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- W2255920199 abstract "Volcanogenic sedimentary rocks such as Unbangsan formation and tuffaceous rocks of Yucheon Group are distributed in the Geumsan area (Namhae), and the Cretaceous granitic rocks had intruded into the group. The granitic rocks are divided into granodiorite and so-called Geumsan granite from their occurrence and mineral compositions. The Geumsan granite, intruding into the granodiorite, is characterized by hypersolvus, micrographic granite. It seems like that the Geumsan granite was solidified from the H₂O-saturated, K-enriched magma under the highly super-cooled condition due to decompression. The pressure condition of the minimum melt composition of the granite is assumed to be 0.5∼2 kbar, indicating the granite is shallow-emplaced pluton. This is in good harmony with observed features of the miarolitic cavity structure and micrographic texture. Comparing the characteristics of the micrographic granites among the Geumsan, Masan, Kimhae and Busan areas, those between the Geumsan and Busan areas are similar, except the plagioclase content. The formation and the quantity of the micrographic texture in the granitic rocks seem likely to have more related to the physical factors such as intruding and cooling rates of granitic magma as well as structural condition (fault, fracture etc.), rather than the emplacing depth of the magma." @default.
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- W2255920199 date "1997-01-01" @default.
- W2255920199 modified "2023-09-24" @default.
- W2255920199 title "남해지역 금산 미문상화강암에 대한 암석기재" @default.
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