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Gold Science and Technology ›› 2019, Vol. 27 ›› Issue (3): 315-327.doi: 10.11872/j.issn.1005-2518.2019.03.315

• Mineral Exploration and Resource Evaluation • Previous Articles     Next Articles

Research on Ore-Control Conditions and Metallogenic Law of Gold Deposits in Central Zhaoping Fault,Eastern Shandong Province

Weiqing SUN1(),Shen LIU2(),Caixia FENG2,Yan FAN2,Yongchang LIU3   

  1. 1. Shandong Institute of Geology Sciences,Key Laboratory of Gold Mineralization Process and Resources Utilization,Ministry of Land and Resources,Key Laboratory of Metal Mineralization Geological Processes and Resources Utilization in Shandong Province,Jinan 250013,Shandong,China
    2. Department of Geology,Northwest University,Xi’an 710069,Shaanxi,China
    3. Shandong Zhengyuan Geological Exploration Institute,General Administration of Metallurgical Geology of China,Yantai 264000,Shandong,China
  • Received:2019-01-02 Revised:2019-03-21 Online:2019-06-30 Published:2019-07-10
  • Contact: Shen LIU E-mail:swq_1970@163.com;liushen@nwu.edu.cn

Abstract:

As one of the famous gold-enriched areas in China,a large number of super-large,large and medium-sized gold deposits have been discovered in Jiaodong Peninsula.Some research had been carried out on the formation mechanism,metallogenic epoch,material source,division of regional metallogenic belt and the temporal-spatial relationship between main geological bodies and gold mineralization in Jiaodong Peninsula.But there is still a lack of detailed understanding of the tectonic ore-controlling conditions,distribution regularities and occurrence regularities of gold deposits in this area.In this study,the regional geological characteristics,the geological characteristics of gold deposits and the ore-controlling characteristics of faulted structures and the metallogenic regularity of gold deposits are discussed,which will provide a reasonable explanation for the above-mentioned scientific problems,and hopefully provide a possible guidance for later prospecting.The middle section of Zhaoping Fault is an important gold metallogenic belt in Jiaodong Peninsula.The following typical gold deposits have attracted possible concerns:(1)Xiadian super large gold deposit and Dayingezhuang super large gold deposit;(2)Jiangjiayao,Caojiawa and Jiaogezhuang medium and small gold deposits.Nevertheless,the structural ore-controlling conditions,distribution regularity and ore body occurrence regularity of various gold deposits distributed in the middle part of the fault zone are still the main problems to be solved urgently.Based on the analysis and summary of the geological characteristics,gold deposit geological characteristicsBased on the analysis and summary of the geological characteristics,gold deposit geological characteristics,structural ore-controlling characteristics and gold metallogenic regularity of Xiadian large-scale gold deposit,Dayingezhuang super large scale gold deposit and Jiaogzhuang small-sized gold deposit,the following results and understandings are obtained.Dayingezhuang super large gold deposit is mainly controlled by Zhaoping main fault.Xiadian super large gold deposit is mainly controlled by main ore-controlling faults associated with lower wall,derived low-grade and low-order faults.Xiadian Beiqu orebody is controlled by local tensional micro-fracture zone of rock mass in lower wall of main fault.The Dayingezhuang,Xiadian and Jiaogezhuang gold deposits in the middle section of Zhaoping Fault zone are approximately isometric.The intersection of nearly EW-trending faults and Zhaoping Faults is favorable for mineralization.The bend or intersection of faults is the main ore-hosting part.

Key words: gold deposit, ore control conditions, metallogenic law, ore-body occurrence law, Zhaoping fault, Shandong Province

CLC Number: 

  • P618.51

Fig.1

Geological and gold deposits distribution map of northwestern Jiaodong"

Fig.2

Photomicrograph of pyrite and chalcopyrite in Dayingezhuang super large gold deposit"

Fig.3

Photomicrograph of galena and sericite in the Dayingezhuang super large gold deposit"

Fig.4

Ore structure and tectonic map of the Dayingezhuang super large gold deposit"

Table 1

Analysis and comparison of ore combination(×10-6)"

元素 核实报告品位 本次报告品位
Au 2.8 2.74
Ag 12.49 14.11
Cu 700 120
Pt 900 490
Zn 400 190
S 14 200 8 760

Table 2

Orebody characteristics of Jiaogezhuang small gold deposit"

矿体编号 勘探线 矿体长度/m 形状 走向 倾向 倾角/(°) 矿体厚度/m 平均金品位/(×10-6 斜向长度/m 斜深/m
15~40 359 鞍状 SE SE 20~38 2.62 2.42 550 740
19~18 227 透镜状 SE SE 28~34 3.75 2.23 378 441
20~40 174 透镜状 SE SE 33~37 1.6 2.05 194 303
18 60 透镜状 SE SE 34 0.83 1.51 45 120
V 4~11 43 透镜状 SE SE 27~31 1.09 2.29 140 89
0 43 透镜状 SE SE 31 0.86 1.92 60 120

Table 1

Mineral composition statistics of Jiaogezhuang small gold deposit"

矿物种类 矿石矿物 碳酸盐矿物 脉石矿物
金属矿物 硫化矿物 氧化矿物
主要矿物 银金矿 黄铁矿 - 菱铁矿 石英
次要矿物 - 方铅矿、闪锌矿、黄铜矿 褐铁矿 - 绢云母
少量矿物 - 辉铜矿、斜方辉铅铋矿 铜蓝 - 钾长石、绿泥石

Fig.5

Characteristics of orebodies and gold minerralization in the middle section of Zhaoping fault zone"

Fig.6

Clastic rock and quartz vein type gold mineralization in the middle section of Zhaoping fault zone"

Fig.7

Distribution regularity of gold deposits in the middle section of Zhaoping fault zone"

Fig.8

Distribution regularity of gold orebodies in the middle section of Zhaoping fault zone"

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