现代地质 ›› 2021, Vol. 35 ›› Issue (06): 1608-1621.DOI: 10.19657/j.geoscience.1000-8527.2021.124
第鹏飞1(), 汤庆艳2, 刘聪2, 宋宏2,3,4, 张家和2, 刘东晓5, 王玉玺6, 蒲万峰6
收稿日期:
2021-09-10
修回日期:
2021-10-11
出版日期:
2021-12-10
发布日期:
2022-02-14
作者简介:
第鹏飞,男,高级工程师,1985年出生,矿物学、岩石学、矿床学,主要从事矿产资源储量评审和矿床学研究。Email: 236749076@qq.com。
基金资助:
DI Pengfei1(), TANG Qingyan2, LIU Cong2, SONG Hong2,3,4, ZHANG Jiahe2, LIU Dongxiao5, WANG Yuxi6, PU Wanfeng6
Received:
2021-09-10
Revised:
2021-10-11
Online:
2021-12-10
Published:
2022-02-14
摘要:
西秦岭造山带发育有大量三叠纪的金矿床,早子沟和加甘滩金矿床是其中最典型的两个矿床,其金资源量分别为116 t和154 t,均为特大型金矿床。早子沟、加甘滩金矿床均位于夏河—合作区域性逆冲推覆断裂以南。早子沟赋矿地层为三叠统古浪堤组,赋矿岩石为泥质板岩、条带状硅质板岩及粉砂质板岩;加甘滩矿区出露地层为三叠统隆务河组,金矿体赋存于长石石英变砂岩夹粉砂质板岩岩性段内。加甘滩金矿床的研究程度相对较低,属中低温构造蚀变岩型金矿床;早子沟金矿床研究程度较高,但是对它的成因仍有不同的认识。石英的微量元素地球化学特征能够提供成矿流体来源与演化的信息,通过对早子沟和加甘滩金矿床开展石英的微量元素地球化学特征研究,探讨其成矿流体来源、成矿条件以及石英微量元素对金矿床形成的指示,为西秦岭造山带金矿床成因研究提供重要的信息。早子沟和加甘滩金矿床不同类型矿石中石英具有相似的稀土元素球粒陨石标准化配分曲线,总体表现出轻稀土元素相对富集、重稀土元素轻微亏损的特征,而且轻稀土元素与重稀土元素分馏程度高,重稀土元素内部分馏程度弱。 早子沟金矿床成矿期热液石英中Rb与Li呈负相关,Rb与Cs呈正相关,而加甘滩金矿床热液石英中Rb与Li、Cs相关性不明显,表明早子沟金矿床石英中Li含量随流体含量的增加而减少,而Cs含量随流体含量的增加而增加。大多数样品具有Eu负异常和弱的Ce正异常,表明早子沟和加甘滩金矿床形成于还原环境,成矿温度较低。样品的(La/Yb)N较大,反映成矿深度相对较浅。石英的Y/Ho值分别为25.14~30.14和23.40~28.94,指示成矿流体与地壳关系密切。大多数石英样品的Th/La和 Nb/La 值小于1,在大陆地壳标准化图解中具有明显的Sc负异常,Cr、W、Pb和U正异常,表明成矿流体富Cl-,相对富集Cr、W、Pb和U等元素。结合大地构造背景分析,早子沟和加甘滩金矿形成于大陆边缘环境。
中图分类号:
第鹏飞, 汤庆艳, 刘聪, 宋宏, 张家和, 刘东晓, 王玉玺, 蒲万峰. 西秦岭夏河—合作地区早子沟和加甘滩金矿床石英微量元素特征及意义[J]. 现代地质, 2021, 35(06): 1608-1621.
DI Pengfei, TANG Qingyan, LIU Cong, SONG Hong, ZHANG Jiahe, LIU Dongxiao, WANG Yuxi, PU Wanfeng. Trace Element Characteristics of Quartz from the Zaozigou and Jiagantan Gold Deposits in the Xiahe-Hezuo District, West Qinling[J]. Geoscience, 2021, 35(06): 1608-1621.
