Citation: | HAO Shi-long, LI Cheng-lu, HU Zhong-xian. GEOCHEMICAL ANOMALY AND PROSPECTING POTENTIAL IN BOGENLI AREA, HEILONGJIANG PROVINCE[J]. Geology and Resources, 2020, 29(5): 419-428, 410. DOI: 10.13686/j.cnki.dzyzy.2020.05.003 |
On the basis of 1:50000 mineral prospective survey in Dubaoshan area and gold deposit general prospecting results in Bogenli area of Nenjiang City, Heilongjiang Province, the paper comprehensively analyzes the regional metallogenic regularity, characteristics of geophysical-geochemical anomalies and prospecting potential. The 1:50000 geochemical anomaly characteristics show that Au anomaly is dominant, with high anomaly strength, most reaching the inner zone and closely related to Ag anomaly. Six comprehensive anomalies are delineated combined with the 1:50000 geophysical prospecting characteristics and remote sensing information. For the 08XHt-3 anomaly, the Au-20 anomaly area is 3.79 km2 with the maximum value of 43.1×10-9, averagely 7.53×10-9, reaching the inner zone. In the 08DHt-11, the Au-47 anomaly area is 2.157 km2 with the maximum value of 29.9×10-9, averagely 8.58×10-9, reaching the inner zone. The later geophysical-geochemical prospecting in 1:10000 scale shows good reproducibility of Au anomaly, which is consistent with geophysical anomaly. The maximum Au anomaly value of delineated BG12HtAu-22 is 115.9×10-9, averagely 23.55×10-9, reaching the inner zone. The maximum Au anomaly values of BG12HtAu-42 and BG12HtAu-43 are 43.6×10-9 and 25.7×10-9 respectively, both reaching the middle zone. Through comprehensive analysis of the regional metallogenic regularity and mineralization conditions in the study area, combined with the characteristics of geophysical-geochemical anomalies and 1 gold orebody and 5 mineralized bodies discovered by a few engineering verification, it is considered that the study area has great prospecting potential and is worthy of further investigation.
[1] |
韩振哲, 刘娜, 公凡影, 等.黑龙江多宝山-大新屯地区铜金多金属成矿作用及找矿方向[J].地质论评, 2015, 61(4):787-796. http://www.cnki.com.cn/Article/CJFDTotal-DZLP201504009.htm
|
[2] |
李成禄, 曲晖, 赵忠海, 等.黑龙江省霍龙门地区成矿地质特征及潜力分析[J].地质与资源, 2013, 22(4):273-278, 329. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract8961.shtml
|
[3] |
李成禄, 徐文喜, 于援帮, 等.小兴安岭西北部与永新金矿有关岩浆岩的年代学和地球化学及成矿构造环境[J].现代地质, 2017, 31(6):1114-1130. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz201706002
|
[4] |
李成禄, 李胜荣, 徐文喜, 等.黑龙江省嫩江县永新碲金矿床黄铁矿标型特征及稳定同位素研究[J].矿物岩石地球化学通报, 2018, 37(1):75-86. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwysdqhxtb201801010
|
[5] |
李成禄, 于援帮, 袁茂文, 等.大兴安岭东北部永新金矿床金银系列矿物和碲化物的发现及其意义[J].地学前缘, 2019, doi: 10.13745/j.esf.sf.2019.8.20.
|
[6] |
Yuan M W, Li S R, Li C L, et al. Geochemical and isotopic composition of auriferous pyrite from the Yongxin gold deposit, Central Asian Orogenic Belt:Implication for ore genesis[J]. Ore Geology Reviews, 2018, 93:255-267. doi: 10.1016/j.oregeorev.2018.01.002
|
[7] |
刘宝山.黑龙江黑河孟德河金矿床控矿因素及找矿标志[J].黄金, 2015, 36(1):18-21. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=huangj201501006
|
[8] |
刘宝山, 杨晓平, 李成禄.黑龙江省嫩江三合屯韧性剪切带与金矿化[J].矿产与地质, 2017, 31(3):503-506, 513. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcydz201703011
|
[9] |
李成禄, 曲晖, 赵忠海, 等.黑龙江霍龙门地区早石炭世花岗岩的锆石U-Pb年龄、地球化学特征及构造意义[J].中国地质, 2013, 40(3):859-868. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201303017
|
[10] |
李成禄, 徐文喜, 李胜荣, 等.大兴安岭东北部霍龙门地区早二叠世花岗岩的锆石U-Pb年龄、地球化学特征及构造意义[J].矿物岩石, 2017, 37(3):46-54. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys201703007
|
[11] |
曲晖, 李成禄, 杨福深.小兴安岭西北部霍龙门地区花岗质杂岩锆石U-Pb年龄、岩石地球化学特征及地质意义[J].世界地质, 2015, 34(1):34-43. http://qikan.cqvip.com/Qikan/Article/Detail?id=664402363
|
[12] |
徐文喜, 李成禄.大兴安岭东北部霍龙门地区中侏罗世花岗岩——锆石U-Pb年龄、地球化学特征及构造意义[J].地质与资源, 2018, 27(6):522-530. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract8502.shtml
|
[13] |
张兴洲, 乔德武, 迟效国, 等.东北地区晚古生代构造演化及其石油地质意义[J].地质通报, 2011, 30(2/3):205-213. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201102004
|
[14] |
汪岩, 杨晓平, 那福超, 等.嫩江-黑河构造带中花岗质糜棱岩的确定及地质意义[J].地质与资源, 2013, 22(6):452-459. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract8994.shtml
|
[15] |
李成禄, 徐文喜, 于援帮, 等.黑龙江省嫩江-黑河构造混杂岩带金矿成矿作用及找矿预测[M].北京:地质出版社, 2019:140-145.
