汪子杰,张德明,徐晓慧.高密-万家地区招(远)-平(度)断裂特征研究[J].地质找矿论丛,2022,37(1):96-102
高密-万家地区招(远)-平(度)断裂特征研究
Study on characteristics of Zhaoyuan-Pingdu fault in Gaomi-Wanjia area
投稿时间:2021-03-02  
DOI:10.6053/j.issn.1001-1412.2022.01.013
中文关键词:  断裂特征  物探解译  招(远)-平(度)断裂  高密-万家地区  山东省
英文关键词:Characteristics of fault  interpretation of geophysical data  Zhaoyuan-Pingdu fault  Gaomi-Wanjia area  Shandong province
基金项目:中国地质调查局地质调查项目(编号:DD20160044-4)、山东省地勘基金项目(编号:鲁勘字(2018)32号)联合资助。
作者单位
汪子杰 山东省第四地质矿产勘查院, 山东 潍坊 261021 
张德明 山东省第四地质矿产勘查院, 山东 潍坊 261021 
徐晓慧 山东省第四地质矿产勘查院, 山东 潍坊 261021 
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中文摘要:
      招(远)-平(度)断裂(简称招平断裂)是山东省内重要的一条金矿控矿断裂,其南段覆盖区研究程度较北段明显偏低。文章基于1:5万高密等4幅区域地质调查工作,详细研究了区内断裂分布情况和活动特征;在充分收集调查区及邻近区物探相关资料基础上,对招平断裂进行各类物探资料的精细解译及综合分析、物探施工验证,明确了招平断裂的展布特征和活动期次。结果表明,招平断裂呈NNE向通过调查区,依次被NW向的七级断裂、大栏断裂、高密断裂所错断,向南与胶河断裂为同一条断裂,其存在3期活动,主活动期为早白垩世。
英文摘要:
      Zhaoyuan-Pingdu fault is an important gold ore-control fault in Shandong province.More researches have been conducted in its North part than in the South part with cover.Based on data of geological survey of 4 sheets of Gaomi etc.at scale 1:50000 distribution and activity of the fault are dealt with in detail.Data of geophysical survey and the workings of check in the study area and the surroundings are collected as detail as possible and elaborately interpreted and analyzed.Its distribution and active stages are made clear-lt runs NNE through the study area,is displaced in turn by WE Qiji fault,Dalan fault and Gaomi fault then becomes Jiaohe fault to south.It was active in 3 stages,mainly in Cretaceous Epoch.
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