img

QQ群聊

img

官方微信

高级检索

黄金科学技术 ›› 2017, Vol. 25 ›› Issue (3): 38-45.doi: 10.11872/j.issn.1005-2518.2017.03.038

• 专题报道 • 上一篇    下一篇

招平断裂北段水旺庄深部超大型金矿床的发现、特征和找矿方向

刘国栋,温桂军,刘彩杰,鲍中义*,孙忠全,范家盟,李山,闫春明,郭志峰   

  1. 山东省第六地质矿产勘查院,山东  招远  265400
  • 收稿日期:2017-03-03 修回日期:2017-04-23 出版日期:2017-06-30 发布日期:2017-09-11
  • 通讯作者: 鲍中义(1979-),男,河北藁城人,工程师,从事地质矿产勘查和研究工作。gybzy2005@126.com
  • 作者简介:刘国栋(1978-),男,山东招远人,助理工程师,从事地质矿产勘查和研究工作。27888355@qq.com
  • 基金资助:

    山东省泰山学者建设工程专项经费“胶东型金矿的构造岩浆背景和深部找矿关键技术”(编号:ts201511076)和2016年度山东省地矿局地质科技攻关项目“招平断裂带北段控矿构造及找矿方向研究”(编号:KY2016011)联合资助

Discovery,Characteristics and Prospecting Direction of Shuiwangzhuang Deep Super-large Gold Deposit in the Northern Section of Zhaoping Fault

LIU Guodong,WEN Guijun,LIU Caijie,BAO Zhongyi,SUN Zhongquan,FAN Jiameng,LI Shan,YAN Chunming,GUO Zhifeng   

  1. 6th Geology & Mineral Resources Survey Institute,Shandong,Zhaoyuan    265400,Shandong,China
  • Received:2017-03-03 Revised:2017-04-23 Online:2017-06-30 Published:2017-09-11

摘要:

水旺庄矿区位于玲珑金矿田外围,深部找矿难度非常大。在深入分析断裂深部成矿规律的基础上,提出了“胶西北三大断裂赋矿深度对称、矿体规模对称—对称成矿”的新认识,在曾被国外专家放弃勘查的水旺庄矿区发现并探获金金属量达170 t的深部超大型金矿床,将招平断裂勘查深度延伸至标高-2 173 m。金矿体分别赋存于破头青断裂和九曲断裂中,尤其是赋存于九曲断裂中的2号主矿体规模最大,单矿体金金属量超过120 t。水旺庄矿区深部找矿成果揭示,九曲断裂为招平断裂北段主干断裂,该断裂(208号脉)沿走向向北东1 800~5 000 m范围是深部找矿的优质靶区,招平断裂深部找矿潜力巨大。

关键词: 对称成矿, 深部找矿, 成矿规律, 九曲断裂, 招平断裂, 玲珑金矿田, 水旺庄金矿区

Abstract:

Shuiwangzhuang mining area is located in the peripheral area of the Linglong gold orefield,and the deep ore prospecting of the area is very difficult.Based on the in-depth analysis of deep metallogenic regularity of fault,this paper presents a new understanding named symmetric mineralization that the ore bearing depth and orebody scale of the three main faults in northwestern Jiaodong Peninsula are symmetrical,finds Shuiwangzhuang deep-seated super-large gold deposit where had been abandoned by foreign experts and is seized gold metal amounts to 170 t,so the depth of the exploration of the fault extends to the elevation of -2 173 m.Gold orebodies are hosted in Potouqing fault and Jiuqu fault,especially the No.2 main orebody in Jiuqu fault is the largest one,which gold metal amounts of single ore exceeds 120 t.The deep prospecting results reveal that Jiuqu fault is the main fault in the northern Zhaoping fault,the range of 1 800 m to 5 000 m along the strike of the fault (No.208) to the east of the north is high quality target area for deep ore prospection,so there is a great potential for prospecting in the deep part of Zhaoping fault.

