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전자현미경을 이용한 흑요석 내 미세결정의 형태와 조직 관찰

Detailed Morphology and Texture of Microlites in Obsidian observed through Electron Microscopy

  • 좌용주 (경상대학교 지질과학과 및 기초과학연구소) ;
  • 황가현 (경상대학교 지질과학과 및 기초과학연구소)
  • Jwa, Yong-Joo (Department of Geology and Research Institute of Natural Sciences, Gyeongsang National University) ;
  • Hwang, Ga-hyun (Department of Geology and Research Institute of Natural Sciences, Gyeongsang National University)
  • 투고 : 2018.10.15
  • 심사 : 2018.12.19
  • 발행 : 2018.12.31

초록

흑요석 내 미세결정은 화산암질 마그마의 과냉각 조건에서 정출된 아주 작은 결정이다. 백두산, 일본 규슈와 홋카이도, 그리고 이태리 리파리 섬에서 산출되는 흑요석을 대상으로 그 내부에 포함된 미세결정의 형태와 조직을 전자현미경을 사용하여 관찰하여 정리하였다. 전자현미경의 후방산란전자 이미지로부터 관찰한 보다 자세한 미세결정에 대한 형태학적 분류는 기존의 광학현미경으로 얻을 수 없는 미세결정의 결정화에 대한 정보를 제공해 준다. 이 논문에서는 Clark (1961)의 미세결정 형태 분류 14가지 중에서 10가지에 대해 새로이 기재하였다. 즉, Lath, Crenulite, Bacillite, Margarite, Belonites, Trichites, Arculites, Furculite, Scopulites, Scopulitic growth 등의 미세결정에 대한 형태와 조직적 특징을 구체적으로 살펴보았다. 이런 기재적 연구로부터 향후 산성 마그마의 냉각과정동안 흑요석 내 미세결정의 결정 작용과 광물 공생관계를 밝히는데 활용될 것이다.

Microlite is crystallized under the supercooled condition of volcanic magma. This study reports the morphology and texture of microlites included in the obsidians from the Baekdusan (Mt. Baekdu), Kyushu (Japan), Hokkaido (Japan) and Lipari Island (Italy) by using a scanning electron microscope (SEM). Morphology and texture observed from the back scattered electron (BSE) image could give more detailed information on the microlite crystallization which cannot be acquired from the conventional optical microscope. Ten types of microlites are newly described according to the 14 morphological types of microlites by Clark (1961): Lath, Crenulite, Bacillite, Margarite, Belonites, Trichites, Arculites, Furculite, Scopulites, Scopulitic growth. Detailed description of the ten microlites can be used to interpret the crystallization and paragenetic relations of crystals during the cooling of acidic volcanic magma.

키워드

참고문헌

  1. Cho, N.-C., Kang, H.-T., and Han, M.-S., 2005, Characterization of the Sangmuryongri obsidian artefacts based on chemical composition and texture. Journal of Korean Ancient Historical Society, 49, 5-26 (in Korean with English abstract).
  2. Cho, N.-C., Kang, H.-T., and Chung, K.-Y., 2006, Provenance study of obsidian artifacts found in the Korean peninsula based on trace elements and Sr isotope ratios. Journal of Korean Ancient Historical Society, 53, 5-21 (in Korean with English abstract).
  3. Clark, D. L., 1961, The Obsidian Dating Method. Current Anthropology 2, 111-114. https://doi.org/10.1086/200172
  4. Donaldson, C. H., 1976, An Experimental Investigation of Olivine Morphology. Contributions to Mineralogy and Petrology, 57, 187-213 https://doi.org/10.1007/BF00405225
  5. Hibbard, M. J., 1995, Petrography to petrogenesis. Prentice-Hall, Inc. 587p.
  6. Hwang, G.-h. and Jwa, Y.-J., 2017, Morphology and texture of microlites in the Baekdusan and Kyushu obsidians. Journal of Korean Earth Science Society, 38, 546-551 (in Korean with English abstract). https://doi.org/10.5467/JKESS.2017.38.7.546
  7. Izuho, M. and Hirose, W., 2010, A review of archaeological obsidian studies in Hokkaido Island (Japan). In: Crossing the Straits: Prehistoric Obsidian Source Exploration in the North Pacific Rim (Kuzmin, Y.V. and Glasscock, M.D., eds.), BAR International Series 2152, 9-25.
  8. Jang, Y.D., Park, T.Y., Lee, S.M., and Kim, J.J., 2007, Petrologic and mineralogic studies on the origin of Paleolithic obsidian implements from Wolseongdong, Korea. Journal of the Korean Earth Science Society, 28, 731-740 (in Korean with English abstract).
  9. Jin, M.E., Moon, S.W., Ryu, C.K., and Jwa, Y.-J., 2014, Mineralogical study on microlites in the Baekdusan obsidian and the Gadeokdo obsidian artefacts. Journal of Mineralogical Society of Korea, 27, 243-249 (in Korean with English abstract). https://doi.org/10.9727/jmsk.2014.27.4.243
  10. Jwa, Y.-J., Yi, S., Jin, M.-E., Kasztovszky, Z., Harsanyi, I., and Sun, G.-M., 2018, Application of prompt gamma activation analysis to provenance study of the Korean obsidian artefacts. Journal of Archaeological Science: Reports, 20, 374-381. https://doi.org/10.1016/j.jasrep.2018.05.016
  11. Manga, M., 1998, Orientation distribution of mircolites in obsidian. Journal of Volcanology and Geothermal Research, 86, 107-115. https://doi.org/10.1016/S0377-0273(98)00084-5
  12. Martinelli, M.C., Iovino, M.R., Tykot, R.H., and Vianello, A., 2016, Lipari obsidian in the late Neolithic: artifacts, supply and function. In: Program and Abstracts of the International Obsidian Conference, Lipari, Italy, pp. 52.
  13. Ross, C.S., 1962, Microlites in glassy volcanic rocks. American Mineralogist, 47, 723-740.
  14. Sharp, T.G., Stevenson, R.J., and Dingwell, D.B., 1996, Microlites and 'nanolite' in rhyolitic glass: microstructural and chemical characterization. Bulletin of Volcanology, 57, 631-640. https://doi.org/10.1007/s004450050116
  15. Yi, S. and Jwa, Y.-J., 2016, On the provenance of prehistoric obsidian artifacts in South Korea. Quaternary International, 392, 37-43. https://doi.org/10.1016/j.quaint.2015.08.012
  16. Yi, S. and Lee, Y.-I., 1996, Preliminary consideration on the geochemical characteristics of the obsidian artefacts. Journal of the Korean Archaeological Society, 35, 172-187.