焦家式金矿勘查与研究

周明岭; 孙亮亮; 吕军阳; 王斌; 刘向东; 鲍中义; 张琪彬; 周晓萍; 解天赐; 王珊珊; 刘彩杰; 徐韶辉; 闫春明; 张朋; 张亮亮; 杨真亮; 范家盟; 赵成乐; 郭美丽; 李瑞翔

doi:10.12090/j.issn.1006-6616.2024061

焦家式金矿勘查与研究

doi: 10.12090/j.issn.1006-6616.2024061

周明岭^{1, 2,},
孙亮亮^{1, 2,},
吕军阳^{1, 2},
王斌^{1, 2},
刘向东^{1, 2},
鲍中义^{1, 2},
张琪彬^{1, 2},
周晓萍^{1, 2},
解天赐^{1, 2},
王珊珊^{1, 2},
刘彩杰^{1, 2},
徐韶辉^{1, 2},
闫春明^{1, 2},
张朋^{1, 2},
张亮亮^{1, 2},
杨真亮^{1, 2},
范家盟^{1, 2},
赵成乐^{1, 2},
郭美丽^{1, 2},
李瑞翔^{1, 2}

1.
山东省地质矿产勘查开发局第六地质大队，山东威海 264209
2.
自然资源部深部金矿勘查开采技术创新中心，山东威海 264209

详细信息

作者简介:
周明岭（1968—），男，学士，研究员，从事地质矿产勘查与研究。Email：lyzhouml@126.com

中图分类号: P61；P624
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- 文章访问数: 152
- HTML全文浏览量: 16
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- 被引次数: 0
出版历程
- 收稿日期: 2024-05-29
- 修回日期: 2024-09-12
- 录用日期: 2024-10-09
- 预出版日期: 2024-10-10
- 刊出日期: 2024-10-28

Exploration and scientific research of the Jiaojia-type gold deposit

ZHOU Mingling^{1, 2
,},
SUN Liangliang^{1, 2
,},
LYU Junyang^{1, 2},
WANG Bin^{1, 2},
LIU Xiangdong^{1, 2},
BAO Zhongyi^{1, 2},
ZHANG Qibin^{1, 2},
ZHOU Xiaoping^{1, 2},
XIE Tianci^{1, 2},
WANG Shanshan^{1, 2},
LIU Caijie^{1, 2},
XU Shaohui^{1, 2},
YAN Chunming^{1, 2},
ZHANG Peng^{1, 2},
ZHANG Liangliang^{1, 2},
YANG Zhenliang^{1, 2},
FAN Jiameng^{1, 2},
ZHAO Chengle^{1, 2},
GUO Meili^{1, 2},
LI Ruixiang^{1, 2}

1.
No. 6 Geological Team of Shandong Provincial Bureau of Geology and Mineral Resources, Weihai 264209, Shandong, China
2.
Ministry of Natural Resources Technology Innovation Center for Deep Gold Resources Exploration and Mining, Weihai 264209, Shandong, China

More Information

Author Bio:
周明岭，二级研究员，中共党员，原山东省地质矿产勘查开发局第六地质大队副队长、总工程师。1991年毕业于中国地质大学（北京）地质学专业，获学士学位。2023年荣获第十八次李四光地质科学奖野外奖。周明岭同志长期坚持扎根野外一线，主要从事以金为主的地质矿产勘查、区域地质调查和地质科学研究工作，主持和参与完成地质勘查和科研项目100余项，在胶东地区连续探获了焦家深部、朱郭李家、前陈、纱岭、玲南、水旺庄、姜家窑、西涝口等大型—超大型金矿床10余处，累计探明金资源量1400余吨。不断丰富和发展了焦家式金矿成矿理论，参与“胶东焦家金矿田千吨金矿勘查理论和关键技术”“胶东金矿理论技术创新与深部找矿突破”等研究工作，研发创新了金矿深部找矿技术和方法。先后发表具有重要影响的学术论文20余篇（其中SCI论文5篇、EI论文4篇），专著6部，授权发明专利2项。个人荣获国家科技进步二等奖1项，省部级科学技术奖一等奖1项、二等奖2项，荣获“山东省有突出贡献的中青年专家”“山东省国土资源系统先进个人”“山东省找矿突破战略行动（2011—2013年度）先进个人”“山东省地矿局第二届曹国权地质科学奖”“山东省地矿局第二批科技领军人才”“山东省地矿局‘十一五’优秀科技工作者”等荣誉称号

