Chronology of Petrogenesis and Mineralization of Datongkeng Porphyry W-Mo Deposit in West Zhejiang
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摘要: 浙西淳安大铜坑斑岩型钨钼矿位于扬子陆块东南缘，矿体主要产于花岗岩体与南华系休宁组变质砂岩内外接触带上，是揭示浙皖赣相邻区域成矿规律的重要组成.成矿花岗岩为高钾钙碱性系列准过铝质Ⅰ型花岗岩，岩石富集Rb、K，亏损Sr、Ba等大离子亲石元素，富集Th、U，相对亏损Nb、Ta、Ti等高场强元素，稀土元素含量较低(ΣREE=106.2×10-6~211.5×10-6)，轻重稀土分异明显(ΣLREE/ΣHREE=6.4~12.2)，中等的Eu负异常(δEu=0.50~0.63)，具有类似岛弧岩浆岩的特征.锆石SHRIMP U-Pb定年结果表明花岗岩侵位时间为148.3±1.9 Ma，辉钼矿Re-Os等时线年龄显示成矿作用发生于146.47±0.81 Ma，成岩年龄与成矿时代高度耦合，进一步证实钨钼成矿作用与花岗岩体的形成有着密切的成因联系，二者在时间上是一个连续的过程，形成于晚侏罗世古太平洋板块俯冲挤压的构造环境，也是华南地区中生代第2次大规模钨钼成矿作用延续到浙西的响应.
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关键词:
- 锆石SHRIMP U-Pb年龄 /
- 辉钼矿Re-Os年龄 /
- 地球化学 /
- 年代学 /
- 大铜坑钨钼矿 /
- 花岗岩 /
- 浙西
Abstract: As an important component to reveal the metallogenic regularity in the Zhejiang-Anhui-Jiangxi border region, the Datongkeng porphyry W-Mo deposit in Chun'an County is located in the southeastern margin of the Yangtze block, and the W-Mo ore bodies are mainly located in the internal or external contact zones between granite and sandstone of Xiuning Formation. The Datongkeng granite is characterized by quasi-aluminous, showing the nature of Ⅰ-type granite and high-K calc-alkalic series rock. The granite is rich in Rb, K, Th, U, and relatively depleted in Sr, Ba, Nb, Ta, Ti. The total REE contents are relatively low (ΣREE=106.2×10-6-211.5×10-6), and the rocks show obvious LREE and HREE fractionation (ΣLREE/ΣHREE=6.4-12.2), moderately negative Eu anomalies (δEu=0.50-0.63), suggesting that these rocks have the characters of typical volcanic arc rocks. The SHRIMP U-Pb zircon age of 148.3±1.9 Ma for granite is close to the Re-Os isochron age of 146.47±0.81 Ma for five molybdenite samples from the Datongkeng W-Mo deposit, indicating magmatism and mineralization are a continuous process, which took place in the compression tectonic environment related to the subduction of pacific plate at Late Jurassic, and corresponds to the second large-scale W-Mo mineralization in South China. -
图 2 大铜坑钨钼矿区地质图(a)和L12勘探线剖面(b)
Fig. 2. Geological map of the Datongkeng tungsten-molybdenum deposit (a) and a profile from No.12 exploration line (b)
图 3 大铜坑花岗岩地质特征和镜下显微照片
a.基性岩墙群；b.含辉钼矿石英脉体；c.花岗岩岩心；d.斜长石斑晶，正交偏光；e.钾长石斑晶，正交偏光；f.石英斑晶，正交偏光.Bt.黑云母；Kfs.钾长石；Pl.斜长石；Qz.石英
Fig. 3. Geological feature and photomicrography of the Datongkeng granite
