Prospecting prediction and verification at a depth of 3000 m in the Shuiwangzhuang gold deposit, northwestern Jiaodong Peninsula, eastern China
-
摘要:
水旺庄金矿床位于胶西北招平断裂带北段玲珑金矿田东南缘,累计探明金资源量逾180 t,已控制矿体最大垂深2200 m。目前,胶西北主要金矿田深部找矿的深度均已达2000 m,正确认识3000 m深度的找矿前景,既是该区域进一步开展深部找矿的现实需要,也对全国深部找矿具有重要的示范意义。通过对矿床地质特征、矿化富集规律、深部地球物理探测等研究,预测了水旺庄金矿床的深部找矿前景,并进行了深部钻探验证。同时,对区内深部金资源潜力进行了讨论。研究表明,水旺庄金矿床主要矿体严格受控于NNE—NE走向招平断裂带,具有NE向侧伏和SE向倾伏的特征,沿侧伏和倾伏方向金矿化具有分段富集的规律,预测在5号勘探线以东、-2200 m标高以深会出现新的矿化富集区。大地电磁测深剖面显示,招平断裂带向深部延伸稳定,沿倾向具有波状起伏的特征,于-2500~-3000 m标高范围倾角明显变缓,由27°变为18°,指示该区域具有良好的深部找矿前景。根据预测结果,实施了3000.58 m钻孔进行验证,于2831.15~2832.65 m深度探获厚1.50 m、品位达6.85 g/t的金矿体。进一步分析认为,招平断裂带北段深部找矿潜力巨大,初步预测在-2000~-3000 m深度存在第三矿化富集带,预测金资源量可能超400 t。
Abstract:The Shuiwangzhuang gold deposit is located at the southeast segment of the Linglong goldfield, northwestern Jiaodong Peninsula, with a pre-mining endowment more than 180 t of gold.The maximum controlled depth of the orebodies is 2200 m.At present, the prospect depth of main gold fields in the northwestern Jiaodong Peninsula has reached 2000 m, a correct understanding of the prospecting potential at a depth of 3000 m is not only a practical need for further deep prospecting in this region, but also has important demonstration significance for deep prospecting throughout the country.Basing on the research of geological characteristics, mineralization enrichment regularities and deep geophysical probing, deep prospecting potential of the Shuiwangzhuang gold deposit was implemented, and the deep drill hole was constructed to verify its effect.At the same time, the deep gold resources potential is discussed.The main orebodies are controlled by the NEE- to NE-trending Zhaoping fault system, with NE direction of lateral trending and SE direction of plunging.The orebodies segment into a number of enrichment zones along the lateral trending and plunging direction.The orebodies may extend to the east of No.5 exploration line, and below the depth of -2200 m.The MT profile shows that the Zhaoping fault system extend stably to the deep, and the dip angle changes from 27° to 18° at a depth of -2500~-3000 m, indicating good prospecting potential.According to the prospecting results, a 3000.58 m drill hole was constructed, and one gold orebody with thickness of 1.5 m and gold grade of 6.85 g/t was found from 2831.15 m to 2832.65 m.Further analysis shows huge potential of the deep in the northern Zhaoping fault system.It is predicted that there exists a third mineralization enrichment zone at the depth of -2000 ~ -3000 m, and the gold resources may exceed 400 t.
