吉林大学学报(地球科学版) ›› 2025, Vol. 55 ›› Issue (1): 125-138.doi: 10.13278/j.cnki.jjuese.20230239

• 地质与资源 • 上一篇    下一篇

长江中下游成矿带大金山地区综合信息找矿效果及深部找矿潜力分析

王学阳1,2,杨言辰1,刘志宏3,张继武2,戴台鹏2   

  1. 1.吉林大学地球科学学院,长春 130026
    2.长春黄金研究院有限公司,长春 130012
    3.江苏省地质调查研究院,南京 210018
  • 收稿日期:2023-09-15 出版日期:2025-01-26 发布日期:2025-02-07
  • 通讯作者: 刘志宏(1984—),男,高级工程师,硕士,主要从事矿产勘查方面的研究,E-mail:287738032@qq.com
  • 作者简介:王学阳(1990—),男,工程师,博士研究生,主要从事矿床地质、矿产勘查方面的研究,E-mail:553970726@qq.com
  • 基金资助:
    中国地质调查局发展研究中心项目(中地调研合同〔2020〕第296号);江苏省地质局地质勘查基金项目(苏地质发〔2022〕82号);江苏省地质勘查基金项目(苏财建〔2016〕140号);江苏省国土资源厅找矿项目(苏国土资函〔2010〕8号)

Effect and Deep Potential of Comprehensive Information Prospecting in the Middle-Lower Yangtze Metallogenic Belt, Dajinshan Area

Wang Xueyang1,2, Yang Yanchen1, Liu Zhihong3, Zhang Jiwu2, Dai Taipeng2   

  1. 1. College of Earth Sciences,Jilin University, Changchun 130026, China
    2. Changchun Gold Research Institute Co., Ltd., Changchun 130012, China
    3. Geological Survey of Jiangsu Province, Nanjing 210018, China
  • Received:2023-09-15 Online:2025-01-26 Published:2025-02-07
  • Supported by:
    the Development Research Center Project of China Geological Survey (Zhongdi Research Contract \[2020\] No. 296),the Geological Exploration Fund Project of Jiangsu Provincial Geological Bureau (Su Geological Development \[2022\] No. 82),the Jiangsu Provincial Geological Exploration Fund Project (Su Cai Jian \[2016\] No. 140) and the Exploration Project of Jiangsu Provincial Department of Land and Resources (Su Guo Tu Zi Han \[2010\] No. 8)

摘要: 大金山地区大地构造位置处于扬子板块北缘,长江中下游成矿带宁芜矿集区,该地区成矿地质条件优越,具有进一步找矿的潜力。为揭示大金山地区找矿潜力,本文结合区域成矿地质背景、大金山地区地质特征,对激电中梯、土壤地球化学测量成果开展相关性分析。研究表明:北西向断裂破碎带显示高阻高充电异常,而北西向断裂带控制了矿体的产出,因此高阻高充电异常可间接指导找矿;土壤地球化学测量圈定的10处综合异常具有一定找矿潜力。在高阻高充电异常及强烈Au异常的视电阻率异常R4和R5、视充电率异常M2、综合异常HT-10的套合区域布设了2个钻孔,探获了3条铜矿体、3条硫铁矿体,取得了找矿突破。通过与区域内成矿特征相似的典型矿床(大岭岗金铜矿床、南门头铜矿床)进行对比,结合钻孔岩心原生晕分析,认为大金山地区深部具有良好的找矿潜力。根据斑岩型铜金矿床的赋矿岩石、构造环境和深部探获的斑状二长花岗岩,认为大金山地区深部有盲矿体存在,且具有探获斑岩型铜金矿床的潜力。

关键词: 综合信息, 典型矿床, 原生晕, 深部找矿潜力, 大金山地区, 宁芜矿集区, 长江中下游成矿带, 斑岩型铜金矿床

Abstract: The Dajinshan area is located in the Ning-Wu ore concentration zone along the Middle-Lower Yangtze metallogenic belt at the northern margin of  Yangtze plate. The area has favorable geological conditions for mineralization and shows potential for further prospecting. To identify the prospecting potentials in Dajinshan area, this study performed a correlation analysis between induced polarization(IP) medium gradient survey and soil geochemical survey results. The results show that a NW-trending fractured and broken zone exhibits high resistance and chargeability anomalies, which are indicative of controlling mineralization. These anomalies can thus serve as indirect guides for prospecting. Ten comprehensive anomalies were identified through soil geochemical surveys that indicate significant prospecting potential. Two drill holes were drilled in areas where high resistance, chargeability, and strong Au anomalies overlapped, leading to the discovery of three copper orebodies and three pyrite orebodies, achieving a major prospecting advancement. By comparing these findings with similar metallogenic characteristics (Dalinggang gold-copper deposit, Nanmentou copper deposit), and analyzing the primary halo in drill core samples, it is believed that the deeper parts of the Dajinshan area likely have promising prospecting potentials. Based on the ore-bearing rocks, tectonic environment, and the discovery of porphyritic monzonite granites in the deeper parts of porphyry-type copper-gold deposits, it is believed that blind orebodies may exist at depth, suggesting the potential for porphyry-type copper-gold deposits.

