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Gold Science and Technology ›› 2019, Vol. 27 ›› Issue (6): 791-801.doi: 10.11872/j.issn.1005-2518.2019.06.791

• Mineral Exploration and Resource Evaluation •     Next Articles

Study on Geochemical Background Field of the Gold Deposits in Jiaodong，China

Yumin CHEN1(),Qingdong ZENG2,3,4(),Zhifu SUN5,Zhaokun WANG1,Hongrui FAN2,3,4,Fengli XIAO1,Shaoxiong CHU2,3   

  1. 1. Shandong Gold Group Co. ，Ltd. ，Jinan 250101，Shandong，China
    2. Key Laboratory of Mineral Resources，Institute of Geology and Geophysics，Chinese Academy of Sciences，Beijing 100029，China
    3. Innovation Academy of Earth Science，Chinese Academy of Sciences，Beijing 100029，China
    4. College of Earth Sciences，University of Chinese Academy of Sciences，Beijing 100049，China
    5. Shandong Gold Geology and Mineral Exploration Co. ，Ltd. ，Laizhou 261400，Shandong，China
  • Received:2019-08-22 Revised:2019-10-28 Online:2019-12-31 Published:2019-12-24
  • Contact: Qingdong ZENG E-mail:chenym@sd-gold.com;zengqingdong@mail.iggcas.ac.cn

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Abstract:

Jiaodong gold ore-concentrating area is the third largest gold mining area in the world after the Lande gold mining area in South Africa and Muruntau gold mining area in Uzbekistan，and its proved gold resources exceed 4 500 t.Jiaodong gold ore-concentrating area formed in the Early Cretaceous tectonic regime transition period and has the characteristics of large-scale concentrated mineralization.This area is composed of a lot of super-large，large gold deposits and includes altered rock type，quartz vein type and interlayer fracture zone type gold deposit.The typical altered rock type gold deposits are Sanshandao，Jiaojia，Xincheng，Dayingezhuang，Xiadian and Dongfeng 171 deposits，and so on.The quartz vein type gold deposits include Linglong，Jinqingding and Denggezhuang deposits，and so on.The interlayer fracture zone type gold deposits are represented by the Pengjiakuang gold deposit.These gold deposits are mainly controlled by the regional faults，secondary faults and interlayer slide faults along the northern margin of the Laiyang basin.The gold deposits in Jiaodong mainly occur within the Mesozoic granite，minor whthin Jiaodong Group，Jingshan Group and Mesozoic strata.This paper selects the scientific problem of the source of ore-forming materials，and systematically analyzes the surface and deep-drilling samples sampled from the Jiaodong area by means of Au element geochemical analysis，in order to reveal the geochemical background characteristics of Au element in this area，and provides geochemical field constraints for discussing the metallogenic mechanism of high-intensity massive accumulation of Au element in this area.The results show that the average abundance of Au element (1.10×10-9) of the Jiaodong group is lower than that of Clark value of continental crust (1.21×10-9) and the value of continental crust of North China Platform，which shows the characteristic of gold deficit geochemical field.Moreover，the results also show that the gold geochemical background feild of the Jiaodong group is characterized by higher average Au abundance in the central area (1.35×10-9) and lower average Au abundance in the east and west of the Jiaodong area (0.95×10-9 and 0.76×10-9).The average abundance of Au element in the fresh rock samples of different rock types (Jiaodong Group,0.79×10-9；Mesozoic granites,0.77×10-9；Gabbro,0.63×10-9；Lamprophyre,0.93×10-9；Acidic dykes,0.82×10-9) from the deep drilling holes is lower than that of Clark value of continental crust and the value of continental crust of North China Platform，which also display the characteristic of gold geochemical deficit field.Therefore，there exists an Au element geochemical deficit field in the Jiaodong ore-concentrating area，combined with the evidence of hydrothermal activities in gold ore areas，we think the Jiaodong Group and the Mesozoic granite might partly provide the source of metallogenic materials for the formation of gold deposits in the Jiaodong area.

Key words: geochemical background field, gold abundance, material resource, gold ore-concentrating area, deep drilling, Jiaodong

CLC Number: 

  • P618.51

Fig.1

Geological sketch map of the gold deposits in Jiaodong area and sampling location of the gold geochemical samples（modified after Chen,et al[10]）"

Table 1

Statistical of geochemical analysis results of gold element of the surface samples in Jiaodong area"

岩石类型w（Au）/（×10-9）w（Au）最小值/（×10-9）w（Au）最大值/（×10-9）样品数量/件样品采集地区
胶东群变质岩0.760.471.086胶西北（莱州—招远）
荆山群大理岩0.720.550.92胶西北（莱州—招远）
玲珑花岗岩0.730.431.2641胶西北（莱州—招远）
郭家岭花岗岩0.690.480.957胶西北（莱州—招远）
中基性岩脉0.630.610.643胶西北（莱州—招远）
胶东群变质岩1.350.533.5315胶东中部（栖霞）
胶东群变质岩0.950.721.5812胶东东部（牟乳—文登）
中生代花岗岩1.180.526.3518胶东东部（牟乳—文登）
大陆地壳1.21中国东部
华北地台大陆地壳1.01 207华北地台

Table 2

Statistical of gold element analysis results of rock core samples of the deep drill holes from the Sanshandao gold deposit，northwest Jiaodong"

岩性w(Au)/（×10-9）w(Au)最小值/（×10-9）w(Au)最大值/（×10-9）样品数量/件样品采集地区
胶东变质岩0.790.281.8994胶西北三山岛金矿
中生代花岗岩0.770.262.50209胶西北三山岛金矿
蚀变岩152.300.335 520108胶西北三山岛金矿
辉长岩0.630.301.6418胶西北三山岛金矿
煌斑岩0.930.461.8310胶西北三山岛金矿
酸性脉岩0.820.331.4513胶西北三山岛金矿
大陆地壳1.21中国东部
华北地台大陆地壳1.01 207华北地台

Fig.2

Columnar diagram and gold abundance map of the deep drill holes in Sanshandao gold mine area"

Table 3

Gold abundances of the major rocks in Jiaodong area，metamorphic rocks and igneous rocks in east China，and major metamorphic rocks in North China Platform"

岩性样品数量/件w（Au）/（×10-9）资料来源
胶东群斜长角闪岩1212.17张韫璞等[44]
胶东群斜长角闪岩7024.2杨士望[20]
胶东群斜长角闪岩9163朱奉三[45]
胶东群斜长角闪岩4姚凤良等[46]
胶东群斜长角闪岩455杨敏之等[47]
胶东群黑云变粒岩22.5杨敏之等[47]
胶东群二云片岩412杨敏之等[47]
胶东群变粒岩7170杨敏之等[47]
胶东群斜长角闪岩621杨敏之等[47]
玲珑花岗岩444.5姚风良等[46]
郭家岭花岗岩306.1姚风良等[46]
煌斑岩315姚风良等[46]
荆山群斜长角闪岩10202杨敏之等[47]
荆山群斜长浅粒岩4150杨敏之等[47]
荆山群石榴石大理岩325杨敏之等[47]
荆山群云母条带大理岩391杨敏之等[47]
荆山群云母片岩330杨敏之等[47]
荆山群黑云石英片岩418杨敏之等[47]
华北地台变粒岩3951.0迟清华等[32]
华北地台麻粒岩3171.4迟清华等[32]
华北地台斜长角闪岩3381.2迟清华等[32]

Fig.3

Fine veins of the hydrothermal activities from the deep drill rock core （ZK965） in Sanshandao gold mine area，northwest Jiaodong"

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