-
-
表 1 水旺庄金矿床典型勘探线矿体特征
Table 1. Main orebody characteristics of typical exploration lines in the Shuiwangzhuang gold deposit
勘探线号 矿体长度/m 厚度/m 品位/(g·t-1) 厚度×品位/(m·g·t-1) 矿化富集程度 42线 2006 8.88 3.67 32.61 强 34线 1732 5.99 3.46 20.79 弱 26线 1950 10.50 3.33 35.03 强 10线 1410 13.10 4.78 62.75 强 5线 1227 2.06 2.37 4.89 弱 表 2 水旺庄金矿床流体包裹体捕获压力与成矿深度估算
Table 2. Metallogenic depth calculated from the capture pressure of the fluid inclusions in the Shuiwangzhuang gold deposit
捕获压力/MPa 静水压力估算深度/km 静岩压力估算深度/km 回归方程估算深度/km 最小值 60 6 2.2 6 最大值 180 18 6.7 11 平均值 120 12 4.4 8.5 -
[1] 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
[2] 宋明春, 宋英昕, 丁正江, 等. 胶东金矿床: 基本特征和主要争议[J]. 黄金科学技术, 2018, 26(4), 406-422. https://www.cnki.com.cn/Article/CJFDTOTAL-HJKJ201804006.htm
[3] 宋明春, 徐军祥, 焦秀美, 等. 山东省地质矿产勘查开发局60年重要找矿成果和深部隐伏区找矿技术进展[J]. 山东国土资源, 2018, 34(10) : 1-14. https://www.cnki.com.cn/Article/CJFDTOTAL-SDDI201810001.htm
[4] 于学峰, 李大鹏, 田京祥, 等. 山东金矿深部勘查进展与成矿理论创新[J]. 山东国土资源, 2018.34(5) : 1-13. doi: 10.3969/j.issn.1672-6979.2018.05.001
[5] 鲍中义, 孙忠全, 刘国栋, 等. 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. doi: 10.3969/j.issn.1672-6979.2014.02.008
[6] 刘国栋, 温桂军, 刘彩杰, 等. 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[J]. 黄金科学技术, 2017, 25(3) : 38-45. https://www.cnki.com.cn/Article/CJFDTOTAL-HJKJ201703006.htm
[7] 刘国栋, 李娟. 胶东招平断裂-2200m特大型金矿体地质特征与找矿标志[J]. 山东国土资源, 2019, 35(1) : 4-10. https://www.cnki.com.cn/Article/CJFDTOTAL-SDDI201901001.htm
[8] 刘国栋, 宋国政, 鲍中义, 等. 胶东招平断裂北段深部找矿新突破及对断裂空间展布的新认识[J]. 大地构造与成矿学, 2019, 43(2) : 226-234. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201902003.htm
[9] 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
[10] 宋国政, 李山, 闫春明, 等. 焦家金矿田Ⅰ号主矿体地质特征及找矿方向[J]. 地质与勘探, 2018, 54(2) : 219-229. doi: 10.3969/j.issn.0495-5331.2018.02.001
[11] Yang L Q, Guo L N, Wang Z L, et al. Timing and mechanism of gold mineralization at the Wang'ershan gold deposit, Jiaodong Peninsula, eastern China[J]. Ore Geology Reviews, 2017, 88: 491-510. doi: 10.1016/j.oregeorev.2016.06.027
[12] 刘向东, 邓军, 张良, 等. 胶西北寺庄金矿床热液蚀变作用[J]. 岩石学报, 2019, 35(5) : 1551-1565.
[13] 丁正江, 孙丰月, 刘福来, 等. 胶东中生代动力学演化及主要金属矿床成矿系列[J]. 岩石学报, 2015, 31(10) : 3045-3080. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201510011.htm
[14] 曲晓明, 王鹤年, 饶冰. 胶东群部分熔化实验及其对花岗岩成因的指示[J]. 地球化学, 2000, 29(2) : 153-161. doi: 10.3321/j.issn:0379-1726.2000.02.007
[15] 刘平华, 刘福来, 王舫, 等. 山东半岛荆山群富铝片麻岩锆石U-Pb定年及其地质意义[J]. 岩石矿物学杂志, 2011, 30(5) : 829-843. doi: 10.3969/j.issn.1000-6524.2011.05.007
[16] 谢士稳, 王世进, 颉颃强, 等. 华北克拉通胶东地区粉子山群碎屑锆石SHRIMP U-Pb定年[J]. 岩石学报, 2014, 30(10) : 2989-2998. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201410014.htm
[17] 朱光, 徐嘉炜, Flether C J N, 等. 应用X射线衍射分析胶北蓬莱群板岩中的变质作用[J]. 地质与勘探, 1994, 30(2) : 42-49. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT402.010.htm
[18] 初航, 陆松年, 王慧初, 等. 山东长岛地区蓬莱群辅子夼组碎屑锆石年龄谱研究[J]. 岩石学报, 2011, 27(4) : 1017-1028. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201104013.htm
[19] Ma L, Jiang S Y, Dai B Z, et al. Multiple sources for the origin of Late Jurassic Linglong adakitic granite in the Shandong Peninsula, eastern China: Zircon U-Pb geochronological, geochemical and Sr-Nd-Hf isotopic evidence[J]. Lithos, 2013, 162/163: 251-263. doi: 10.1016/j.lithos.2013.01.009
[20] Yang L Q, Dilek Y, Wang Z L, et al. Late Jurassic, high Ba-Sr Linglong granites in the Jiaodong Peninsula, East China: Lower crustal melting products in the eastern North China Craton[J]. Geological Magazine, 2018, 155(5) : 1040-1062. doi: 10.1017/S0016756816001230
[21] 耿科, 王瑞江, 李洪奎, 等. 胶西北丛家花岗闪长岩体SHRIMP锆石U-Pb年代学研究[J]. 地球学报, 2016, 37(1) : 90-100. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201601011.htm
[22] Goss C S, Wilde A S, Wu F Y, et al. The age, isotopic signature and significance of the youngest Mesozoic granitoids in the Jiaodong Terrane, Shandong Province, North China Craton[J]. Lithos, 2010, 120(3/4) : 309-326.