图1 夏河—合作地区金矿床的分布图[41,42,43] 1.第四系;2.新近系;3.上三叠统;4.中—上三叠统;5.二叠系;6.石炭系;7.白垩纪玄武岩;8.三叠纪火山岩;9.印支期花岗岩;10.中酸性脉岩;11.断裂;12.角度不整合界线;13.金矿;14.铜矿;15.铅矿;16.锑矿;17.汞矿;18.铁矿;19.铁铜矿;20.铜钼矿;21.铜钨矿;22.多金属矿
Fig.1 Geologic map of the major gold deposits in the Xiahe-Hezuo region[41,42,43]
样品号 | 岩性 | 矿床 | Li | Be | Sc | V | Cr | Co | Ni | Cu | Pb | Zn | Cd | Rb | Sr | Y | Cs | W | Mo | Sb | Bi | Ba | Zr | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
ZD① | 花岗斑岩 | 早子沟 | 2.57 | 0.062 | 0.042 | 0.433 | 4.370 | 0.103 | 0.871 | 1.570 | 16.60 | 7.96 | 0.015 | 2.830 | 3.30 | 0.200 | 0.320 | 0.396 | 1.770 | 10.5 | 0.042 | 11.40 | 8.3 | |
ZH② | 花岗斑岩 | 3.15 | 0.119 | 0.265 | 1.120 | 1.250 | 0.337 | 1.010 | 4.450 | 22.40 | 3.77 | 0.017 | 6.370 | 13.70 | 0.908 | 0.605 | 0.883 | 0.393 | 17.0 | 0.473 | 17.10 | 16.0 | ||
ZH③ | 板岩 | 26.80 | 0.195 | 0.047 | 0.762 | 9.860 | 0.071 | 0.872 | 1.090 | 5.08 | 20.10 | 0.049 | 1.440 | 8.85 | 0.262 | 0.261 | 0.635 | 0.300 | 23.5 | 0.020 | 5.97 | 0.8 | ||
ZH④ | 石英脉 | 31.90 | 0.358 | 0.003 | 0.196 | 0.447 | 0.068 | 0.654 | 0.175 | 2.28 | 2.16 | n.d. | 0.893 | 2.43 | 0.090 | 0.337 | 0.102 | 0.078 | 124.0 | 0.010 | 5.18 | 0.7 | ||
ZH⑤ | 石英脉 | 18.30 | 0.161 | 0.017 | 0.337 | 6.030 | 0.089 | 0.921 | 0.381 | 10.40 | 5.68 | 0.018 | 0.973 | 2.40 | 0.085 | 0.208 | 59.400 | 0.358 | 24.8 | 0.013 | 3.89 | 0.4 | ||
ZH⑥ | 碳酸盐脉 | 14.10 | 0.176 | 0.079 | 1.310 | 2.220 | 0.218 | 7.310 | 3.310 | 16.90 | 4.05 | 0.009 | 3.320 | 5.98 | 0.176 | 0.337 | 1.600 | 0.069 | 274.0 | 0.112 | 9.04 | 1.6 | ||
JH① | 蚀变细 粒长英 质砂岩 | 加甘滩 | 5.05 | 0.032 | 0.019 | 0.310 | 0.383 | 0.071 | 0.371 | 0.443 | 4.74 | 5.69 | n.d. | 0.801 | 1.32 | 0.109 | 0.129 | 0.200 | 0.038 | 20.90 | 10.100 | 5.08 | 4.8 | |
JH② | 3.75 | 0.021 | 0.029 | 0.386 | 0.378 | 0.232 | 0.405 | 4.360 | 2.98 | 5.18 | n.d. | 0.847 | 1.64 | 0.117 | 0.124 | 0.226 | 0.043 | 28.60 | 9.810 | 5.99 | 1.0 | |||
JH③ | 1.54 | 0.035 | n.d. | 0.307 | 0.459 | 0.097 | 0.445 | 2.470 | 2.26 | 10.60 | 0.007 | 0.457 | 9.38 | 0.040 | 0.131 | 0.837 | 4.290 | 214.00 | 2.230 | 6.49 | 0.4 | |||
