한국산업보건학회지 (Journal of Korean Society of Occupational and Environmental Hygiene)

  • 제26권3호
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  • Pages.253-266
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  • 2016
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  • 2384-132X(pISSN)
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  • 2289-0564(eISSN)
한국산업보건학회 (Korean Industrial Hygiene Association)
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가평 사문암 광산의 석면 산출의 산상과 모암의 특성

Occurrences of Asbestos within Gapyeong Serpentinite Mines and Characteristics of Host Rocks

  • 송석환 (중부대학교 대학원 환경보건학과) ;
  • 강준구 (중부대학교 대학원 환경보건학과)
  • Song, Suckhwan (Graduate school, Department of Environment and Health, Joongbu University) ;
  • Kang, Joongu (Graduate school, Department of Environment and Health, Joongbu University)
  • 투고 : 2016.06.07
  • 심사 : 2016.09.23
  • 발행 : 2016.09.30
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초록

Objectives: This study is for characteristics of asbestos occurrence (NOA, naturally occurring asbestos) from the Gapyeong area and its host rocks, serpentinites. Methods: Representative samples are collected from the serpentinite bodies, following degrees of hydrothermal alteration and metamorphism, after about 2 year field trips. Mineralogical, morphological and optical characteristics of the asbestos and host rocks are confirmed by PLM, XRD EPMA and SEM results. Results: The serpentinites are dunites and harzburgites, and host asbestos, including chrysotile, tremolite and actinolite. The asbestos chrysotiles are found as veins ranging from several millimeters to several centimeters in thickness, while asbestos-tremolite and -actinolite occur along cracks and fractures ranging up to ten centimeters in thickness. The chryostiles occur mainly as cross and slip fibers, while the amphibole asbestos is found as vein, slip and oblique fibers. More tremolitic grains are colorless and commonly show elongated or fiber shapes, whereas the magnesio hornblende grains mainly show light green and occur as subhedral to euhedral diamond grains. Conclusions: Overall characteristics of serpentinites from the Gapyeong area are similar to worldwide orogenic-related Alpine type ultramafic rocks serpentinized and serpentinites in South Chungcheong-do Province, Korea, and occurrences of asbestos are similar to those of the ultramafic bodies in South Chungcheong-do Province.

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참고문헌

  1. Agency for Toxic Substances and Disease Control, Toxicological profiles for asbestos(Update): U.S. Department of Health & Human Services, Public Health Service, Atlanta, Georgia.; 2001. p. 327
  2. Churchill RK, Hill RL. A General Location Guide for Ultramafic Rocks in California - Areas More Likely to Contain Naturally Occurring Asbestos, 2000, Map scale 1:1,100,000, California Department of conversation, Division of Mines and Geology Open-File Report 2000-19; 2000. p.7
  3. Churchill RK, Higgins CT, Hill B. Areas More Likely to Contain Natural Occurrences of Asbestos in Western El Dorado County, California, State of California Department of Conservation, Division of Mines and Geology, Open-File Report 2000-002.; 2000. p.66
  4. Clinkenbeard JP, Churchill RK, Kiyoung L. Guidelines for geological investigations of naturally occurring asbestos in California. California Geological Surveys, Special Publication; 2002. p.124
  5. Dymek RF, Brothers SC, Schiffries CM. Petrogenesis of ultramafic metamorphic rocks from 3800 Ma Isua supracrustal belt, western Greenland. J Petrol 1988; 29: 1353-1397 https://doi.org/10.1093/petrology/29.6.1353
  6. Higgins CT, Clinkenbeard JP. Relative likelihood for the presence of naturally occurring asbestos in Eastern Sacramento County, California. Dept. of Conservation, California Geological Survey. Special Report 192.; 2006. p. 34
  7. Kim BG, Lee SM, So CS, Sin MS. Explanatory Text of the Geological Map of Yongduri sheet. 1:50000. Geological and Mineralogical Institute of Korea, 1974
  8. Lee SM, Kim BG, So CS, Sin MS. Explanatory Text of the Geological Map of Yongduri sheet. 1:50000. Geological and Mineralogical Institute of Korea, 1974
  9. Paktung AD. Metamorphism of the ultramafic rocks of the Thompson mine, Thompson nickel belt, Northern Manitovia. Canadian Miner 1984; 22: 77-91
  10. Raymond, LA, Metamorphic petrology. Wm. C. Brown Publishers, 1995; 656-675.
  11. Song SH, Choi SG, Woo JG. Genetic implications of ultramafic rocks from the Bibong area in the Kyeonggi gneiss complex. Econ. Environ Geol 1997; 30(5): 477-491
  12. Song SH, Choi SG, Oh CH, Seo JE, Choi, SH. Petrography and Geochemistry of the Ultramafic rocks from the Hongseong and Kwangcheon areas, Chungcheonnam-Do. Korean Society of Econ Environ Geol. 2004; 37(5): 477-497
  13. Song SH, Hwang JH, Hwang BG, Kim, HW. Occurrence types and mineralogical characteristics of asbestos for the Kwangcheon area, Chungnam. Korean Industrial Hygiene Association 2008; 18: 271-281
  14. Song SH, Lim HJ, Lee WS. Genetic Differences of Two Asbestos Mines, Boryoung Area. Econ Environ Geol 2013; 46(2): 165-178 https://doi.org/10.9719/EEG.2013.46.2.165
  15. Streckeisen A. To each plutonic rock its proper name. Earth-Science Reviews 1976; 12: 1-33 https://doi.org/10.1016/0012-8252(76)90052-0
  16. Wee SM, Choi SG, So CG. Preliminary study on ultramafic rocks from the Chungnam Province, Korea. Econ Environ Geol 1994; 27(2): 171-180
  17. Woo YK, Choi SW, Park KH. Genesis of talc ore deposits in the Yesan area of Chungnam, Korea. J Korean Inst Mining Geol 1991; 24(4): 363-378
  18. Wylie AG, Verkouteren JR. Amphibole asbestos from Libby, Montana: Aspects of nomenclature: American Mineralogist 2000; 85: 1540-1542