图 4 大铜坑花岗岩A/NK-A/CNK(a)及K2O-SiO2(b)图解
图a据Maniar and Piccoli(1989)；图b据Rickwood(1989)
Fig. 4. A/NK vs. A/CNK diagram (a) and K2O vs. SiO2 diagram (b) for the Datongkeng granite
图 5 大铜坑花岗岩稀土元素球粒陨石标准化曲线(a)和微量元素蛛网图(b)
Fig. 5. Chondrite-normalized REE patterns (a) and trace element spider diagram (b) for the Datongkeng granite
图 6 大铜坑花岗岩锆石的阴极发光图像及SHRIMP分析点位和206Pb-238U视年龄
Fig. 6. CL photomicrographs, meansured points and age data (206Pb/238U) of zircons from the Datongkeng granite
图 7 大铜坑花岗岩锆石SHRIMP U-Pb年龄谐和图(a, b, c, d)和加权平均年龄(e, f)
Fig. 7. SHRIMP U-Pb concordia ages (a, b, c, d) and average model ages (e, f) of zircons from the Datongkeng granite
图 8 大铜坑钨钼矿床辉钼矿Re-Os同位素等时线年龄(a)及模式年龄加权平均值(b)
Fig. 8. Re-Os weighted isochronage (a) and average model ages (b) of molybdenite from the Datongkeng W-Mo deposit
图 9 大铜坑花岗岩Sr/Y-Y(a)和LaN/YbN-YbN(b)图解
据Defant and Drummond(1990)和Defant and Kepezhinskas(2001)
Fig. 9. Sr/Y vs. Y diagram (a) and LaN/YbN vs. YbN (b) diagram for the Datongkeng granite
图 10 大铜坑花岗岩构造环境判别图解
图a, b, c, d据Pearce et al.(1984)；图e据Harris et al.(1986)；图f据Batchelor and Bowden(1985)
Fig. 10. Tectonic setting discriminative diagram for the Datongkeng granite
表 1 大铜坑花岗岩主量元素(%)和微量元素(10-6)组成
Table 1. Major elements (%) and trace elements (10-6) of the Datongkeng granite
样品 DTK01 DTK02 DTK03 DTK04 DTK05 DTK06 DTK07 DTK08 DTK09 DTK10 DTK11 SiO2 68.78 69.16 68.68 67.28 68.47 70.74 67.77 67.33 69.55 68.97 68.38 TiO2 0.43 0.45 0.40 0.44 0.34 0.39 0.44 0.40 0.43 0.40 0.44 Al2O3 14.80 14.27 13.78 14.80 14.68 13.01 13.64 13.64 14.84 14.25 13.97 TFe2O3 3.08 3.22 2.56 2.91 3.58 4.04 5.40 4.62 3.01 4.81 6.43 MnO 0.04 0.04 0.04 0.03 0.03 0.03 0.04 0.07 0.09 0.06 0.08 MgO 0.94 0.97 0.86 0.94 0.98 0.78 0.89 0.76 0.82 0.79 0.87 CaO 2.73 2.40 2.45 2.41 2.27 1.3 2.39 3.12 2.33 2.16 2.40 Na2O 3.33 3.06 2.93 3.31 2.78 2.27 2.63 3.00 3.33 2.95 3.00 K2O 3.82 4.34 4.43 4.30 4.5 5.84 3.89 3.84 3.91 3.91 3.45 P2O5 0.15 0.16 0.14 0.15 0.18 0.17 0.18 0.12 0.13 0.12 0.13 LOI 1.58 1.70 3.28 2.80 1.72 0.98 2.32 2.7 1.1 1.23 0.38 Total 99.68 99.77 99.55 99.37 99.53 99.55 99.59 99.59 99.54 99.66 99.53 A/CNK 1.02 1.01 0.98 1.02 1.08 1.05 1.06 0.92 1.06 1.10 1.07 K2O/Na2O 1.15 1.42 1.51 1.30 1.62 2.57 1.48 1.28 1.17 1.33 1.15 σ 1.98 2.09 2.11 2.39 2.08 2.37 1.71 1.93 1.97 1.82 1.64 Mg# 44 43 46 45 41 33 30 30 41 29 26 A.R 2.23 