• Title/Summary/Keyword: obsidian artifacts

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Provenance Estimation on the Yeoncheon Samgeori Obsidian Artifacts (연천 삼거리 유적지 흑요석제 석기에 대한 산지 추정)

  • Yi, Seonbok;Jwa, Yong-Joo;Jin, Mi-Eun;Kil, Youngwoo
    • The Journal of the Petrological Society of Korea
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    • v.28 no.4
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    • pp.299-306
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    • 2019
  • We estimated the provenance of the obsidian artifacts from Samgeori site at Yeoncheon, one of the prehistoric sites in South Korea. Pyroxene microlites are of hedenbergite to augite compositions, and intergrown and/or overgrown with Fe-oxides showing poikilitic texture. Major oxides contents for the matrix of the obsidian artifacts exhibit a narrow compositional range, especially SiO2 contents being 73.0~75.5 wt.% of acidic rhyolitic composition. Also, rare earth element (REE) contents are relatively constant in the obsidian artifacts, and the chondrite-normalized REE patterns show a strong Eu negative anomaly. These mineralogical and geochemical features of the Samgeori obsidian artifacts were compared with those from both the Baekdusan obsidians and Japanese Kyushu obsidians which have been thought to be two major obsidian provenances around South Korea. It is suggested that the Samgeori obsidian artifacts were possibly originated from the Baekdusan obsidians.

Classification of Obsidian Artifacts found in the Korean Peninsula using Sr isotope ratio (Sr 동위원소비를 이용한 한반도 흑요석의 분류 연구)

  • Cho Nam-Chul;Kang Hyung-Tae;Chung Gwang-Ryong
    • 한국문화재보존과학회:학술대회논문집
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    • 2005.11a
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    • pp.268-271
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    • 2005
  • Sixty-four obsidian artifacts found in the Korean Peninsula have been characterised by a study of their minor elements and Sr isotope ratio. The artifacts are from the following locations: Yondaedo Island; Yokjido Island; Sangnodaedo Island, Tongyeong, Gyeongnam; Dongsamdong, Busan; Songdo Island, Yeosu, Jeonnam; Suyanggae, Danyang, Chungbuk; Sangmuyongri, Yanggu, Gangwondo; Paektusan Mountain; Kyushu region, Japan. The study of minor elements and Sr isotope ratio recognised three distinct major groups. This result suggests that there are no correlations among the three groups whose provenances are different. But as a result of classification using Sr isotope ratio, obsidian artifacts found in the southern part of the Korean Peninsula classified two groups within C group. This research will furnish scientific datum to be able to mutual comparison of obsidians excavated from other site.

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A Classification of Obsidian Artifacts by Applying Pattern Recognition to Trace Element Data

  • Lee, Chul;Czae, Myung-Zoon;Kim, Seung-Won;Kang, Hyung-Tae;Lee, Jong-Du
    • Bulletin of the Korean Chemical Society
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    • v.11 no.5
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    • pp.450-455
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    • 1990
  • Fifty eight obsidian artifacts and four obsidian source samples have been analyzed by instrumental neutron activation analysis. Artifact samples have been classified into classes by unsupervised learning techniques such as eigenvector projection and nonlinear mapping. The source samples have thereafter been connected to the classes by the supervised learning techniques such as SLDA and SIMCA so as to characterize each class by possible source sites. Some difference attributable to different nonlinear mapping techniques and the elemental effects on the separation between classes have been discussed.

Classification of Obsidian Artifacts found in the Korean Peninsula by Chemical Compositions and Magnetic Properties (성분분석 및 자기적 특성에 의한 한반도 흑요석의 분류 연구)

  • Cho, Nam-Chul;Park, Yong-Hee;Doh, Seong-Jae;Kang, Hyung-Tae;Nam, In-Tak
    • Journal of Conservation Science
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    • v.16 s.16
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    • pp.89-103
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    • 2004
  • Provenance discrimination of sixty four obsidian artifacts found in the Korean Peninsular has been carried out using major elements, minor elements and magnetic properties. Most of obsidians in this study were classified into the subalkaline series based on the contents of $Al_2O_3,\;CaO,\;and\;Na_2O+K_2O$ in samples. Provenance & obsidians were classified into three major groups using major elements and minor elements analyse. This result suggests that there are no correlations among the three groups whose provenances are different. Although the magnetic properties of obsidians do not yield clear groupings according to the archaeological site, the bivariate plot for the magnetic susceptibility and the saturation isothermal remanent magnetization shows a rough correlation with the results of major and minor elements analyses.

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