Key words: comprehensive information, typical deposits, primary halo, prospecting potential in the deep part, Dajinshan area, Ning-Wu ore concentration area;Middle-Lower Yangtze metallogenic belt, porphyry-type copper-gold deposit

中图分类号: 

  • P618.4
[1] 林成贵, 程志中, 吕志成, 颜廷杰, 贾儒雅, 姚晓峰, 宓奎峰, 李康宁. 甘肃省早子沟金矿原生晕分带特征及深部找矿预测[J]. 吉林大学学报(地球科学版), 2020, 50(1): 70-84.
[2] 明添学, 唐忠, 李永平, 罗建宏, 李蓉, 薛戈, 陈雷. 云南巧家东坪铅锌矿床原生晕特征与找矿潜力[J]. 吉林大学学报(地球科学版), 2018, 48(5): 1394-1404.
[3] 程文斌, 尹力, 陈翠华, 宋玉坤, 李关清, 张兴国, 夏抱本, 达瓦次仁. 西藏柯月Pb-Zn-Sb-Ag多金属矿床I号矿体原生晕地球化学特征[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1711-1723.
[4] 孙莉, 肖克炎,高阳. 彩霞山铅锌矿原生晕地球化学特征及深部矿产评价[J]. 吉林大学学报(地球科学版), 2013, 43(4): 1179-1189.
[5] 彭翼,何玉良,曾涛,钟江文,许国丽,苏小岩,谌军,彭松民,李震. 河南省Mo矿区域成矿模式与综合信息预测模型[J]. 吉林大学学报(地球科学版), 2013, 43(4): 1262-1275.
[6] 肖克炎, 娄德波,黄文斌,孙莉,叶天竺. 区域矿产预测图及综合解释模型[J]. 吉林大学学报(地球科学版), 2012, 42(6): 1966-1975.
[7] 王微, 王世称, 刘光胜, 马生忠. 运用综合信息开展地震区划[J]. J4, 2011, 41(3): 892-899.
[8] 叶水盛, 袁鑫. 地学综合信息图库管理系统的进一步开发应用[J]. J4, 2010, 40(3): 726-732.
[9] 叶水盛, 陈慧娟. 综合信息矿产资源评价中图库管理系统的开发应用研究[J]. J4, 2009, 39(3): 547-553.
[10] 薛顺荣,肖克炎,丁建华. 基于MRAS的证据权重法在香格里拉地区的综合信息成矿预测[J]. J4, 2008, 38(5): 738-0744.
[11] 刘志远,徐学纯. 辽东青城子金银多金属成矿区综合信息找矿模型及找矿远景分析[J]. J4, 2007, 37(3): 437-0443.
[12] 曾道明,纪宏金,陈 满,胡大千,朱永正. 胶东山城金矿地质与地球化学变量的关系[J]. J4, 2006, 36(04): 511-515.
[13] 廖桂香,许亚明,付宝霞. 青海省金矿综合信息预测[J]. J4, 2006, 36(01): 44-0048.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 程立人,张予杰,张以春. 西藏申扎地区奥陶纪鹦鹉螺化石[J]. J4, 2005, 35(03): 273 -0282 .
[2] 李 秉 成. 陕西富平全新世古气候的初步研究[J]. J4, 2005, 35(03): 291 -0295 .
[3] 和钟铧,杨德明,王天武,郑常青. 冈底斯带巴嘎区二云母花岗岩SHRIMP锆石U-Pb定年[J]. J4, 2005, 35(03): 302 -0307 .
[4] 陈 力,佴 磊,王秀范,李 金. 绥中某电力设备站场区地震危险性分析[J]. J4, 2005, 35(05): 641 -645 .
[5] 纪宏金,孙丰月,陈满,胡大千,时艳香,潘向清. 胶东地区裸露含金构造的地球化学评价[J]. J4, 2005, 35(03): 308 -0312 .
[6] 初凤友,孙国胜,李晓敏,马维林,赵宏樵. 中太平洋海山富钴结壳生长习性及控制因素[J]. J4, 2005, 35(03): 320 -0325 .
[7] 李斌,孟自芳,李相博,卢红选,郑民. 泌阳凹陷下第三系构造特征与沉积体系[J]. J4, 2005, 35(03): 332 -0339 .
[8] 李涛, 吴胜军,蔡述明,薛怀平,YASUNORI Nakayama. 涨渡湖通江前后调蓄能力模拟分析[J]. J4, 2005, 35(03): 351 -0355 .
[9] 旷理雄,郭建华,梅廉夫,童小兰,杨丽. 从油气勘探的角度论博格达山的隆升[J]. J4, 2005, 35(03): 346 -0350 .
[10] 章光新,邓伟,何岩,RAMSIS Salama. 水文响应单元法在盐渍化风险评价中的应用[J]. J4, 2005, 35(03): 356 -0360 .