2.16 2.13 2.25 1.98 3.62 1.98 2.12 2.27 2.12 2.16 DI 79.70 81.18 82.18 81.15 79.60 84.96 76.68 76.72 80.72 78.62 75.26 Ba 386 373 517 383 324 357 347 322 314 410 242 Rb 195 243 252 257 256 241 225 224 234 203 143 Sr 309 242 177 252 198 201 182 190 197 182 182 Y 22.6 24.5 20.0 24.7 24.2 23.9 22.4 21.8 23.9 22.3 21.5 Zr 131 141 128 154 121 118 106 109 115 108 111 Nb 15.4 15.6 13.9 18.5 18.9 21.2 19.4 17.9 19.7 18.3 19 Th 21.5 18.5 19.8 22.4 19.6 18.7 16.4 18.6 19 20.1 17.2 Ga 21.8 20.1 17.6 22.7 18.6 19.4 17.4 17.6 18.7 17.8 18.9 Hf 3.95 4.30 3.90 4.67 3.55 3.69 3.26 3.38 3.64 3.47 3.41 Ta 1.48 1.58 1.40 1.76 2.08 2.21 1.91 1.95 2.19 2.07 1.94 U 9.51 12.2 11.5 9.86 12.8 11.9 9.31 12.3 13 9.9 9.2 La 37.3 26.5 21.9 38.6 38 39 25.6 21.6 19.9 27.8 21.3 Ce 72.4 54.6 43.6 76.5 93 86 51.5 44.2 43.2 56.3 44 Pr 7.91 6.35 5.03 8.71 8.60 10.10 6.00 5.04 4.87 6.38 5.01 Nd 29.1 24.6 20.0 32.2 35 43 22.7 19 18.8 23.6 19 Sm 5.70 5.13 4.08 6.45 6.4 8.6 4.84 4.15 4.36 4.82 4.15 Eu 1.01 0.94 0.80 1.03 1.04 1.35 0.86 0.71 0.78 0.81 0.76 Gd 4.80 4.64 3.72 5.29 5.50 7.80 4.44 3.9 4.2 4.3 3.91 Tb 0.70 0.71 0.57 0.78 0.66 1.15 0.71 0.64 0.7 0.69 0.64 Dy 4.01 4.06 3.34 4.30 3.60 6.20 3.91 3.59 3.96 3.72 3.57 Ho 0.71 0.74 0.61 0.76 0.66 1.14 0.73 0.68 0.75 0.69 0.67 Er 1.94 2.11 1.75 2.14 2.00 3.30 2.02 1.92 2.11 1.97 1.9 Tm 0.30 0.31 0.27 0.31 0.27 0.45 - - - - - Yb 1.99 2.24 1.85 2.17 1.9 3.00 2.02 2.04 2.25 2.04 1.98 Lu 0.31 0.34 0.28 0.32 0.28 0.42 0.31 0.31 0.33 0.3 0.3 ΣREE 168.18 133.27 107.80 179.56 196.91 211.51 125.64 107.78 106.21 133.42 107.19 LREE/HREE 10.4 7.8 7.7 10.2 12.2 8.0 7.9 7.2 6.4 8.7 7.3 Rb/Sr 0.63 1.00 1.42 1.02 1.29 1.20 1.24 1.18 1.19 1.12 0.79 Sr/Y 13.67 9.88 8.85 9.20 8.18 8.41 8.13 8.72 8.24 8.16 8.47 LaN/YbN 13.4 8.5 8.5 12.8 14.3 9.3 9.1 7.6 6.4 9.8 7.7 LaN/SmN 4.2 3.3 3.5 3.9 3.8 2.9 3.4 3.4 3.0 3.7 3.3 GdN/YbN 2.0 1.7 1.7 2.0 2.4 2.2 1.8 1.6 1.5 1.7 1.6 δEu 0.59 0.59 0.63 0.54 0.54 0.50 0.57 0.54 0.56 0.55 0.58 TZr(℃) 809 816 804 822 805 803 792 784 801 796 797 注：A/CNK=Al2O3/(CaO+Na2O+K2O)mol；Mg#=(MgO/40.31)/(MgO/40.31+0.7×TFe2O3/71.85)；DTK01~DTK06数据为本次实测，DTK07~DTK11数据引自 Li et al.(2013) .
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表 2 大铜坑花岗岩体中锆石的SHRIMP U-Pb年龄测定结果
Table 2. SHRIMP U-Pb dating result of zircons from the Datongkeng granite
