The three-dimensional geological model and the coupling relationship between deep ore body and fault of Sanshandao super giant gold deposit in Jiaodong
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摘要:
近年在胶东三山岛地区的深部和北部海域找矿取得重大进展,已成为中国深部找矿的典型案例。对三山岛金矿床进行三维可视化分析,对指导深部找矿具有重要的实际意义。基于311个钻孔资料建立了三山岛超巨型金矿床的三维地质模型,剖析了金矿床的三维空间特征,指出了沿控矿断裂深部找矿的重点区段。三维可视化分析发现,研究区以往认为各自独立的数个金矿床,主要矿体向深部相互连接,构成资源量超过1000 t的超巨型金矿床;赋矿的三山岛断裂产状起伏变化明显,浅部倾角较陡,向深部逐渐变缓,呈铲式阶梯状。对主要矿体厚度、品位变化与断裂面倾角变化的耦合关系分析表明,矿体品位和厚度沿走向和倾向均呈现高低相间变化的特点,两者呈正相关。金矿体主要赋存于断裂表面坡度较缓段,在三山岛北部海域,三山岛断裂在2000 m深度范围内有2个倾角明显缓倾的台阶,分别赋存了浅部和深部金矿体。其中,浅部台阶位于-20~-600 m标高,断裂表面坡度平均值为48.21°,矿体赋存部位的断裂表面坡度平均值为44.72°;深部台阶位于-940~-1760 m标高,断裂表面坡度平均值为44.56°,矿体赋存部位的断裂表面坡度平均值为42.75°。综合分析认为,断裂的缓倾角段是深部找矿的重点区域。
Abstract:In recent years, great progress has been made in the deep prospecting in the Sanshandao area and the northern sea area, Jiaodong, and it has become a typical case of deep prospecting in China.The three-dimensional visualization analysis of it is of great practical significance to the guidance of deep prospecting.In this paper, the three-dimensional geological model of Sanshandao super giant gold deposit is established based on 311 borehole data.The three-dimensional spatial characteristics of the gold deposit are analyzed, and the key ore-prospecting sections along the ore-controlling faults are pointed out.The three-dimensional visualization analysis shows that the main orebodies of several gold deposits, which were previously considered to be independent, are connected to each other to the deep, and constitute a super-giant gold deposit with more than 1000 tons of resources.The Sanshandao fault, which is endowed with ore, has obvious fluctuation of occurrence, with steep dip angle in the shallow part and gradual slow dip angle in the deep part, showing a shovel step shape.The coupling relationship between the thickness and grade of the main orebody and the dip angle of the fracture surface shows that the grade and thickness of ore body change alternately along strike and dip, and they are positively correlated.The gold orebody mainly occurs in the section where the fracture surface with relatively low slope.In the northern sea area, the Sanshandao fault has two significant steps with low-angle dip in 2000 m depth range, which occurrence the shallow and deep gold ore body respectively.In the shallow step of the fracture, which located at -20~-600 m elevation, the average slope of the surface is 48.21°while it is 44.72°at the orebody occurrence section.In the deep step of the fracture, which located at -940~-1760 m elevation, the average slope of the surface is 44.56°while it is 42.75°at the orebody occurrence section.Comprehensive analysis shows that the gentle dip angle section of the fault is the key area for deep ore prospecting.
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Key words:
- Sanshandao gold deposit /
- 3D model /
- surface slope /
- deep prospecting /
- Jiaodong
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图 1 胶东地区区域地质及金矿床分布图[3]
Figure 1.
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[1] 毛景文, 赫英, 丁悌平. 胶东金矿形成期间地幔流体参与成矿过程的碳氧氢同位素证据[J]. 矿床地质, 2002, 21(2): 121-128. doi: 10.3969/j.issn.0258-7106.2002.02.004
[2] 邓军, 王庆飞, 杨立强, 等. 胶西北金矿集区成矿作用发生的地质背景[J]. 地学前缘, 2004, 11(4): 527-533. doi: 10.3321/j.issn:1005-2321.2004.04.019
[3] 宋明春, 宋英昕, 丁正江, 等. 胶东焦家和三山岛巨型金矿床的发现及有关问题讨论[J]. 大地构造与成矿学, 2019, 43(1): 92-110. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201901008.htm
[4] 于学峰, 宋明春, 李大鹏, 等. 山东金矿找矿突破进展与前景[J]. 地质学报, 2016, 90(10): 2847-2862. doi: 10.3969/j.issn.0001-5717.2016.10.021
[5] 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. doi: 10.3969/j.issn.1671-2552.2015.09.017 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20150917&flag=1
[6] 宋明春. 对我国深部金矿资源勘查有关问题的认识与思考[J]. 黄金科学技术, 2017, 25(3): 1-2. https://www.cnki.com.cn/Article/CJFDTOTAL-HJKJ201703001.htm
