collision belt in South Korea

Lile Felsic
DOI: 10.1016/j.gr.2005.06.005 Publication Date: 2006-01-10T12:08:03Z
ABSTRACT
Abstract The Odesan area in the eastern Gyeonggi Massif, South Korea, consists principally of migmatitic and porphyroblastic gneisses intruded by mangerite. Mafic mangerites with SiO 2 contents from 52.40 to 54.20 wt.% have higher FeO* + MgO (14.98–18.28 wt.%) and CaO contents (5.80–7.84 wt.%) but lower total alkali contents (4.74  2 O + K 2 O  2 2 O + K 2 O
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