点号 206Pbc(%) U(10-6) Th(10-6) 232Th/238U 206Pb*(10-6) 年龄(Ma) 206Pb/238U ±1σ(%) 207Pb*/206Pb* ±1σ(%) 207Pb*/235U ±1σ(%) 206Pb*/238U CA1-1.1 1.96 225 222 1.02 4.6 148.5 3.9 0.046 3 7.9 0.153 0 8.4 0.023 3 2.7 CA1-2.1 0.73 693 814 1.21 13.4 142.6 3.4 0.056 3 3.0 0.146 8 3.9 0.022 4 2.4 CA1-3.1 0.31 1 750 300 0.18 32.6 138.1 3.2 0.046 5 2.3 0.143 1 3.3 0.021 6 2.3 CA1-4.1 0.47 1 712 288 0.17 31.8 137.0 3.2 0.048 6 2.2 0.139 3 3.2 0.021 5 2.3 CA1-5.1 0.12 2 178 361 0.17 39.0 132.7 4.0 0.047 4 1.9 0.137 5 3.6 0.020 8 3.1 CA1-6.1 0.44 1 119 146 0.13 20.6 136.2 3.2 0.048 0 3.0 0.141 4 3.8 0.021 4 2.4 CA1-7.1 0.20 1 815 361 0.21 32.9 134.4 3.1 0.046 9 2.0 0.140 4 3.1 0.021 1 2.3 CA1-8.1 0.26 2 145 424 0.20 38.3 132.2 3.0 0.047 7 1.9 0.136 5 3.0 0.020 7 2.3 CA1-9.1 0.07 1 724 362 0.22 31.5 135.5 3.5 0.047 8 2.0 0.140 8 3.3 0.021 2 2.6 CA1-10.1 0.46 158 150 0.98 17.0 756.3 17.7 0.064 8 2.6 1.126 0 3.6 0.124 5 2.5 CA1-11.1 0.43 1 938 377 0.20 34.0 129.9 3.0 0.049 8 2.3 0.137 9 3.2 0.020 4 2.3 CA1-12.1 0.22 447 184 0.43 50.0 788.1 17.5 0.069 2 1.4 1.185 0 2.8 0.130 0 2.4 CA1-13.1 0.53 1 057 345 0.34 19.9 139.1 3.2 0.049 9 2.6 0.145 8 3.5 0.021 8 2.4 CA1-14.1 0.34 2 440 536 0.23 42.9 130.1 3.0 0.049 2 1.8 0.139 1 2.9 0.020 4 2.3 CA1-15.1 0.32 1 184 253 0.22 27.7 172.8 4.1 0.037 3 3.7 0.209 8 4.4 0.027 2 2.4 CA1-16.1 0.18 894 1 161 1.34 18.0 148.9 3.1 0.048 7 1.9 0.152 4 2.9 0.023 4 2.1 CA1-17.1 / 146 30 0.21 2.88 146.7 3.6 0.047 8 5.0 0.156 3 5.9 0.023 0 2.5 CA1-18.1 0.02 1 046 336 0.33 21.5 152.7 3.1 0.050 1 1.6 0.165 0 2.9 0.024 0 2.1 CA1-19.1 10.09 2 154 3 173 1.52 46.4 144.1 3.1 0.131 5 6.6 0.160 0 23 0.022 6 2.2 CA1-20.1 / 488 465 0.99 59.1 851.1 16 0.066 5 0.90 1.293 0 2.2 0.141 1 2.0 CA1-21.1 0.69 95 74 0.81 10.5 782.0 17 0.066 2 2.1 1.075 0 4.6 0.129 0 2.3 CA1-22.1 0.02 1 078 871 0.84 126 822.2 15 0.065 5 0.66 1.226 0 2.2 0.136 1 2.0 CA1-23.1 4.82 568 405 0.74 11.8 147.0 3.2 0.090 9 1.7 0.168 0 12 0.023 1 2.2 CA1-24.1 0.00 139 203 1.51 2.81 150.3 3.6 0.050 2 4.6 0.163 2 5.2 0.023 6 2.4 CA1-25.1 0.18 799 1 062 1.37 15.6 144.2 3.0 0.051 8 2.0 0.157 1 3.5 0.022 6 2.1 CA1-26.1 / 481 54 0.12 9.71 149.6 3.2 0.047 2 2.5 0.154 7 3.3 0.023 5 2.1 CA1-27.1 0.01 539 779 1.49 10.8 148.7 3.1 0.049 2 2.3 0.158 0 3.1 0.023 3 2.1 CA1-28.1 / 322 524 1.68 6.58 151.7 3.3 0.048 2 3.2 0.164 9 5.6 0.023 8 2.2 注：误差为1σ；Pbc和Pb*分别代表普通铅和放射性成因铅；标准校正值的误差为0.40%(不包括在上述误差内，但包括不同样品靶的数据比较).应用实测204Pb校正普通铅.