JH④ | 5.72 | 0.115 | 0.084 | 0.404 | 0.373 | 0.066 | 0.352 | 0.519 | 0.34 | 2.68 | n.d. | 0.654 | 23.40 | 0.463 | 0.129 | 0.415 | 0.048 | 8.06 | 0.021 | 3.13 | 0.2 | |||
JH⑤ | 石英脉 | 6.54 | 0.053 | 0.051 | 0.476 | 0.426 | 0.237 | 0.747 | 2.180 | 7.18 | 34.40 | 0.065 | 0.710 | 12.60 | 0.286 | 0.156 | 0.206 | 0.042 | 13.10 | 0.033 | 7.77 | 0.5 | ||
JH⑥ | 石英脉 | 4.42 | 0.050 | 0.004 | 0.571 | 0.487 | 0.152 | 1.400 | 0.835 | 1.03 | 5.40 | 0.005 | 0.779 | 5.02 | 0.101 | 0.145 | 0.283 | 0.199 | 14.70 | 0.036 | 6.23 | 0.8 | ||
样品号 | 岩性 | 矿床 | Nb | Ga | Tl | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Hf | Ta | Th | U | |
ZD① | 花岗斑岩 | 早子沟 | 0.169 | 0.391 | 0.044 | 0.329 | 0.670 | 0.074 | 0.284 | 0.054 | 0.013 | 0.050 | 0.007 | 0.039 | 0.008 | 0.020 | 0.003 | 0.017 | 0.003 | 0.251 | 0.060 | 0.163 | 0.2 | |
ZH② | 花岗斑岩 | 0.430 | 0.848 | 0.041 | 3.970 | 7.560 | 0.800 | 2.860 | 0.492 | 0.070 | 0.440 | 0.050 | 0.219 | 0.035 | 0.095 | 0.011 | 0.067 | 0.010 | 0.474 | 0.105 | 1.600 | 0.4 | ||
ZH③ | 板岩 | 0.119 | 0.173 | 0.016 | 1.100 | 2.150 | 0.236 | 0.835 | 0.152 | 0.030 | 0.120 | 0.013 | 0.055 | 0.010 | 0.027 | 0.004 | 0.023 | 0.003 | 0.029 | 0.020 | 0.375 | 0.1 | ||
ZH④ | 石英脉 | 0.029 | 0.088 | 0.015 | 0.068 | 0.142 | 0.017 | 0.074 | 0.018 | 0.003 | 0.015 | 0.002 | 0.014 | 0.003 | 0.009 | n.d. | 0.010 | 0.002 | 0.019 | 0.016 | 0.027 | 0.1 | ||
ZH⑤ | 石英脉 | 0.018 | 0.079 | 0.014 | 0.088 | 0.173 | 0.018 | 0.077 | 0.018 | 0.009 | 0.028 | 0.003 | 0.021 | 0.003 | 0.011 | n.d. | 0.007 | n.d. | 0.013 | 0.008 | 0.020 | 0.1 | ||
ZH⑥ | 碳酸盐脉 | 0.180 | 0.513 | 0.039 | 0.682 | 1.230 | 0.123 | 0.415 | 0.054 | 0.012 | 0.056 | 0.005 | 0.032 | 0.007 | 0.022 | n.d. | 0.022 | 0.004 | 0.053 | 0.027 | 0.142 | 0.1 | ||
JH① | 蚀变细 粒长英 质砂岩 | 加甘滩 | 0.049 | 0.098 | 0.011 | 0.086 | 0.170 | 0.019 | 0.070 | 0.012 | 0.003 | 0.013 | 0.002 | 0.019 | 0.004 | 0.015 | 0.002 | 0.019 | 0.003 | 0.140 | 0.016 | 0.104 | 1.8 | |
JH② | 0.074 | 0.102 | 0.010 | 0.127 | 0.265 | 0.031 | 0.112 | 0.023 | 0.004 | 0.023 | 0.003 | 0.021 | 0.005 | 0.015 | 0.002 | 0.016 | 0.003 | 0.030 | 0.015 | 0.044 | 0.1 | |||
