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Guang-cheng CHI, Li-hua SONG, Na WANG, De-song CUI, Guo-xing ZHOU. Identification of Alteration Mineral Composition of Kimberlite from Shandong Mengy by X-ray Powder Diffractometer[J]. Rock and Mineral Analysis, 2010, 29(4): 475-477.
Citation: Guang-cheng CHI, Li-hua SONG, Na WANG, De-song CUI, Guo-xing ZHOU. Identification of Alteration Mineral Composition of Kimberlite from Shandong Mengy by X-ray Powder Diffractometer[J]. Rock and Mineral Analysis, 2010, 29(4): 475-477.
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Identification of Alteration Mineral Composition of Kimberlite from Shandong Mengy by X-ray Powder Diffractometer

  • Shenyang Institute of Geology and Mineral Resources, Shenyang110032, China

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  • Received Date: October 07, 2009
  • Accepted Date: January 13, 2010
  • Published Date: July 31, 2010
    Abstract
  • The kimberlite from Shandong Mengy mainly consists of alteration minerals. X-ray powder diffraction results showed that the barren-kimberlite consists of calcite, dolomite, quartz, calzirtite with dolomite and calzirtite as the signature minerals, the lean-kimberlite consists of serpentine, calcite, grossular, magnetite and phlogopite with grossular as the signature mineral, the rich-kimberlite consists of serpentine, calcite, chlorite, apatite, magnetite and phlogopite with chlorite and apatite as the signature minerals. The research results indicate that X-ray powder diffraction is a powerful tool for identifying kimberlite alteration mineral composition, studying on the relationship between component change of alteration minerals and ore potentiality of kimberlite, and assessing barren-kimberlite, lean-kimberlite and bonanza-kimberlite based on the signature minerals.
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