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Gold Science and Technology ›› 2017, Vol. 25 ›› Issue (3): 61-69.doi: 10.11872/j.issn.1005-2518.2017.03.061

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Feature of Ore-controlling Structure and Prospecting Direction for the Liaoshang-type Gold Deposit in the Northeast Margin of Jiaolai Basin，Shandong Province

WANG Zhixin1，JIAO Xiumei2，DING Zhengjiang 1，3，LIU Xiaomin 1，LI Guohua 1，JI Xubo 4，TANG Junzhi 4   

  1. 1.3th Geology & Mineral Resources Survey Institute，Shandong，Yantai    264000，Shandong，China；
    2.Shandong Provincial Bureau of Geology & Mineral Resources，Jinan    250013，Shandong，China；
    3.China University of Geosciences（Beijing），Beijing    100083，China；
    4.Shandong Humon Smelting Co.，Ltd.，Yantai    264100，Shandong，China
  • Received:2017-03-20 Revised:2017-05-10 Online:2017-06-30 Published:2017-09-11

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Abstract:

The Liaoshang type，pyrite-bearing carbonate vein as the gold carrier，is a new type gold deposit summed up from deep exploration achievement.The deposit is the first large gold deposit in the northeastern margin of Jiaolai Basin.This article analyze the geological characteristics，ore controlling structure and mineralization regularity of the Liaoshang large gold deposit.The results show that the ore-bearing structure is detachment fault system developed between Jingshan group and Mesozoic granite，as well as metamorphosed basement and Mesozoic cover，and provided wide space for large scale metallogenisis.On this basis，the prospecting direction of the same type gold deposits in the northeastern margin of Jiaolai Basin is defined，which provides guidance for the further exploration in this area.

Key words: Jiaolai Basin, Liaoshang type gold deposit, stepwise metallogenic, detachment fault, prospecting direction, Shandong Province

CLC Number: 

  • P618.51 

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