地质学报2012，Vol.86Issue(2)：228-240,13.DOI:11-1951/P.20120113.0857.013
浙江衢州大洲火山断陷盆地构造应力场特征及其与铀成矿关系
Tectonic Stress Field's Characteristic and Its Relationship of Uranium Mineralization at Dazhou Volcanic Faulted Basin in Quzhou, Zhejiang Province
摘要
Abstract
Based on the study of the structural deformation, the occurrence measurement of outcropped conjugate shear joints, and previous research results, the paleo-tectonic stress field of the Dazhou volcanic faulting basin and its relationship to uranium mineralization was studied using mathematical statistics. Four stages of tectonic stress undergone are summarized: pre-Late Jurassic tectonic stage, Moshishan stage, Qujiang stage, and Eocene-Oligocene tectonic stage. And controlling of each stage over uranium mineralization is also discussed. Finally, this study suggests that late three tectonic stages have close relation to the uranium mineralization, I. E. The Moshishan tectonic stress field provided space for mineralization, the Qujiang stage provided conduits, and Eocene-Oligocene tectonic stress destroyed or reformed previously-formed orebodies.关键词
火山断陷盆地/构造应力场/剪节理/铀成矿/衢州地区Key words
volcanic faulted basin/ tectonic stress field/ shear joints/ uranium mineralization/ Quzhou area引用本文复制引用
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..浙江衢州大洲火山断陷盆地构造应力场特征及其与铀成矿关系[J].地质学报,2012,86(2):228-240,13.基金项目
本文为工业和信息化部核能开发三期“衢州地区铀成矿预测技术研究”项目(编号H061)资助的成果. （编号H061）