JH③ | 0.035 | 0.056 | 0.011 | 0.158 | 0.294 | 0.032 | 0.111 | 0.021 | 0.005 | 0.017 | n.d. | 0.008 | n.d. | 0.005 | n.d. | 0.006 | n.d. | 0.014 | 0.007 | 0.055 | 0 | |||
JH④ | 0.023 | 0.044 | 0.011 | 0.033 | 0.089 | 0.036 | 0.101 | 0.037 | 0.013 | 0.074 | 0.013 | 0.082 | 0.016 | 0.040 | 0.006 | 0.032 | 0.005 | 0.006 | 0.014 | 0.197 | 0.1 | |||
JH⑤ | 石英脉 | 0.040 | 0.076 | 0.018 | 0.387 | 0.811 | 0.094 | 0.347 | 0.062 | 0.017 | 0.069 | 0.010 | 0.057 | 0.010 | 0.030 | 0.004 | 0.025 | 0.004 | 0.015 | 0.009 | 0.157 | 6.0 | ||
JH⑥ | 石英脉 | 0.083 | 0.083 | 0.014 | 0.645 | 1.300 | 0.148 | 0.524 | 0.063 | 0.009 | 0.042 | 0.004 | 0.018 | 0.004 | 0.016 | 0.003 | 0.015 | 0.003 | 0.023 | 0.014 | 0.176 | 0.4 |
表1 早子沟和加甘滩金矿床不同矿石中石英稀土和微量元素组成(10-6)
Table 1 REE and trace element concentrations of quartz for different ores from the Zaozigou and Jiagantan gold deposits(10-6)
样品号 | 岩性 | 矿床 | Li | Be | Sc | V | Cr | Co | Ni | Cu | Pb | Zn | Cd | Rb | Sr | Y | Cs | W | Mo | Sb | Bi | Ba | Zr | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
ZD① | 花岗斑岩 | 早子沟 | 2.57 | 0.062 | 0.042 | 0.433 | 4.370 | 0.103 | 0.871 | 1.570 | 16.60 | 7.96 | 0.015 | 2.830 | 3.30 | 0.200 | 0.320 | 0.396 | 1.770 | 10.5 | 0.042 | 11.40 | 8.3 | |
ZH② | 花岗斑岩 | 3.15 | 0.119 | 0.265 | 1.120 | 1.250 | 0.337 | 1.010 | 4.450 | 22.40 | 3.77 | 0.017 | 6.370 | 13.70 | 0.908 | 0.605 | 0.883 | 0.393 | 17.0 | 0.473 | 17.10 | 16.0 | ||
ZH③ | 板岩 | 26.80 | 0.195 | 0.047 | 0.762 | 9.860 | 0.071 | 0.872 | 1.090 | 5.08 | 20.10 | 0.049 | 1.440 | 8.85 | 0.262 | 0.261 | 0.635 | 0.300 | 23.5 | 0.020 | 5.97 | 0.8 | ||
ZH④ | 石英脉 | 31.90 | 0.358 | 0.003 | 0.196 | 0.447 | 0.068 | 0.654 | 0.175 | 2.28 | 2.16 | n.d. | 0.893 | 2.43 | 0.090 | 0.337 | 0.102 | 0.078 | 124.0 | 0.010 | 5.18 | 0.7 | ||
ZH⑤ | 石英脉 | 18.30 | 0.161 | 0.017 | 0.337 | 6.030 | 0.089 | 0.921 | 0.381 | 10.40 | 5.68 | 0.018 | 0.973 | 2.40 | 0.085 | 0.208 | 59.400 | 0.358 | 24.8 | 0.013 | 3.89 | 0.4 | ||
ZH⑥ | 碳酸盐脉 | 14.10 | 0.176 | 0.079 | 1.310 | 2.220 | 0.218 | 7.310 | 3.310 | 16.90 | 4.05 | 0.009 | 3.320 | 5.98 | 0.176 | 0.337 | 1.600 | 0.069 | 274.0 | 0.112 | 9.04 | 1.6 | ||
