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黄金科学技术 ›› 2021, Vol. 29 ›› Issue (6): 781-794.doi: 10.11872/j.issn.1005-2518.2021.06.068

• 矿产勘查与资源评价 • 上一篇    下一篇

四川大梁子铅锌矿床1 944 m中段构造岩元素组合异常及隐伏矿体预测

王海丰1(),龚红胜2(),冯志兴1,韩润生2,丁天柱3,赵新跃3,吴鹏2   

  1. 1.西部矿业股份有限公司,青海 西宁 810001
    2.昆明理工大学有色金属矿产地质调查中心西南地质调查所,云南 昆明 650093
    3.四川会东大梁矿业有限公司,四川 凉山 615205
  • 收稿日期:2021-06-03 修回日期:2021-09-27 出版日期:2021-12-31 发布日期:2022-03-07
  • 通讯作者: 龚红胜 E-mail:ydc1234567@sina.com;156016616@qq.com
  • 作者简介:王海丰(1973-),男,黑龙江佳木斯人,高级工程师,从事矿产地质勘查工作。ydc1234567@sina.com
  • 基金资助:
    西部矿业集团合作项目“会东大梁子铅锌矿床深部及外围成矿控制因素及找矿靶区预测研究”、“云岭学者”人才计划(2014)和云南省矿产资源预测评价工程实验室专项经费(2010)联合资助

Element Association Anomalies of Tectonite and Prediction of Concealed Orebodies in the 1 944 m Middle Section of Daliangzi Pb-Zn Deposit,Sichuan

Haifeng WANG1(),Hongsheng GONG2(),Zhixing FENG1,Runsheng HAN2,Tianzhu DING3,Xinyue ZHAO3,Peng WU2   

  1. 1.Western Mining Co. , Ltd. , Xining 810001, Qinghai, China
    2.Southwest Institute of Geological Survey, Geological Survey Center for Non-ferrous Metals Resources, Kunming University of Science and Technology, Kunming 650093, Yunnan, China
    3.Sichuan Huidong Daliang Mining Co. , Ltd. , Liangshan 615205, Sichuan, China
  • Received:2021-06-03 Revised:2021-09-27 Online:2021-12-31 Published:2022-03-07
  • Contact: Hongsheng GONG E-mail:ydc1234567@sina.com;156016616@qq.com

摘要:

四川大梁子铅锌矿床位于扬子地块西南缘,明显受小江深断裂与普渡河深断裂之间的NWW-近EW和NE向构造控制。目前该矿山深部找矿前景不明朗,亟需探寻新的找矿思路和方法来实现新的找矿突破。本研究利用构造带中金属元素组合晕特征,进行隐伏矿体的预测。通过开展矿床构造精细解析,认为NWW-近EW向右行张扭性—扭张性控矿断裂(F15、F1等)与NW向张性—右行张(扭)性断裂及其次级褶皱组合形成的“负花状构造”,直接控制着矿床和矿体(脉)展布,均为同一应力场作用下的北东构造带的产物。在此基础上,基于1 944 m中段1∶1 000构造地球化学填图,绘制了Pb、Zn成矿元素组合(F2)和Pb、Zn单元素异常综合图,发现综合异常均沿NW-SE向展布,与已知矿体产状和主控断裂产状基本一致。结合矿床地质特征和异常特征,圈定了Ⅰ号、Ⅱ号和Ⅲ号重点找矿靶区。该研究成果为大梁子铅锌矿深部找矿工作指明了方向,也为同类型矿床深部找矿预测提供了一定的参考。

关键词: 构造岩元素组合异常, 构造控矿规律, 隐伏矿体预测, 大梁子铅锌矿床, 川西南

Abstract:

The Daliangzi Pb-Zn deposit in Sichuan Province is located in the southwestern margin of the Yangtze block,which is obviously controlled by the NWW-trending—nearly EW-trending and NE-trending structure between the Xiaojiang deep fault and the Puduhe deep fault. At present,the deep prospecting of the mine is not clear,and it is urgent to explore new prospecting ideas and methods to achieve new prospecting breakthroughs. In this study,the characteristics of the metal-element association halos within mineralization-related fault zones are used to predict the concealed ore bodies. Firstly,the fine analysis of deposit structure is carried out,and it is believed that the combination of NWW—nearly EW-trending dextral extensional—torsional ore-controlling faults (F15,F1,etc.),the NW-trending extensional—dextral extensional (torsional) faults and its secondary folds forms a “negative flower-like structure”,which directly controls the distribution of deposits and ore bodies (veins),and is the product of the northeast structural belt under the same stress field. On the above knowledge,based on the 1∶1 000 tectonic geochemical mapping in the middle section of 1 944 m,the comprehensive maps of the Pb-Zn mineralization element association (F2) and Pb-Zn element anomalies are drawn. It is found that the comprehensive anomalies are all distributed along the NW-SE direction and are consistent with the occurrences of the known orebodies and the main ore-controlling faults. Then,combined with the geological characteristics and anomaly characteristics of the deposit,the No.Ⅰ,No.Ⅱ and No.Ⅲ key prospecting targets are delineated. The research results indicate the deep prospecting direction of the Daliangzi mining area,and also provide a certain reference for the deep prospecting prediction of similar deposits.

