浙江衢州大洲火山岩断陷盆地构造应力场特征及其与铀成矿关系
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Tectonic stress field’s characteristic and its relationship of uranium mineralization at Dazhou volcanic faulted basin in Quzhou ,Zhejiang
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    摘要:

    在构造变形研究的基础上,通过野外露头共轭剪节理的产状测量,采用数学统计方法进行分期配套,并结合前人的研究成果,开展了大洲火山岩断陷盆地古构造应力场及其与铀成矿关系的研究。总结了主要经历的四期构造应力:前晚侏罗世构造期、磨石山期、衢江期、始新世—渐新世构造期,分别讨论了各个期次对铀成矿的控制作用,指出后三个构造期与铀成矿关系密切,即磨石山期构造应力场为成矿准备了储矿空间,衢江期构造应力场为成矿准备了导矿空间,而始新世-渐新世构造期构造应力场对已形成矿体进行了破坏或改造。

    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.

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惠小朝,韩效忠,林建平,王明太,张斌,汤江伟,杜江浩,金淼张,雷遥明.2012.浙江衢州大洲火山岩断陷盆地构造应力场特征及其与铀成矿关系[J].地质学报,86(2):228-240.
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.

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  • 收稿日期:2011-01-19
  • 最后修改日期:2011-07-19
  • 录用日期:2011-07-25
  • 在线发布日期: 2012-01-17
  • 出版日期: