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Volume 11 Issue 2
Jun 2000
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Kim Won. Serpentine Jade (Bowenite) in Korea. Journal of Earth Science, 2000, 11(2): 103-106.
Citation: Kim Won. Serpentine Jade (Bowenite) in Korea. Journal of Earth Science, 2000, 11(2): 103-106.

Serpentine Jade (Bowenite) in Korea

Funds:

the Korea Science and Engineering Foundation 95-1-05-01-01-2

the Center for Mineral Resources Research sponsored by the KOSEF 

  • Received Date: 14 Feb 2000
  • Accepted Date: 10 Mar 2000
  • A bowenite deposit, recently discovered in Booyo County, Republic of Korea, is the first of its kind in the country. This deposit is located along the contacts of garnet veins intruding the serpentinite. The bowenite is translucent, dark green in color, greasy in luster, 5 in Mohs ' scale of hardness, ~2.57 in SG, 2.58 in RI, and 1.56 in ND. The X ray powder diffraction analysis identified the bowenite as antigorite of the serpentine group minerals, whose major chemical compositions are composed of SiO2 (42.49 %), MgO (39.08 %), Fe2O3 (3.85 %), and H2O (11.87 %) and whose important trace elements include Cr (2 188×10-6), Ni (1110×10-6), and Co (58×10-6). The IR spectrum shows the absorptions at 3 670 (OH stretching), 1 190, 1 070, 980 (SiO stretching) and 610 cm-1 (OH bending). The DTA/TGA thermogram shows the peaks at 343, 755 and 830.1 ℃. The endothermic reaction at 755 ℃ denotes expulsion of structural water, and the strong exothermal reaction at 830.1 ℃ is related to the formation of olivine. Black inclusions finely dispersed in the mineral are identified, with X ray Gandolfi camera method, as magnetite.

     

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