摘要

摘要: 焦家式金矿是20世纪60年代山东地质工作者在胶东西北部发现的金矿类型，其产出受区域性构造破碎带控制，成矿期普遍发生黄铁绢英岩化蚀变，成矿特征是规模大、蚀变分带明显、矿化集中、矿体形态简单、品位相对均匀、矿物组合简单。从发现到确立金矿类型经历了12年的勘查研究历程，在此之后得以迅速推广，并在胶东及全国多地取得了丰硕的找矿成果。21世纪以来，胶东地区焦家式金矿深部勘查成果不断涌现。截至2020年，累计提交金资源储量3617.12 t，助推胶东地区成为世界第三大金矿集区，中国黄金储量跃居世界第二。同时，对焦家式金矿的研究工作也取得了长足进展：成矿时代被精确限定在126~120 Ma；金矿形成于区域强烈伸展背景下，成矿物质来源具有多源性，太古代拉斑玄武岩为含金初始矿源岩；将成矿过程精细划分为4个阶段，并提出“热隆−伸展”成矿理论和“阶梯式”成矿模式；成矿深度为5~10 km，成矿后剥蚀厚度为5.2±1.2 km，矿床保存较好；胶西北地区三山岛、焦家和招平三大成矿带5000 m以浅预测金资源总量为7258~10150 t，显示出焦家式金矿深部巨大的找矿潜力。从浅部到深部不同勘查阶段总结出一套关键勘查技术组合。这些研究成果丰富完善了焦家式金矿成矿理论体系，使得成矿预测更加准确可靠，有力指导了胶东地区金矿勘查。
- 焦家式金矿 /
- 成矿特征 /
- 成矿模式 /
- 金矿勘查 /
- 胶东
Abstract: [Objective] Jiaojia-type gold deposit is a new type of gold mine discovered by Shandong geologists in northwestern Jiaodong in the 1960s, and its output is controlled by regional tectonic fracture zones. Pyrite sericitized alteration generally occurred during the ore-forming period, which is characterized by a large scale, distinct alteration zones, concentration of mineralization, simple morphology of the ore body, relatively uniform grade, and simple mineral combinations. The deposit has gone through 12 years of exploration and scientific research, from discovery to establishment. [Methods] This new type of gold deposit has been rapidly promoted since its establishment and has achieved fruitful prospecting results in China. Deep exploration achievements of the Jiaojia-type gold deposit have been coming up in the Jiaodong area since the 21st century. [Results] The accumulated gold resource reserves submitted have been 3617.12 tons by 2020, which has helped the Jiaodong area become the third largest gold cluster in the world, and gold reserves of China have risen to the second rink in the world. Research on the Jiaojia-style gold mine has also made considerable progress, with the age of mineralization accurately limited to 126~120 Ma and formation occurring under a strong regional extension background. The source of mineralization material has multiple origins, with the Archean tholeiite being the initial source rock of gold-bearing minerals. The ore-forming process is divided into four stages, and the “thermo-extension”metallogenic theory and the step metallogenic model are proposed. The metallogenic depth is about 5~10 km, and the post-metallogenic denudation thickness is 5.2±1.2 km, with the deposits well preserved. [Conclusion] The metallogenic prediction study concluded that the total gold resources in the three major metallogenic zones of Sanshandao, Jiaojia, and Zhaoping in the northwestern Jiaozhou area were 7258~10150 tons of metal at a depth of 5000 m, which demonstrates the immense potential of the deeper part of the Jiaojia-type gold deposits for exploration. A set of key exploration techniques was summarized for different exploration stages, from shallow to deep. [Significance] These studies enriched the metallogenic theory of the Jiaojia-type gold deposit, making the metallogenic prediction results highly accurate, reliable, and effective in guiding the gold exploration in the Jiaodong peninsula.
- Jiaojia-type gold deposit /
- mineralization characteristics /
- metallogenic model /
- gold exploration /
- Jiaodong