JH① | 蚀变细 粒长英 质砂岩 | 加甘滩 | 5.05 | 0.032 | 0.019 | 0.310 | 0.383 | 0.071 | 0.371 | 0.443 | 4.74 | 5.69 | n.d. | 0.801 | 1.32 | 0.109 | 0.129 | 0.200 | 0.038 | 20.90 | 10.100 | 5.08 | 4.8 | |
JH② | 3.75 | 0.021 | 0.029 | 0.386 | 0.378 | 0.232 | 0.405 | 4.360 | 2.98 | 5.18 | n.d. | 0.847 | 1.64 | 0.117 | 0.124 | 0.226 | 0.043 | 28.60 | 9.810 | 5.99 | 1.0 | |||
JH③ | 1.54 | 0.035 | n.d. | 0.307 | 0.459 | 0.097 | 0.445 | 2.470 | 2.26 | 10.60 | 0.007 | 0.457 | 9.38 | 0.040 | 0.131 | 0.837 | 4.290 | 214.00 | 2.230 | 6.49 | 0.4 | |||
JH④ | 5.72 | 0.115 | 0.084 | 0.404 | 0.373 | 0.066 | 0.352 | 0.519 | 0.34 | 2.68 | n.d. | 0.654 | 23.40 | 0.463 | 0.129 | 0.415 | 0.048 | 8.06 | 0.021 | 3.13 | 0.2 | |||
JH⑤ | 石英脉 | 6.54 | 0.053 | 0.051 | 0.476 | 0.426 | 0.237 | 0.747 | 2.180 | 7.18 | 34.40 | 0.065 | 0.710 | 12.60 | 0.286 | 0.156 | 0.206 | 0.042 | 13.10 | 0.033 | 7.77 | 0.5 | ||
JH⑥ | 石英脉 | 4.42 | 0.050 | 0.004 | 0.571 | 0.487 | 0.152 | 1.400 | 0.835 | 1.03 | 5.40 | 0.005 | 0.779 | 5.02 | 0.101 | 0.145 | 0.283 | 0.199 | 14.70 | 0.036 | 6.23 | 0.8 | ||
样品号 | 岩性 | 矿床 | Nb | Ga | Tl | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Hf | Ta | Th | U | |
ZD① | 花岗斑岩 | 早子沟 | 0.169 | 0.391 | 0.044 | 0.329 | 0.670 | 0.074 | 0.284 | 0.054 | 0.013 | 0.050 | 0.007 | 0.039 | 0.008 | 0.020 | 0.003 | 0.017 | 0.003 | 0.251 | 0.060 | 0.163 | 0.2 | |
ZH② | 花岗斑岩 | 0.430 | 0.848 | 0.041 | 3.970 | 7.560 | 0.800 | 2.860 | 0.492 | 0.070 | 0.440 | 0.050 | 0.219 | 0.035 | 0.095 | 0.011 | 0.067 | 0.010 | 0.474 | 0.105 | 1.600 | 0.4 | ||
ZH③ | 板岩 | 0.119 | 0.173 | 0.016 | 1.100 | 2.150 | 0.236 | 0.835 | 0.152 | 0.030 | 0.120 | 0.013 | 0.055 | 0.010 | 0.027 | 0.004 | 0.023 | 0.003 | 0.029 | 0.020 | 0.375 | 0.1 | ||
ZH④ | 石英脉 | 0.029 | 0.088 | 0.015 | 0.068 | 0.142 | 0.017 | 0.074 | 0.018 | 0.003 | 0.015 | 0.002 | 0.014 | 0.003 | 0.009 | n.d. | 0.010 | 0.002 | 0.019 | 0.016 | 0.027 | 0.1 | ||
ZH⑤ | 石英脉 | 0.018 | 0.079 | 0.014 | 0.088 | 0.173 | 0.018 | 0.077 | 0.018 | 0.009 | 0.028 | 0.003 | 0.021 | 0.003 | 0.011 | n.d. | 0.007 | n.d. | 0.013 | 0.008 | 0.020 | 0.1 | ||