Key words: symmetric mineralization, deep prospecting, metallogenic regularity, Jiuqu fault, Zhaoping fault, Linglong gold orefield, Shuiwangzhuang gold mining area

中图分类号: 

  • P618.51 

[1]  Song Mingchun.The main achievements and key theory and methods of deep-seated prospecting in the Jiaodong gold concentration area,Shandong Province[J].Geological Bulletin of China,2015,34(9):1758-1771.[宋明春.胶东金矿深部找矿主要成果和关键理论技术进展[J].地质通报,2015,34(9):1758-1771.]
[2] Cui Shuxue,Yuan Wenhua,Yang Zhili.Geological characte- ristics in the deep of Sizhuang gold deposit in Laizhou City[J].Northwestern Geology,2008,41(4):82-92.[崔书学,袁文花,杨之利.莱州寺庄金矿床深部地质特征[J].西北地质,2008,41(4):82-92.]
[3] Lin Wenwei,Zhao Yiming,Xu Yu.Active properties and age of Zhaoyuan-Pingdu fracture zone[J].Regional Geology of China,2000,19(1):36-51.[林文蔚,赵一鸣,徐钰.胶东招远—平度断裂活动性质及活动时代[J].中国区域地质,2000,19(1):36-51.]
[4] Song Mingchun,Cui Shuxue,Yang Zhili,et al.Great progress and far-reaching significance of deep exploration in the Jiaojia  metallogenic belt,Shandong Province[J].Geology and Prospecting,2008,44(1):1-8.[宋明春,崔书学,杨之利,等.山东焦家金矿带深部找矿的重大突破及其意义[J].地质与勘探,2008,44(1):1-8.]
[5] Gao Shujian,Wei Xufeng,Sun Ruigang,et al.Geological cha- racteristics and ore prospecting future in deep part of Matang gold deposit in Laizhou City[J].Shandong Land and Resources,2010,26(6):7-12.[高书剑,魏绪峰,孙瑞刚,等.莱州马塘金矿地质特征与深部找矿远景[J].山东国土资源,2010,26(6):7-12.]
[6] Song Mingchun,Yi Pihou,Xun Junxiang,et al.A step meta- llogenetic model for gold deposits in the northwestern Shandong Peninsula,China[J].Science China:Earth Sciences,2012,55:940-948.[宋明春,伊丕厚,徐军祥,等.胶西北金矿阶梯式成矿模式[J].中国科学(地球科学),2012,55:940-948.]
[7] Wang Zhenjun,Li Weiming,Yuan Bo.Features of structural superimposed halos in Sanshandao-Xinli-Cangshang gold deposits,Shandong Province[J].Gold Science and Technology,2013,21(4):48-53.[王振军,李伟明,原波.山东三山岛—新立—仓上金矿床构造叠加晕特征浅析[J].黄金科学技术,2013,21(4):48-53.]
[8] Liu Dianhao,Lv Guxian,Zhang Pijian,et al.A study of 3D ore-controlling of the tectonic altered rocks of the Sanshandao fault in Jiaodong Peninsula and the discovery of an offshore super-large gold deposit in China[J].Earth Science Frontiers,2015,22(4):162-172.[刘殿浩,吕古贤,张丕建,等.胶东三山岛断裂构造蚀变岩三维控矿规律研究与海域超大型金矿的发现[J].地学前缘,2015,22(4):162-172.]
[9] Song Mingchun,Zhang Junjin,Zhang Pijian,et al.Discovery and tectonic-magmatic background of superlarge gold deposit in offshore of northern Sanshandao,Shandong Peninsula,China[J].Acta Geologica Sinica,2015,89(2):365-383.[宋明春,张军进,张丕建,等.胶东三山岛北部海域超大型金矿床的发现及其构造—岩浆背景[J].地质学报,2015,89(2):365-383.]
[10] Zhang Pijian,Song Mingchun,Liu Dianhao,et al.Features of deepseated gold orebodies of No.171 lode and structural ore-controlling action in Linglong gold orefield,Shandong Peninsula[J].Mineral Deposits,2015,34(5):855-873.[张丕建,宋明春,刘殿浩,等.胶东玲珑金矿田171号脉深部金矿床特征及构造控矿作用[J].矿床地质,2015,34(5):855-873.]
[11] Jiang Weiming,Qi Wen,Meng Wei,et al.Study on the metallogenic regularity and prospective prognosis in Linglong Dongfeng mining area,Shandong Province[J].Gold Science and Technology,2012,20(4):21-25.[姜维明,齐斐,孟伟,等.山东玲珑矿田东风矿区成矿规律及远景预测[J].黄金科学技术,2012,20(4):21-25.]
[12] Song Mingchun,Cui Shuxue,Yi Pihou,et al.Prospecting and Metallogenic Model of Deep Large and Super-large Gold Deposits in the Gold Concentration Area,Northwest China[M].Beijing:Geological Publishing House,2005.[宋明春,崔书学,伊丕厚,等.胶西北金矿集中区深部大型—超大型金矿找矿与成矿模式研究[M].北京:地质出版社,2005.]
[13] Song Mingchun,Song Yingxin,Cui Shuxue,et al.Characte- ristic comparison between shallow and deepseated gold ore bodies in Jiaojia superlarge gold deposit,northwestern ShandongPeninsula[J].Mineral Deposits,2011,30(5):923- 932.[宋明春,宋英昕,崔书学,等.胶东焦家特大型金矿床深、浅部矿体特征对比[J].矿床地质,2011,30(5):923-932.]
[14] Shi Yuchen,Liu Changchun,Yang Chenghai,et al.Distri- bution relation and genesis of alterted and quartz-vein gold deposits in east Shandong[J].Shandong Land and Resources,2005,21(8):19-21.[石玉臣,刘长春,杨承海,等.胶东地区蚀变岩型与石英脉型金矿的空间分布关系及形成机制[J].山东国土资源,2005,21(8):19-21.]
[15] Cui Shuxue.Analysis on south widening and ore prospecting future of Jiaojia fault belt[J].Shandong Land and Resources,2007,23(10):7-10.[崔书学.焦家断裂带南延问题及南延段找矿前景分析[J].山东国土资源,2007,23(10):7-10.]
[16] Bao Zhongyi,Sun Zhongquan,Liu Guodong.Geological cha- racteristics and prospecting direction of deposits in Shui- wangzhuang area in Potouqing fault[J].Shandong Land and Resources,2014,30(2):29-33.[鲍中义,孙忠全,刘国栋.破头青断裂水旺庄矿区矿床地质特征及找矿方向[J].山东国土资源,2014,30(2):29-33.]
[17] Li Shixian,Liu Changchun,An Yuhong,et al.Geology of Jiaodong Gold Deposits[M].Beijing:Geological Publishing House,2007.[李士先,刘长春,安郁宏,等.胶东金矿地质[M].北京:地质出版社,2007.]

