| 南雄断裂带构造演化及铀成矿作用 |
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| 引用本文： | 杨尚海.南雄断裂带构造演化及铀成矿作用[J].铀矿地质,2010,26(5):257-263. |
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| 作者姓名： | 杨尚海 |
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| 作者单位： | 核工业230研究所,湖南,长沙,410011 |
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| 基金项目： | 文章部分资料及图件引自核工业290研究所《南雄断裂带坪下水地区铀矿普查技术报告》,成文后王联社、朱捌、黄国龙、于伟营等同仁提出了许多有益的修改意见和建议,在此一并致谢! |
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| 摘 要： | 文章从粤北地区受南雄断裂带控制的南东侧盆地沉积建造组合、构造岩成分特征等入手,探讨南雄断裂带的发生发展、构造动力演化及不同阶段断裂组合形式和铀矿床区域定位规律,提出与南雄断裂带强烈挤压阶段相配套的北西向张性断裂系统是幔源岩浆作用及其深部热流体侵入通道和铀矿体赋存部位的观点。下一步工作重点应针对北西向张性断裂的隐蔽性特点,选择有效的地球物理和地球化学勘查手段,查明北西向断裂地表出露的确切位置、产状变化及其空间展布规律,配合钻探工程揭露验证,不断深化对区域铀成矿规律的认识,扩大找矿效果。
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| 关 键 词： | 南雄断裂 构造演化 张性断裂 控矿作用 |
Research of the structural evolution and its action on uranium mineralization of Nanxiong fracture belt,southern China |
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| YANG Shang-hai.Research of the structural evolution and its action on uranium mineralization of Nanxiong fracture belt,southern China[J].Uranium Geology,2010,26(5):257-263. |
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| Authors: | YANG Shang-hai |
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| Institution: | YANG Shang-hai(Research Institute No.230,CNNC,Changsha,Hunan 410011,China) |
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| Abstract: | By studying the sediment formations in the basin to the southeast of Naxiong fracture belt and the lithologic composition of structre rocks,this paper discusses the the origination and development,evolution of structural dynamics,fracture pattern and locating pattern of uranium deposits.It was suggested that the NW striking tensional fractures matched to Nanxiong fracture belt during the intensely compress periond were the intrusive passageway of mantle magmatism and deep hydrothermal fluid,and the store pl... |
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| Keywords: | Nanxiong fracture belt structure evolution tensional fracture control over mineralization |
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