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Article Navigation >  Acta Sedimentologica Sinica  > 2010  >  28(6): 1175-1181

XIA Xuehui. Sedimentary Genesis Feature of Bamianshan Unusual Large Fluorite Deposit in Zhejiang Province[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1175-1181.
Citation: XIA Xuehui. Sedimentary Genesis Feature of Bamianshan Unusual Large Fluorite Deposit in Zhejiang Province[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1175-1181.
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Sedimentary Genesis Feature of Bamianshan Unusual Large Fluorite Deposit in Zhejiang Province

  • Geology Institute of China Chemical Geology and Mining Bureau, Zhuozhou Hebei 072754

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  • Corresponding author: XIA Xuehui
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2010-12-10
  • Bamianshan is an unusual large fluorite deposit discovered in recent years. This paper studies the geologic background of mineralization, geological feature of orebody, ore characters, characters of petrochemistry composition, REE characters of rocks and ores, and SmNd isotope of Bamianshan fluorite deposit. It shows that Bamianshan fluorite deposit is an unusual large fluorite deposit which was formed mostly by sedimentation and later hydrothermal reformation. Based on the analysis data and combined with characters of orehosted rocks and orebody, it is predicted that the sedimentary rocks of Cambrain System as its source bed, which supplied necessary materials of Bamianshan fluorite deposit. Magmatism in later stage altered some orebodies in different extent and
    formed partial deep lean vein ore bodies in structure belt.
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Publishing history
  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2010-12-10

Sedimentary Genesis Feature of Bamianshan Unusual Large Fluorite Deposit in Zhejiang Province

  • Geology Institute of China Chemical Geology and Mining Bureau, Zhuozhou Hebei 072754
    Corresponding author: XIA Xuehui
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2010-12-10

Abstract: Bamianshan is an unusual large fluorite deposit discovered in recent years. This paper studies the geologic background of mineralization, geological feature of orebody, ore characters, characters of petrochemistry composition, REE characters of rocks and ores, and SmNd isotope of Bamianshan fluorite deposit. It shows that Bamianshan fluorite deposit is an unusual large fluorite deposit which was formed mostly by sedimentation and later hydrothermal reformation. Based on the analysis data and combined with characters of orehosted rocks and orebody, it is predicted that the sedimentary rocks of Cambrain System as its source bed, which supplied necessary materials of Bamianshan fluorite deposit. Magmatism in later stage altered some orebodies in different extent and
formed partial deep lean vein ore bodies in structure belt.

XIA Xuehui. Sedimentary Genesis Feature of Bamianshan Unusual Large Fluorite Deposit in Zhejiang Province[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1175-1181.
Citation: XIA Xuehui. Sedimentary Genesis Feature of Bamianshan Unusual Large Fluorite Deposit in Zhejiang Province[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1175-1181.
shu

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