ZH⑥ | 碳酸盐脉 | 0.180 | 0.513 | 0.039 | 0.682 | 1.230 | 0.123 | 0.415 | 0.054 | 0.012 | 0.056 | 0.005 | 0.032 | 0.007 | 0.022 | n.d. | 0.022 | 0.004 | 0.053 | 0.027 | 0.142 | 0.1 | ||
JH① | 蚀变细 粒长英 质砂岩 | 加甘滩 | 0.049 | 0.098 | 0.011 | 0.086 | 0.170 | 0.019 | 0.070 | 0.012 | 0.003 | 0.013 | 0.002 | 0.019 | 0.004 | 0.015 | 0.002 | 0.019 | 0.003 | 0.140 | 0.016 | 0.104 | 1.8 | |
JH② | 0.074 | 0.102 | 0.010 | 0.127 | 0.265 | 0.031 | 0.112 | 0.023 | 0.004 | 0.023 | 0.003 | 0.021 | 0.005 | 0.015 | 0.002 | 0.016 | 0.003 | 0.030 | 0.015 | 0.044 | 0.1 | |||
JH③ | 0.035 | 0.056 | 0.011 | 0.158 | 0.294 | 0.032 | 0.111 | 0.021 | 0.005 | 0.017 | n.d. | 0.008 | n.d. | 0.005 | n.d. | 0.006 | n.d. | 0.014 | 0.007 | 0.055 | 0 | |||
JH④ | 0.023 | 0.044 | 0.011 | 0.033 | 0.089 | 0.036 | 0.101 | 0.037 | 0.013 | 0.074 | 0.013 | 0.082 | 0.016 | 0.040 | 0.006 | 0.032 | 0.005 | 0.006 | 0.014 | 0.197 | 0.1 | |||
JH⑤ | 石英脉 | 0.040 | 0.076 | 0.018 | 0.387 | 0.811 | 0.094 | 0.347 | 0.062 | 0.017 | 0.069 | 0.010 | 0.057 | 0.010 | 0.030 | 0.004 | 0.025 | 0.004 | 0.015 | 0.009 | 0.157 | 6.0 | ||
JH⑥ | 石英脉 | 0.083 | 0.083 | 0.014 | 0.645 | 1.300 | 0.148 | 0.524 | 0.063 | 0.009 | 0.042 | 0.004 | 0.018 | 0.004 | 0.016 | 0.003 | 0.015 | 0.003 | 0.023 | 0.014 | 0.176 | 0.4 |
图4 早子沟(a)和加甘滩(b)金矿床不同矿石中石英微量元素原始地幔标准化配分曲线(球粒陨石数据引自Palme 和 O’Neill[48])
Fig.4 Chondrite-normalized REE patterns of the quartz for different ores from the Zaozigou(a) and Jiagantan(b) gold deposits (chondrite-normalized data after ref. [48])
图5 早子沟(a)和加甘滩(b)金矿床石英微量元素大陆地壳标准化曲线(大陆地壳数据引自文献[49])
Fig.5 Continental crust-normalized trace element patterns for the quartz from the Zaozigou (a) and Jiagantan (b) gold deposits (continental data after ref.[49])
图7 早子沟和加甘滩金矿床石英Sr与Rb(a)、U与Th(b)、Nb与Ta (c)、Hf与Zr(d)含量的相关性图解(锡矿床、变质石英和热液石英的范围来自Monecke et al. [57] )
Fig.7 Plots of Sr vs. Rb(a), U vs.Th (b), Nb vs. Ta (c), and Hf vs. Zr (d) of quartz from the Zaozigou and Jiagantan gold deposits (other data from ref. [57])
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