Key words: element association anomalies of tectonite, structure ore-controlling law, concealed orebody prediction, Daliangzi lead-zinc deposit, southwestern Sichuan

中图分类号: 

  • P618.4

图1

川滇黔铅锌成矿区主要断裂及矿床分布图(据柳贺昌等,1999修改)1.超大型、大型铅锌矿床;2.中、小型铅锌矿床;3.城镇;4.省界;5.金沙江及流向;6.构造带及编号;7.断裂;8.峨眉山玄武岩;9.本次工作区范围;a-安宁河断裂带;b-小江断裂带;c-康定—彝良—水城断裂带;d-弥勒—师宗断裂带;e-昭通—曲靖断裂带;f-寻甸—宣威构造带;g-矿山厂—金牛厂构造带;h-会泽—彝良构造带;i-巧家—大关构造带;j-巧家—金沙厂构造带;k-普渡河断裂带"

图2

大梁子铅锌矿区域构造纲要图N-Q-第三系—第四系;T-K-三叠系—白垩系;Z-P-震旦系—二叠系;Pt-前震旦系;P2 β-峨眉山玄武岩;1.地质界线;2.向斜;3.背斜;4.实测推测正断层;5.实测推测逆断层"

图3

大梁子铅锌矿地质简图(据张长青等,2014修改)1.下寒武统龙王庙组;2.下寒武统沧浪铺组上段;3.下寒武统沧浪铺组下段;4.下寒武统筇竹寺组上段;5.下寒武统筇竹寺组下段;6.上震旦统灯影组八段;7.上震旦统灯影组七段第2层;8.上震旦统灯影组七段第1层;9.上震旦统灯影组六段第2层;10.上震旦统灯影组六段第1层;11.上震旦统灯影组五段;12.上震旦统灯影组四段第4层;13.上震旦统灯影组四段第3层;14.上震旦统灯影组四段第2层;15.上震旦统灯影组四段第1层;16.上震旦统灯影组三段;17.上震旦统灯影组二段;18.矿体;19.“黑破带”;20.实测断层;21.推测断层;22.构造破碎带"

图4

F15断裂带剖面素描及力学分析图(据吴建标等,2021修改)σ1-最大主压应力;σ2-中间主压应力;σ3-最小主压应力;f4-断裂及编号;j-节理;Py-黄铁矿;Ⅰ-早期;Ⅱ-晚期;1.断裂运动方向;2.溶蚀孔洞;3.含褐铁矿Pb-Zn矿化体;4.片理化;5.张性断层;6.压性断层"

图5

NW向F6(S)断裂剖面素描及力学分析图σ1-最大主压应力;σ2-中间主压应力;σ3-最小主压应力;f-断裂;Ⅰ-早期;Ⅱ-晚期;1.断裂运动方向;2.方解石脉;3.Pb-Zn矿脉;4.黑色刺穿角砾岩;5.张性断层;6.压性断层"

图6

NE向断裂剖面素描及力学分析图σ1-最大主压应力;σ2-中间主压应力;σ3-最小主压应力;f11-断裂及编号;j-节理;①黑色夹白色白云岩;②片理化白云岩;③灰白色碎裂硅化白云岩;1.断裂运动方向;2.张性断层;3.压性断层"

图7

SN向断裂剖面素描及力学分析图σ1-最大主压应力;σ2-中间主压应力;σ3-最小主压应力;f1-1-断裂及编号;j-节理;P-劈理;①黑色夹碎裂白云岩;②透镜体状黑色白云质碎裂岩;1.断裂运动方向;2.透镜体;3.裂隙;4.张性断层;5.压性断层"

图8

大梁子铅锌矿区本部矿段和南、北矿段控矿构造格局示意图(a)和复式“负花状+刺穿”构造组合样式图(b)1.矿区力偶作用的方向;2.推测倾伏背斜轴;3.背斜轴;4.地层分界线;5.勘探线及编号;6.“黑破带”;7.断裂及运动方向;8.推测断裂及运动方向;9.右行扭张性断裂;10.右行张扭性断裂;11.左行压扭性断裂;12.推测矿体;13.矿体;14.矿化带及倾向;15.最小主压应力方向;16.深部热液运移方向;17.刺穿体;18.河水"

表1

大梁子铅锌矿1 944 m中段构造岩各因子元素组合"

因子元素组合
F1Sc、Rb、Zr、Nb、Cs、Ti、Cr、V、Li、Be、Hf、Ta、Bi、Th、U、LREE
F2Cu、Zn、Ge、Ag、Cd、In、Pb、Sb、Hg、Ga、(As、Sn、Mo)
F3Ni、As、TL、Mo、(Sb)
F4P、(Ba、U、LREE、HREE)
F5Mn、(Sr、Co、Ni)

图9

大梁子铅锌矿1 944 m中段F2、F3、F5元素组合异常图1.燧石条带白云岩及硅质白云岩;2.硅质白云岩及硅质条带白云岩;3.硅质白云岩及硅质白云岩夹硅质岩;4.硅质白云岩及砂质白云岩;5.燧石结核砂泥白云岩及板状泥砂白云岩;6.剖面线;7.正断层及产状;8.断裂早期运动方向;9.断裂晚期运动方向;10.地层界线;11.褶皱;12.矿体水平投影;13.F2元素组合异常等值线;14. F3元素组合异常等值线;15. F5元素组合异常等值线;16.F2元素组合异常中心编号;17. F3元素组合异常中心编号;18. F5元素组合异常中心编号"

图10

大梁子铅锌矿1 944 m中段找矿靶区预测图1.燧石条带白云岩及硅质白云岩;2.硅质白云岩及硅质条带白云岩;3.硅质白云岩及硅质白云岩夹硅质岩;4.硅质白云岩及砂质白云岩;5.燧石结核砂泥白云岩及板状泥砂白云岩;6.剖面线;7.正断层及产状;8.断裂早期运动方向;9.断裂晚期运动方向;10.地层界线;11.褶皱;12.矿体水平投影;13.F2元素组合异常等值线;14. Pb元素异常等值线;15.Zn元素异常等值线;16.F2元素组合异常中心编号;17. Pb元素异常中心编号;18. Zn元素异常中心编号;19.靶区及编号"

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