HTML全文

图 1 胶东地区区域地质图及金矿分布图

F₁—三山岛−仓上断裂带；F₂—龙口−莱州断裂带；F₃—招远−平度断裂带；F₄—西林−陡崖断裂带；F₅—桃村断裂带；F₆—郭城断裂带；F₇—朱吴断裂带；F₈—海阳断裂带；F₉—金牛山断裂带

Figure 1. Regional geological map and distribution of gold deposits in the Jiaodong area

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图 2 胶东西北部地区焦家式金矿控矿断裂组合示意图

F₁—三山岛−仓上断裂带；F₂—龙口−莱州断裂带；F₃—招远−平度断裂带

Figure 2. Schematic diagram of the ore-controlling fault pattern in the northwest Jiaodong area

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图 3 焦家式金矿构造−蚀变−矿化分带模式（据李士先等，2007修改）

Figure 3. Structure-alteration-mineralization zoning model of the Jiaojia-type gold deposit （modified by Li et al.，2007）

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图 4 胶东各类型金矿吨位−品位图

其他类型金矿包含石英脉型、石英脉−蚀变岩型和斑岩型

Figure 4. Tonnage-grade diagram of various gold deposit types in the Jiaodong area

Note: Other gold deposites include quartz vein, quartz vein-alteration and porphyry.

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图 5 焦家式金矿床典型类型金矿石照片

a、b—浸染状黄铁绢英岩化碎裂岩型；c、d—浸染状−细脉状−网脉状黄铁绢英岩化花岗质碎裂岩型；e、f—细脉状−网脉状黄铁绢英岩化花岗岩型

Figure 5. Typical gold ore photograph of the Jiaojia-type gold deposit

(a、b) Disseminated pyrite sericite cataclastic type； (c、d) Disseminated-veined-reticulated porphyritic sericite granitic cataclastic type；(e、f) Veined-reticulated pyritic sericitization granite type

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图 6 胶东金矿区域成矿模式图（据宋明春等，2014b修改）

Figure 6. Regional metallogenetic model of the Jiaodong gold deposit （modified by Song et al.，2014b）

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图 7 台上−水旺庄金矿床地质勘查模型

Figure 7. Geological exploration model of the Taishang-Shuiwangzhuang gold deposit

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图 8 三山岛−焦家金矿田重磁联合反演模拟计算的地质剖面图（据曹春国等，2012修改）

Figure 8. Geological profile of the combined gravity and magnetic inversion simulation of the Sanshandao-Jiaojia gold field （modified by Cao et al.，2012）

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图 9 焦家式金矿典型矿床矿化富集规律及成矿预测图

Figure 9. Mineralization enrichment regularity and metallogenic prediction of the typical Jiaojia-type gold deposit

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图 10 浅部勘查阶段各成矿带提交金资源储量和查明矿床数量及其占比

a—金资源储量及占比；b—矿床数量及占比

Figure 10. Ratio of submitted gold resources and quantity of identified deposits in each metallogenic belt during the shallow exploration stage

(a) Gold resource reserves; (b) Proportion of deposits

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图 11 深部勘查阶段各成矿带提交金资源储量和查明矿床数量及其占比

a—金资源储量及占比；b—矿床数量及占比

Figure 11. Ratio of submitted gold resources and quantity of identified deposits in each metallogenic belt during the deep exploration stage

(a) Gold resource reserves; (b) Proportion of deposits

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