This article deal with the petrographical and petrochemical characteristics on the cretaceous volcanic rocks in the Cheolwon basin. The volcanic rocks areas are composed of basalt in Gungpyeong Formation Basalt, Geumhaksan Andesite, Dongmakgol Tu...

http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.
변환된 중국어를 복사하여 사용하시면 됩니다.
https://www.riss.kr/link?id=T11736263
안동 : 안동대학교, 2009
2009
한국어
경상북도
v, 67 p. ; 26cm
0
상세조회0
다운로드다국어 초록 (Multilingual Abstract)
This article deal with the petrographical and petrochemical characteristics on the cretaceous volcanic rocks in the Cheolwon basin. The volcanic rocks areas are composed of basalt in Gungpyeong Formation Basalt, Geumhaksan Andesite, Dongmakgol Tu...
This article deal with the petrographical and petrochemical characteristics on the cretaceous volcanic rocks in the Cheolwon basin.
The volcanic rocks areas are composed of basalt in Gungpyeong Formation Basalt, Geumhaksan Andesite, Dongmakgol Tuff, rhyolite, Sinseo Breccia, Jijangbong Tuff, intrusive Bojangsan Andesite, acidic intrusive rocks, in ascending order. According to chemical analyses for major elements, the volcanic rocks show the calc-alkaline rock series ranged medium-K to high-K. The compositional variations of major elements show that contents of Al2O3, Fe2O3, TiO2, MnO, CaO, MgO, and P2O5 decrease with increasing SiO2, but Na2O contents are dispersed and almost constant, K2O are increased slightly. The trace element compositions and REE patterns of the volcanic rocks, which are characterized by a high LILE/HFSE ratio and enrichments in LREE, suggest that they are typical of calc-alkaline rock series of continental margin arc that produced under the subduction environment. On the discrimination diagram, the volcanic rocks discriminate as the continental margin arc. From these results, the rhyolitic magma seems to have been evolved from the basaltic andesitic magma with fractional crystallization of plagioclase, pyroxene, hornblende, biotite.
목차 (Table of Contents)