[7] 宋英昕, 宋明春, 丁正江, 等. 胶东金矿集区深部找矿重要进展及成矿特征[J]. 黄金科学技术, 2017, 25(3): 4-18. https://www.cnki.com.cn/Article/CJFDTOTAL-HJKJ201703003.htm
[8] 毛先成, 张苗苗, 邓浩, 等. 矿区深部隐伏矿体三维可视化预测方法[J]. 地质学刊, 2016, 40(3): 363-371. doi: 10.3969/j.issn.1674-3636.2016.03.363
[9] 刘少华, 肖克炎, 王新海. 地质三维属性建模及其可视化[J]. 地质通报, 2010, 29(10): 1554-1557. doi: 10.3969/j.issn.1671-2552.2010.10.020 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20101019&flag=1
[10] 陈建平, 吕鹏, 吴文, 等. 基于三维可视化技术的隐伏矿体预测[J]. 地学前缘, 2007, (5): 54-62. doi: 10.3321/j.issn:1005-2321.2007.05.006
[11] 张洋洋, 周万蓬, 吴志春, 等. 三维地质建模技术发展现状及建模实例[J]. 东华理工大学学报(社会科学版), 2013, 32(3): 403-409. https://www.cnki.com.cn/Article/CJFDTOTAL-FZSZ201303040.htm
[12] 李青元, 张丽云, 魏占营, 等. 三维地质建模软件发展现状及问题探讨[J]. 地质学刊, 2013, 37(4): 554-561. doi: 10.3969/j.issn.1674-3636.2013.04.554
[13] Huang Leilei, Wang Gongwen, Emmanuel John M, et al. Multi-scale Numerical Simulation and 3D Modeling for Deep Mineral Exploration in the Jiaojia Gold District, China[J]. Natural Resources Research, 2020, 29(1): 415-438. doi: 10.1007/s11053-019-09608-z
[14] 毛先成, 张苗苗, 邓浩, 等. 矿区深部隐伏矿体三维可视化预测方法[J]. 地质学刊, 2016, 40(3): 363-371. doi: 10.3969/j.issn.1674-3636.2016.03.363
[15] 毛先成, 王琪, 陈进, 等. 胶西北金矿集区深部成矿构造三维建模与找矿意义[J]. 地球学报, 2020, 41(2): 166-178. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB202002007.htm
[16] 潘懋, 方裕, 屈红刚. 三维地质建模若干基本问题探讨[J]. 地理与地理信息科学, 2007, 23(3): 1-5. doi: 10.3969/j.issn.1672-0504.2007.03.001
[17] 王功文, 张寿庭, 燕长海, 等. 基于地质与重磁数据集成的栾川钼多金属矿区三维地质建模[J]. 地球科学-中国地质大学学报, 2011, 36(2): 360-366. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201102024.htm
[18] 王功文, 郭运生, 杜杨松, 等. 基于GIS的云南普朗斑岩铜矿床三维成矿预测[J]. 矿床地质, 2007, 26(6): 651-653. doi: 10.3969/j.issn.0258-7106.2007.06.007
[19] 宋明春, 崔书学, 姜洪利, 等. 山东胶西北矿集区和焦家金矿田成矿构造系统[J]. 地质通报, 2011, 30(4): 573-578. doi: 10.3969/j.issn.1671-2552.2011.04.014 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20110413&flag=1
[20] 王金辉, 田京祥. 三山岛断裂在海域北延位置的确定及成矿预测[J]. 地质学报, 2017, 91(12): 2771-2780. doi: 10.3969/j.issn.0001-5717.2017.12.013
[21] 杨奎锋, 朱继托, 程胜红, 等. 胶东三山岛金矿构造控矿规律研究[J]. 大地构造与成矿学, 2017, 41(2): 272-282. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201702004.htm
[22] 刘日富, 周鑫, 吕雨璐, 等. 胶东三山岛-仓上断裂带控矿规律与找矿勘查实践[J]. 地质与勘探, 2019, 55(2): 528-541. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201902008.htm
[23] 赵冬冬, 金刚, 李海松, 等. 山东省莱州市三山岛金矿床地质特征及成因探讨[J]. 地质找矿论丛, 2013, 28(4): 546-551. https://www.cnki.com.cn/Article/CJFDTOTAL-DZZK201304008.htm
[24] 张军进, 丁正江, 刘殿浩, 等. 山东莱州三山岛北部海域超大型金矿勘查实践与找矿成果[J]. 黄金科学技术, 2016, 24(1): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-HJKJ201601001.htm
[25] 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. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201502012.htm
[26] 姜晓辉, 范宏瑞, 胡芳芳, 等. 胶东三山岛金矿中深部成矿流体对比及矿床成因[J]. 岩石学报, 2011, 27(5): 1327-1340. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201105009.htm
[27] 郭春影. 胶东三山岛-仓上金矿带构造-岩浆-流体金成矿系统[D]. 中国地质大学(北京) 博士学位论文, 2009.
[28] 周国发, 吕古贤, 申玉科, 等. 山东三山岛金矿床地质特征及找矿预测[J]. 黄金科学技术, 2011, 19(4): 1-5. doi: 10.3969/j.issn.1005-2518.2011.04.001
[29] 王建, 朱立新, 马生明, 等. 胶东三山岛北海域金矿床热液蚀变作用研究[J]. 地质通报, 2020, 39(11): 1807-1826. doi: 10.12097/j.issn.1671-2552.2020.11.012 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20201112&flag=1
[30] 刘祥朋, 王玺, 宋英昕, 等. 胶西北西岭特大型金矿床蚀变围岩特征研究[J]. 东华理工大学学报(自然科学版), 2017, 40(3): 225-236. doi: 10.3969/j.issn.1674-3504.2017.03.003
[31] Yan J Y, Wang Z H, Wang J H, et al. Using marine magnetic survey data to identify a gold ore-controlling fault: a case study in Sanshandao fault, eastern China[J]. Journal of Geophysics and Engineering, 2018, 15(3): 729-738. doi: 10.1088/1742-2140/aa9c69
[32] 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, 42(7): 992-1000. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201207006.htm
[33] 宋明春, 宋英昕, 李杰, 等. 深部矿阶梯式找矿方法: 以胶东金矿集区深部找矿为例[J/OL]. 中国地质: 1-14[2021-06-03].
[34] 宋明春, 林少一, 杨立强, 等. 胶东金矿成矿模式[J]. 矿床地质, 2020, 39(2): 215-236. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ202002002.htm
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