山东胶东半岛焦家断裂带南缘电性结构研究
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本文为国家重点研发计划(课题编号 2016YFC0600101,2016YFC0600201)及自然基金重点项目(41630320)联合资助的成果。


Electrical structures in the southern reach of the Jiaojia fault belt inferred from audio- frequency magnetotelluric sounding in the Jiaodong Peninsula, Shandong Province
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    摘要:

    胶东半岛是中国金矿最集中的区域,焦家金矿带则是胶东半岛最重要的三条金矿带之一,在该带中已探明新城、焦家、河西等特大型金矿床。焦家金矿带受焦家断裂控制,成矿带基本与断裂带吻合,焦家断裂带北部位置和形态基本探明, 但其南部因史家以南地区的第四系覆盖层而难以追踪。为了解焦家断裂带南部延伸特征,我们在史家地区开展了面积性音频大地电磁测深(AMT)工作,获得了23条电阻率模型剖面,并构建了研究区拟三维电阻率模型。结合区内岩矿石电性参数以及以往的研究成果,初步厘定了焦家断裂带南延位置和形态,认为该断裂带自史家以南受后期NWEW向断裂改造影响,出现错断现象,并且向南拆分成东、西两组断裂。而焦家断裂的低电阻率特征,说明断裂发育于引张或挤压-引张应力背景之下,并且是岩浆活动的浅部通道,岩浆热液的进入使断裂带内发生蚀变硅化、钾化等蚀变作用,金元素局部富集,最终可能在断裂带隐伏有利部位成矿。

    Abstract:

    The Jiaodong peninsula has the highest concentration of gold mines in China. The Jiaojia gold belt is one of the three most important gold belts in the Jiaodong peninsula. In this belt, super gold deposits such as Xincheng, Jiaojia and Hexi have been discovered. As the Jiaojia gold ore belt coincided with the fault zone, the position and shape of the northern Jiaojia fault zone was ascertained. However, the southern part was hard to locate because of the Quaternary cover. In order to determine the southern extension of Jiaojia fault belt, we collected audio magnetotelluric (AMT) data over a 44 km×52 km area in the Shijia district, which included 23 EW oriented profiles. Twenty three pseudo -2D resistivity sections were constructed through careful data processing and a quasi three- dimensional resistivity model was constructed for the study area. Following a comprehensive analysis of rock and ore electrical parameters in the study area, in conjunction with previous geological data, apreliminary position and shape of the southern Jiaojia fault zone was identified. It was concluded that the Jiaojia fault zone was affected by the NW- EW fracture deformation in the south of Shijia district, and subsequent to the faulting was split southward into two groups of fracture to the east and west. Jiaojia fault zone is characterized by low resistivity value, the fault zone is in the lead or extrusion- formed under the background of tensile stress, and can provide a wide channel for magmatic activity. Magmatic hydrothermal entry occurs in the fault and may eventually be beneficial in the fault zone mineralization.

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胡浩,张昆,严加永,邵陆森,付光明.2020.山东胶东半岛焦家断裂带南缘电性结构研究[J].地质学报,94(2):661-674.
HU Hao, ZHANG Kun, YAN Jiayong, SHAO Lusen, FU Guangming.2020. Electrical structures in the southern reach of the Jiaojia fault belt inferred from audio- frequency magnetotelluric sounding in the Jiaodong Peninsula, Shandong Province[J]. Acta Geologica Sinica,94(2):661-674.

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  • 收稿日期:2018-11-15
  • 最后修改日期:2019-03-26
  • 录用日期:2019-08-02
  • 在线发布日期: 2019-08-02
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