[23] 杨宽, 王建平, 林进展, 等. 胶东半岛艾山岩体岩石地球化学特征及成因意义[J]. 地质与勘探, 2012, 48(4) : 693-703. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201204005.htm
[24] 刘利双, 刘福来, 冀磊, 等. 北苏鲁超高压变质带内多成因类型的变花岗质岩石及其地质意义[J]. 岩石学报, 2018, 34(6) : 1557-1580. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201806002.htm
[25] Deng J, Wang Q F. Gold mineralization in China: Metallogenic provinces, deposit types and tectonic framework[J]. Gondwana Research, 2016, 36: 219-274. doi: 10.1016/j.gr.2015.10.003
[26] 杨立强, 邓军, 王中亮, 等. 胶东中生代金成矿系统[J]. 岩石学报, 2014, 30(9) : 2447-2467. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201409001.htm
[27] Yang L Q, Deng J, Guo L N, et al. Origin and evolution of ore fluid, and gold-deposition processes at the giant Taishang gold deposit, Jiaodong Peninsula, eastern China[J]. Ore Geology Reviews, 2016, 72: 585-602. doi: 10.1016/j.oregeorev.2015.08.021
[28] 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
[29] 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
[30] 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: 325-400.
[31] 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
[32] Chai P, Zhang H R, Dong L L, et al. Geology and ore-forming fluids of the Dayingezhuang gold deposit, Jiaodong Peninsula, eastern China: Implications for mineral exploration[J]. Journal of Geochemical Exploration, 2019, 204: 224-239. doi: 10.1016/j.gexplo.2019.06.001
[33] Chai P, Hou Z Q, Zhang H R, et al. Geology, Fluid Inclusion, and H- O-S-Pb Isotope Constraints on the Mineralization of the Xiejiagou Gold Deposit in the Jiaodong Peninsula[J]. Geofluids, 2019, 2019: 1-23.
[34] Chai P, Hou Z Q, Zhang Z Y. Geology, Fluid Inclusion and Stable Isotope Constraints on the Fluid Evolution and Resource Potential of the Xiadian Gold Deposit, Jiaodong Peninsula[J]. Resource Geology, 2017, 67(3) : 341-359. doi: 10.1111/rge.12134
[35] Guo L N, Deng J, Yang L Q, et al. Gold deposition and resource potential of the Linglong gold deposit, Jiaodong Peninsula: Geochemical comparison of ore fluids[J]. Ore Geology Reviews, 2020, 120: 1-17.
[36] 万多. 山东胶东地区招平断裂带北段金矿成矿规律与成矿预测[D]. 吉林大学博士学位论文, 2014.
[37] 张义东. 胶东水旺庄金矿床深部地质特征及成因机制研究[D]. 河北地质大学硕士学位论文, 2018.
[38] 孙丰月, 金巍, 李碧乐. 关于脉状热液金矿床成矿深度的思考[J]. 长春科技大学学报, 2000, 30(S1) : 27-29.
[39] 张华锋, 李胜荣, 翟明国, 等. 胶东半岛早白垩世地壳隆升剥蚀及其动力学意义[J]. 岩石学报, 2006, 22(2) : 285-295. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200602003.htm
[40] 王建平, 刘俊, 刘家军, 等. 黑云母全铝压力计估算胶东西北部玲珑花岗质杂岩剥蚀程度[J]. 矿物学报, 2009, 29(S1) : 481-482. https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2009S1251.htm
[41] 柳振江, 王建平, 郑德文, 等. 胶东西北部金矿剥蚀程度及找矿潜力和方向——来自磷灰石裂变径迹热年代学的证据[J]. 岩石学报, 2010, 26(12) : 3597-3611. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201012013.htm
-