Manganese Skarn in the Shizhuyuan Polymetallic Tungsten Deposit, Hunan, China

• MAO Jingwen

  Institute of Mineral Deposits, Chinese Academy of Geo-logical Sciences

• GUY Bernard

  Departement Geochimie, Ecole des Mines de Saint-Etienne, France

• RAIMBAULT Louis

  Centre d'Informatique Geologique, Ecole des Mines de Paris, France

• SHIMAZAKI Hidehiko

  Geological Institute, University of Tokyo

Bibliographic Information

Other Title

• 中華人民共和国湖南省柿竹園多金属タングステン鉱床のマンガンスカルン
• Manganese Skarn in the Shizhuyuan Polym

Abstract

Manganese skarns in the Shizhuyuan supergiant W-Sn-Mo-Bi-Be deposit consist of spessartine, almandine-spessartine garnet, rhodonite, tephroite, helvite, alabandite, Mn-bearing salite, manganese hedenbergite, Mn-bearing phlo-gopite and rhodochrosite. The development of the skarn is related, in time and space, to the greisenization-mineralizations subsequent to calcic skarnization and related retrograde alteration. Complexity of mineral assemblages and manganese contents of the minerals increase with distance from the, contact zone of the Qianlishan granite stock. The manganese content of host rocks of the deposit is low, and the source of manganese in the skarn is supposed to be mainly from the hydrothermal solution associated with Yanshanian granite emplacement.

Journal

• Shigen-Chishitsu

  Shigen-Chishitsu 46 (255), 1-11, 1996

  The Society of Resource Geology

Keywords

• Shizhuyuan tungsten deposit
• Polymetallic
• Man-ganese skarn
• Spessartine garnet
• Yanshanian granite
• China

Details

• CRID: 1390001204467965312
• NII Article ID: 130003645382
• NII Article ID: 10002858098
• NII Book ID: AN10379890
• DOI: 10.11456/shigenchishitsu1992.46.1
• ISSN: 21854033
• ISSN: 09182454
• NDL BIB ID: 3934755
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I3934755
• Data Source:
  • JaLC
  • NDL
  • CiNii Articles
• Abstract License Flag: Disallowed