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한국, 일본, 러시아 용암동굴 형성층의 형광X선 분석과 편광현미경적 연구
XRF Analysis and Polarizing Microscopic Study of the Lava Cave Formation, Korea, Japan and Russia

Sawa, Isao   (Osaka University of Economics and LawUU0014187  ); Furuyama, Katsuhiko   (Osaka City UniversityUU0014998  ); Ohashi, Tsuyoshi   (Osaka University of Economics and LawUU0014187  ); Kim, Chang-Sik   (JejuCollege of Technology  ); Kashima, Naruhiko   (JejuCollege of Technology  );
  • 초록

    (1) Kaeusetgul Cave in Kimnyong-Ri, Jeju-Do, Korea. Kaeuset-gul Cave (KC) is situated in NNE area of the Manjang-gul cave (125m a.s.l.). Kaeuset-gul Cave lies at $126^{\circ}45'22"$ E in longitude and $33^{\circ}33'09"$ N in latitude. The coast belong Kimnyeong-Ri, Kujwa-eup, Jeju-Do. Altitude of the cave-entrance is 10m and length of the cave is 90m. Lava hand-specimens of KC are studied by X-ray fluorescence analysis (XRF). Average major chemical components of specimens from KC is as follows (wt.%); $SiO_2=47.03$ , $TiO_2=3.16$ , $Al_2O_3=18.41$ , FeO*=13.53, MnO=0.14, MgO=5.05, CaO=8.66, $Na_2O=2.81$ , $K_2O=0.67$ , $P_2O_5=0.55$ in KC. Polarizing microscopic studyindicates that these specimens are described of alkali-basalt. (2) Tachibori Fuketsu (Cave) in Shizuoka Prefecture, Fuji Volcano, Japan Tachibori Fuketsu lies attoward the south in skirt of the Fuji volcano, $138^{\circ}42'04"$ east longitude and $35^{\circ}18'00"$ north latitude. The location of cave entrance is 2745, Awakura, Fujinomiya-shi, Shizuoka Prefecture. The above sea level and length of Tachibori Fuketsu are 1,170m and 82m. Average major chemical components of specimens from cave areas follows (Total 100 wt.%) ; ( $SiO_2$ =50.52, 50.52, $TiO_2$ =1.69, 1.69, $Al_2O_3$ =15.47, F 15.47, FeO*=13.13, MnO=0.20, MgO=5.97, CaO=9.17, $Na_2O$ =2.52, 2.52, $K_2O$ =0.94 0.94 and $P_2O_5=0.40).$ Polarizing microscopic study indicates that these specimens may belong to tholeiite-basalt series. According to polarizing microscopic study, Au (Augite), P1 (Plagioclase), and O1 (Olivine) are contained as phenocryst minerals. (3) Gorely Cave in Kamchatka Peninsula, Russia Gorely caldera is located at the southeastern part of Kamchatka Peninsula, about 75km southwest of Petropavlovsk-Kamchatskiy.. Gorely lava caves are situated in NHE area of Mt. Gorely volcano (1829m a.s.1.). One of lava cave (Go-9612=K-1) lies at $158^{\circ}00'22"$ east longitude and $52^{\circ}36'18"$ north latitude. The elevation of cave entrance is about 990m a.s.1. and the main cave extends in the NNW direction for about 50m by 15m wide and 5m in depth. The cave of K-3is near the K-1 cave. "@Lava hand-specimens K-1 and K-3 caves are studied by X-ray fluorescence analysis and polarizing microscopic observation. Average major chemical components of specimens from these caves are as follows (wt.%) ;( $SiO_2$ =55.12, 55.12, $TiO_2$ =1.25, 1.25, $Al_2O_3$ =16.07, T 16.07, T-FeO* =9.41, MnO=0.16, MgO=5.01, CaO=7.21, $Na_2O$ =3.39, 3.39, $K_2O$ =1.92, 1.92, $P_2O_5$ =0.45) a 0.45) and these values indicate that the Gorely basaltic andesite belong to high alumina basalt. Polarizing microscopic study indicates that these specimens are described of Augite andesite.


  • 주제어

    Lava Cave .   Lava Stalactite .   Polarizing Microscopic Study.  

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  • 이 논문을 인용한 문헌 (2)

    1. Cho, Mi-Ryong ; Shin, Dong-Won 2008. "Types of Korean caves" 洞窟 : 한국동굴학회지 = Journal of the Korean speleological society, 84(): 35~42     
    2. Choi, Byong-Cheon 2008. "An analysis of research trends on caves by the Speleological Society of Korea" 洞窟 : 한국동굴학회지 = Journal of the Korean speleological society, 84(): 46~52     

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