Chinese Journal of Geochemistry

, Volume 5, Issue 1, pp 1–14 | Cite as

REE geochemistry of fluorites from tungsten mineralization at Dajishan, Jiangxi Province, China

  • L. Raimbault
  • Liu Yimao 
  • Guo Qiti 
  • Zhang Yuxue 
  • M. Fonteilles
  • L. Burnol


The available data, although insufficient to understand the complete process of ore formation, give some support to the preliminary results on fluid behavior in the hydrothermal system of Dajishan:
  1. 1.

    Several successive fluids have crystallized minerals, using the same veins as channels.

  2. 2.

    A single vein network, or even the complete vein system, can be considered, in a first approach, as an infinite medium (i.e., an open system) relative to the studied elements.

  3. 3.

    Precise observations indicate the existence of several differenciation processes in the main fluid stage which occurred during ore deposition. Their interpretations—“immobile” fluid and diffusion or ascending fluid and crystallization or mixing—remain uncertain until new data on other minerals are obtained.



Central Group Central Vein Jiangxi Province Granite Body Northern Group 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.


  1. [1]
    Marchand, L., Contribution à l’étude de la distribution des lanthanides dans la fluorine. Etude expérimentale et application au gite de Maine (Saone et Loire, France). Thése de 3° cycle, Université d’Orléans, 1976.Google Scholar
  2. [2]
    Grappin, C., Treuil, M., Yaman, S. et Touray, J. C., Mineral Deposita, 14(1979), 297–309.CrossRefGoogle Scholar
  3. [3]
    Raimbault, L., Géologie, pétrographie et géochimie des granites et minéralisations associées de la région de Meymac (Haute Corréze, France). Thése de docteur-ingénieur, E. N. S. Mines Paris, 1984, 482.Google Scholar
  4. [4]
    Raimbault, L., Utilisation des spectres de terres rares des miréraux hydrothermaux pour la caractérisation des fluides mineralisateurs et l’identification des magmas sources et des processus évolutifs. To be published in Bull. Minéral., 108(1985).Google Scholar
  5. [5]
    Schott, J., Bull. Mineral., 106(1983), 247–262.Google Scholar
  6. [6]
    Sverjensky, D. A., Earth Planet. Sci. Lett., 67(1984), 70–78.CrossRefGoogle Scholar

Copyright information

© Science Press 1986

Authors and Affiliations

  • L. Raimbault
    • 1
    • 2
  • Liu Yimao 
    • 3
  • Guo Qiti 
    • 3
  • Zhang Yuxue 
    • 3
  • M. Fonteilles
    • 4
  • L. Burnol
    • 5
  1. 1.Ecole des Mines, Laboratoire de GéologieUA CNRS 384st EtienneFrance
  2. 2.Groupe des Sciencesde la Terre, Laboratoire Pierre SüeCEA SaclayGif YvetleFrance
  3. 3.Institute of GeochemistryAcademia SinicaChina
  4. 4.Laboratoire de Géologie AppliquéeUA CNRS 384Paris Cedex 05France
  5. 5.ParisFrance

Personalised recommendations