|
[16] |
Yuan M W, Li L, Li S R, et al. Mineralogy, fluid inclusions and S-Pb-H-O isotopes of the Erdaokan Ag-Pb-Zn deposit, Duobaoshan metallogenic belt, NE China:Implications for ore genesis[J]. Ore Geology Reviews, 2019, 113:103074. doi: 10.1016/j.oregeorev.2019.103074
|
[17] |
徐文喜, 李成禄, 鲍希波, 等.大兴安岭东北部首个三叠纪银矿床地质特征及矿床成因分析[J].矿产与地质, 2019, 33(3):434-441. http://www.cqvip.com/QK/96866X/201903/7100105401.html
|
[18] |
庞绪勇, 秦克章, 王乐, 等.黑龙江铜山断裂的变形特征及铜山铜矿床蚀变带-矿体重建[J].岩石学报, 2017, 33(2):398-414. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201702007
|
[19] |
付艳丽, 黄喜峰.野猪沟钼矿找矿前景及工作建议[J].中国科技信息, 2005(10):128. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkjxx200510117
|
[20] |
邓轲, 陈衍景, 张成, 等.黑龙江省三矿沟夕卡岩型铁铜矿床矿物学特征及成矿物理化学条件[J].地学前缘, 2018, 25(5):167-182. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201805011
|
[21] |
Song G X, Cook N J, Wang L, et al. Gold behavior in intermediate sulfidation epithermal systems:A case study from the Zhengguang gold deposit, Heilongjiang Province, NE-China[J]. Ore Geology Reviews, 2019, 106:446-462. doi: 10.1016/j.oregeorev.2019.02.001
|
[22] |
王宝权.黑龙江省争光岩金矿床地质特征及找矿标志[J].地质与资源, 2016, 25(3):244-249, 253. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract8637.shtml
|
[23] |
Gao S, Xu H, Zang Y Q, et al. Late Mesozoic magmatism and metallogeny in NE China:The Sandaowanzi-Beidagou example[J]. International Geology Review, 2017, 59(11):1413-1438. doi: 10.1080/00206814.2016.1266701
|
[24] |
赵书跃, 庞雪娇, 李德胜.黑龙江三道湾子金矿含金石英脉与围岩地球化学及地质意义[J].地质与资源, 2016, 25(2):130-136, 175. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract8616.shtml
|
[25] |
闫文强, 高树学, 杨凤喜, 等.五道沟金矿床控矿因素及找矿方向[J].黄金科学技术, 2008, 16(3):43-44, 48. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hjkxjs200803011
|
[26] |
曲晖, 赵忠海, 李成禄, 等.黑龙江永新金矿地质特征及成因[J].地质与资源, 2014, 23(6):520-524. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract8895.shtml
|
[27] |
Li C L, Li L, Yuan M W, et al. Study on pyrite thermoelectricity, ore-forming fluids and H-O-Rb-Sr isotopes of the Yongxin gold deposit, Central Asian Orogenic Belt:Implications for ore genesis and exploration[J]. Ore Geology Reviews, 2020, 121:103568. doi: 10.1016/j.oregeorev.2020.103568
|
[28] |
梁科伟, 赵忠海, 郭艳.原生晕在深部成矿预测中的应用——以黑河地区永新金矿为例[J].地质与资源, 2019, 28(6):512-518. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract9526.shtml
|
1. |
顾光明,李杭,严城民,马重辉,雷星,胡凯兵. 花岗岩成矿元素迁移富集的分析方法——以滇西南大同山稀土矿区矿化与风化过程为例. 地质与资源. 2024(03): 323-330 .
![]() | |
2. |
高科宁,邓居智,刘文玉,余辉,陈辉,周聪,王彦国,刘宝山. 黑龙江省三合屯金矿床深部电性结构与成矿模式. 吉林大学学报(地球科学版). 2022(03): 684-700 .
![]() | |
3. |
李博文,谷华娟,李成禄,刘宝山,杨晓平. 黑龙江省三合屯金矿床地质特征及找矿潜力分析. 黄金科学技术. 2022(04): 508-517 .
![]() | |
4. |
于喜洹,石国明,符安宗,李新鹏,孙江军,尹国良,林泽付. 黑龙江省多宝山地区中奥陶世侵入岩锆石U-Pb年龄及构造环境. 地质与资源. 2022(05): 588-596 .
![]() | |
5. |
卢昱润,李蕴峰,陈卓,裴赢政,徐立明,魏小勇. 内蒙古牙克石地区钼多金属矿床地质特征及找矿方向. 地质与资源. 2022(06): 754-761 .
![]() |