[1] 曲晖, 王佰义, 王建民, 李成禄, 徐国战, 王卓. 土壤地球化学测量在永新金矿勘查中的应用及找矿效果研究[J]. 黄金科学技术, 2018, 26(2): 143-152.
[2] 郑慕婷,张术根,贺忠春. 湖南康家湾金银多金属矿床金银赋存状态及其与成矿演化的关系[J]. 黄金科学技术, 2017, 25(6): 31-42.
[3] 陈彩华,孙斌,陈冀,陈力子 . 西秦岭中寨—十里铺地区水系沉积物测量找矿效果[J]. 黄金科学技术, 2017, 25(4): 1-9.
[4] 张磊,佟宇,杨振东,白云龙,刘幸,赵永涛. 辽宁苇子沟地区金铜多金属矿成矿机制及找矿方向[J]. 黄金科学技术, 2017, 25(4): 10-17.
[5] 万鹏,丁正江,胡弘,吴凤萍,程蓉蓉,邹键 . 胶东邓格庄金矿床深部成矿特征及找矿方法组合[J]. 黄金科学技术, 2017, 25(3): 46-53.
[6] 宋英昕. 胶东三山岛北部海域金矿床蚀变矿物短波红外光谱特征及其对深部找矿的启示[J]. 黄金科学技术, 2017, 25(3): 54-60.
[7] 王志新,焦秀美,丁正江,刘晓敏,李国华,纪旭波,唐俊智. 胶莱盆地东北缘辽上式金矿构造控矿特征及找矿方向[J]. 黄金科学技术, 2017, 25(3): 61-69.
[8] 吴二,陈远荣,刘奕志,蓝妮拉,冯莉. 辽宁白云金矿床地球化学异常分带模型与找矿预测标志[J]. 黄金科学技术, 2017, 25(1): 27-34.
[9] 金文洪,王凤仙. 加拿大大不列颠哥伦比亚省杰艾尔金多金属矿床成因类型及控矿因素分析[J]. J4, 2012, 20(3): 1-9.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!