基于重磁多尺度边缘检测的长江中下游成矿带构造格架研究
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国家自然科学基金重点基金项目(编号:40930418)和国家科技专项“深部矿产资源立体探测技术与试验”(编号:SinoProbe-03)联合资助


Tectonic Framework Research of the Lower and Middle Reach of the Yangtze River Metallogenic Belt Based on Gravity and Magnetic Multi-scale Edge Detection
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    摘要:

    通过建立不同埋深、不同物性(磁化率、密度)模型体,正演其重力、磁力的地面响应,对比了当前常用的几种边缘增强和检测方法,发现多尺度边缘检测方法对模型体边界识别能力最强。采用该方法对长江中下游成矿带区域重力和航磁数据进行了边缘检测,结合大地电磁剖面和地质资料,建立了长江中下游构造构造格架,初步厘定了长江深断裂、郯庐大断裂等断裂系统的展布位置,划分了板块、火山岩盆地等横向结构的边界。在此基础上,分析了长江中下游成矿带主要矿集区与构造格架的关系,探讨了矿集区形成的深部背景。

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    Through the establishment of different depths and different physical properties (magnetic susceptibility, density) model of the body, forward of its gravity, ground magnetic response, compared to the current edge enhancement and several commonly used detection methods, multiscale edge detection method that the model Boundary Ability to identify the strongest. Using the method of the Yangtze River metallogenic belt of regional gravity and aeromagnetic data for the edge detection, combined with magnetotelluric profiles and geological data, to establish a structural framework structure of the Yangtze River, the initial determination of the Yangtze River deep fault, major fault Tanlu Distribution system such as fault location, dividing the plate, such as horizontal structure of the volcanic basin boundary. On this basis, analysis of the Yangtze River metallogenic belt of the main ore zone and tectonic framework of the relationship between the formation of the ore district deep background.

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严加永,吕庆田,孟贵祥,赵金花,邓震,刘彦.2011.基于重磁多尺度边缘检测的长江中下游成矿带构造格架研究[J].地质学报,85(5):900-914.
Yan jiayong, Lv Qingtian, MENG Guixiang, ZHAO Jinhua, DENG Zhen, LIU Yan.2011. Tectonic Framework Research of the Lower and Middle Reach of the Yangtze River Metallogenic Belt Based on Gravity and Magnetic Multi-scale Edge Detection[J]. Acta Geologica Sinica,85(5):900-914.

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  • 收稿日期:2011-03-29
  • 最后修改日期:2011-03-29
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  • 在线发布日期: 2011-05-16
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