GEOLOGICAL AND PETROLOGICAL CHARACTERS OF THE PLUTONIC ROCKS IN THE LUNCKERYGGEN-BRATTNIPENE REGION, SOR RONDANE MOUNTAINS, EAST ANTARCTICA
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概要
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Plutonic rocks in the Lunckeryggen-Brattnipene region, Sor Rondane Mountains are divided into the older (late Proterozoic) and younger (early Paleozoic) intrusive rocks. The older intrusive rocks are composed of tonalite, quartz diorite, granodiorite and small sheet-like granite, granodiorite and trondhjemite. They have a gneissose structure and show a concordant relation to the surrounding metamorphic rocks. On the basis of their field occurrences, it seems that they have intruded before or during the period of the regional mylonitization. The younger intrusive rocks are composed of syenite, quartz syenite and granite. They occur as stocks or dikes intruding discordantly into the surrounding rocks. The older intrusive rocks give low values of magnetic susceptibility in general, while most of the younger intrusive rocks give high magnetic values in Lunckeryggen and the neighborhood. Magnetic values on the discordant granites of the younger stage decrease northward in the Lunckeryggen-Brattnipene region. Moreover, the magnetic values of the younger intrusive rocks in the western Sor Rondane Mountains show a possibility that the lateral variation extends farther west from the Lunckeryggen-Brattnipene region. The younger intrusive rocks are composed of alkaline rocks in contrast with the older intrusive rocks dominated by tonalite and granodiorite with low K_2O content in the Sor Rondane Mountains. Syenitic rocks in the Sor Rondane Mountains are characterized by high K_2O and low Na_2O contents. Such extremely high K_2O/Na_2O ratios correspond to that of the syenitic rocks in the Yamato and Belgica Mountains and it is considered that the high K_2O/Na_2O ratio may be a general characteristic of the early Paleozoic plutonism in the eastern Queen Maud Land. The transition of the plutonism from calc-alkaline to alkaline affinity corresponds to the tendency of the Pan-African magmatism.
- 国立極地研究所の論文
著者
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Sakiyama Tohru
Faculty Of Science Hiroshima University
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Sakiyama Tohru
Institute Of Natural And Environmental Sciences Himeji Institute Of Technology
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Osanai Yasuhito
Department of earth sciences, Okayama university
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Osanai Yasuhito
Division Of Evolution Of Earth Environments Faculty Of Social Andcultural Studies Kyushu University
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Osanai Yasuhito
Department Of Earth And Planetary System Science Okayama University
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Osanai Yasuhito
Division Of Evolution Of Earth Environments Kyushu University
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Osanai Yasuhito
Division Of Evolution Of Earth Environments Faculty Of Social And Cultural Studies Kyushu University
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Osanai Y
Division Of Evolution Of Earth Environments Faculty Of Social And Cultural Studies Kyushu University
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TAKAHASHI Yuhei
Geological Survey of Japan, Hokkaido Branch
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Takahashi Y
Geological Survey Of Japan Sapporo
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Takahashi Yuhei
Geological Survey Of Japan
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