Tectonic stress field’s characteristic and its relationship of uranium mineralization at Dazhou volcanic faulted basin in Quzhou ,Zhejiang
DOI:
Author:
Affiliation:

Clc Number:

Fund Project:

  • Article
  • |
  • Figures
  • |
  • Metrics
  • |
  • Reference
  • |
  • Related
  • |
  • Cited by
  • |
  • Materials
  • |
  • Comments
    Abstract:

    Based on the study of the structural deformation,through strike-dip surveying of field outcropped conjugate shear joints and adopt mathematical statistics to match by stages, combining previous research achievements.and carried out the study of Dazhou volcanic faulted basin paleo-tectonic stress field and the relationship of uranium mineralization. Summed up four main tectonic stress stages: the former Cretaceous tectonic period、Moshishan tectonic period、Qujiang tectonic period、Eocene-Oligocene tectonic period, discussed the control role of the various periods on uranium mineralization, pointed out the latter three tectonic stress stages play a main part in uranium mineralization, tectonic stress field in Moshishan tectonic period prepared ore storage space,tectonic stress field in Qujiang tectonic period prepared ore transmitting space , tectonic stress field in Eocene-Oligocene tectonic period destroyed and transformed the formed ore deposits.

    Reference
    Related
    Cited by
Get Citation

HUI Xiaochao, HAN Xiaozhong, LIN Jianping, WANG Mingtai, ZHANG Bin, TANG Jiangwei, DU Jianghao, JIN Miaozhang, LEI Yaoming.2012. Tectonic stress field’s characteristic and its relationship of uranium mineralization at Dazhou volcanic faulted basin in Quzhou, Zhejiang[J]. Acta Geologica Sinica,86(2):228-240

Copy
Share
Article Metrics
  • Abstract:
  • PDF:
  • HTML:
  • Cited by:
History
  • Received:January 19,2011
  • Revised:July 19,2011
  • Adopted:July 25,2011
  • Online: January 17,2012
  • Published: