桃山铀矿田桃山断裂及其保矿作用
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:


Author:
Affiliation:

Fund Project:

单位:
  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    桃山铀矿田位于江西省中部,断裂构造发育,既有成矿构造,也有保矿构造,其中斜贯桃山矿田的桃山断裂即是一保矿构造,它形成于车免近时期,走向北东,倾向南东,右行正断,并具铰链断层性质,上盘地块掀斜下落,致使上盘成矿壳层向NW和NE倾斜,由于倾末端的侵蚀深度较小,保矿条件较好,加强这些地带的铀矿勘查和评价具有重要意义。

    Abstract:

    Taoshan uranium orefield is located in the central Jiangxi province, where the fractures, both metallotectonic also oreconservative, had developed extensively, of which Taoshan fault, with NEstriking, SEdipping at 65°~70° , rightlateral slip, developed in neotectonism period, is an oreconservative one, not only their southeast block downgliding, but Jiaolian fault characteristics. Taoshan fault causes the Umineralization shell in NW and NEdipping, so resulting in weak erosion in the end dumping, especially in its northeast part. For this reason, there are good oreprotecting conditions and more prospecting potential in those region and an important significance for uranium ore exploring.

    参考文献
    相似文献
    引证文献
引用本文

张万良.2008.桃山铀矿田桃山断裂及其保矿作用[J].地质论评,54(6):768-774,[DOI].
ZHANG Wanliang.2008.[J]. Geological Review,54(6):768-774.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期:
  • 出版日期: