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黄金科学技术 ›› 2019, Vol. 27 ›› Issue (3): 315-327.doi: 10.11872/j.issn.1005-2518.2019.03.315

• 矿产勘查与资源评价 • 上一篇    下一篇

招平断裂带中段金矿床控矿条件与成矿规律研究

孙伟清1(),刘燊2(),冯彩霞2,范焱2,刘永昌3   

  1. 1. 山东省地质科学研究院,国土资源部金矿成矿地质过程与资源利用重点实验室,山东省金属矿产成矿地质过程与资源利用重点实验室,山东 济南 250013
    2. 西北大学地质学系,陕西 西安 710069
    3. 中国冶金地质总局山东正元地质勘查院,山东 烟台 264000
  • 收稿日期:2019-01-02 修回日期:2019-03-21 出版日期:2019-06-30 发布日期:2019-07-10
  • 通讯作者: 刘燊 E-mail:swq_1970@163.com;liushen@nwu.edu.cn
  • 作者简介:孙伟清(1970-),男,山东济南人,高级工程师,从事矿床学研究工作。swq_1970@163.com
  • 基金资助:
    中国地质调查局老矿山找矿项目“山东省招远市招平断裂带中段深部金矿战略性勘查”(1212011220694)

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

摘要:

招平断裂带中段为胶东地区重要的金成矿带,目前已查明的金矿床主要包括夏甸大型金矿床和大尹格庄特大型金矿床,姜家窑和曹家洼中型金矿床,以及焦格庄小型金矿床。研究人员对招平断裂带中段各类金矿床的构造控矿条件、分布规律和矿体赋存规律仍缺乏较系统的认识,亟待开展进一步研究。通过对金矿区地质特征、金矿床地质特征、构造控矿特征和金矿成矿规律进行分析和总结,得出大尹格庄特大型金矿主要受招平主干断裂控制;夏甸大型金矿床主要受控于主干控矿断裂下盘伴生、派生的低级和低序次断裂,夏甸北耩矿体主要受控于主断裂下盘岩体局部张性显微裂隙带;招平断裂带中段大尹格庄特大型金矿床、夏甸特大型金矿床和焦格庄中、小型金矿床大致呈等间距分布,近EW向断裂与招平断裂的交会部位是有利成矿部位;断裂的拐弯或交会部位为主要赋矿部位。

关键词: 金矿床, 控矿条件, 成矿规律, 矿体赋存规律, 招平断裂带, 山东省

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

中图分类号: 

  • P618.51

图1

胶东西北部地质及金矿床分布图[25] "

图2

大尹格庄特大型金矿黄铁矿和黄铜矿显微照片"

图3

大尹格庄特大金矿方铅矿和绢云母显微照片"

图4

大尹格庄特大型金矿矿石结构和构造图"

表1

矿石组合分析对比"

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

表 2

焦格庄小型金矿床矿体特征"

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

表 3

焦格庄小型金矿床矿石矿物成分统计"

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

图5

招平断裂带中段金矿体和金矿化特征"

图6

招平断裂带中段碎裂岩和石英脉型金矿化"

图7

招平断裂带中段金矿床分布规律"

图8

招平断裂带中段金矿体分布规律"

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