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表 3 大铜坑钨钼矿区辉钼矿Re-Os同位素组成
Table 3. Re-Os isotopic analyses of molybdenite from ores of the Datongkeng W-Mo deposit
编号 样号 样重(g) Re(10-6) Os普(10-9) 187Re(10-6) 187Os(10-9) 模式年龄(Ma) 150417-4 DTK01 0.002 10 116.70±0.80 0.473 2±0.057 1 73.37±0.49 178.80±1.00 146.1±1.9 150417-5 DTK02 0.002 20 28.63±0.18 0.391 9±0.108 7 17.99±0.11 44.01±0.36 146.6±2.1 150417-6 DTK03 0.002 18 9.70±0.08 0.376 2±0.100 0 6.10±0.05 14.83±0.11 145.8±2.2 150417-7 DTK04 0.002 41 94.34±0.64 0.390 5±0.079 7 59.30±0.40 145.21±0.90 146.8±2.0 150417-8 DTK05 0.002 35 94.22±0.66 1.066 3±0.080 2 59.22±0.41 144.40±0.91 146.2±2.0
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表 4 浙皖赣相邻区钨钼矿区成岩年龄及成矿时代
Table 4. The formation age of plutons from the important deposits in West Zhejiang and adjacent regions
矿区名称 岩体岩性 成岩年龄和成矿时代 测试方法 资料来源 乐平塔前钨钼矿 花岗闪长岩 159.7±1.8 Ma LA-ICP-MS锆石U-Pb 刘善宝等，2014 乐平塔前钨钼矿 花岗闪长岩 162±2 Ma 辉钼矿Re-Os 黄安杰等，2013 铅山永平铜钨钼矿 花岗岩 160.0±2.3 Ma SIMS锆石U-Pb 丁昕等，2005 铅山永平铜钨钼矿 花岗岩 156.7±2.8 Ma 辉钼矿Re-Os 李晓峰等，2007 桐庐彰坞钨矿 花岗岩 159.7±2.6 Ma LA-ICP-MS锆石U-Pb 笔者，未发表 绩溪背靠山钨矿 花岗闪长斑岩 152.7~147.7 Ma SHRIMP锆石U-Pb 周翔等，2012 淳安县开岭脚钼矿 花岗闪长岩 151±3 Ma SHRIMP锆石U-Pb 汪建国等，2010 余杭闲林铁钼(铜钨)矿 花岗闪长岩 151.8±2.2 Ma SHRIMP锆石U-Pb 唐增才等，2014 余杭闲林铁钼(铜钨)矿 花岗闪长岩 149.7 Ma 辉钼矿Re-Os 王永彬等，2013 武宁石门寺钨矿 花岗岩 144.2±1.3 Ma LA-ICP-MS锆石U-Pb 黄兰椿和蒋少涌，2012 武宁石门寺钨矿 花岗岩 149.6±1.2 Ma 辉钼矿Re-Os 项新葵等，2013 绍兴漓渚铁钼(钨)矿 花岗闪长岩 150.1±2.6 Ma LA-ICP-MS锆石U-Pb 顾明光等，2011 绍兴漓渚铁钼(钨)矿 花岗闪长岩 149.3 Ma 辉钼矿Re-Os 王永彬等，2013 淳安大铜坑钨钼矿 花岗岩 148.3±1.9 Ma SHRIMP锆石U-Pb 本文 淳安大铜坑钨钼矿 花岗岩 146.47±0.81 Ma 辉钼矿Re-Os 本文 祁门东源钨钼矿 花岗闪长斑岩 146±1 Ma SHRIMP锆石U-Pb 周翔等，2011 淳安大铜坑钨钼矿 花岗岩 146.4±2.3 Ma 辉钼矿Re-Os 周翔等，2011 淳安木瓜钨矿 花岗斑岩 142.2±1.2 Ma LA-ICP-MS锆石U-Pb 厉子龙等，2013 歙县邓家坞钼矿 花岗闪长斑岩 141.8±2.2 Ma 辉钼矿Re-Os 李双等，2012 安吉港口铅锌钨钼矿 花岗闪长岩 141.0±1.4 Ma LA-ICP-MS锆石U-Pb 唐燕文等，2013 安吉港口铅锌钨钼矿 花岗闪长岩 141.2±1.1 Ma 辉钼矿Re-Os 唐燕文等，2013 龙泉毛断钼多金属矿 花岗岩 140.0±1.6 Ma LA-ICP-MS锆石U-Pb 李艳军等，2011 龙泉毛断钼多金属矿 花岗岩 139.0±0.8 Ma 辉钼矿Re-Os 李艳军等，2011
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Batchelor, R.A., Bowden, P., 1985.Petrogenetic Interpretation of Granitoid Rock Series Using Multicationic Parameters.Chemical Geology, 48(1-4):43-55.doi: 10.1016/0009-2541(85)90034-8 Chen, P.R., Hua, R.M., Zhang, B.T., et al., 2002.Early Yanshanian Post-Orogenic Granitoids in the Nanling Region:Petrological Constraints and Geodynamic Settings.Science in China (Series D), 45(8):755-768.doi: 10.1360/02yd9076 Defant, M.J., Drummond, M.S., 1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature, 347(6294):662-665.doi: 10.1038/347662a0 Defant, M.J., Kepezhinskas, P., 2001.Evidence Suggests Slab Melting in Arc Magmas.EOS, Transactions American Geophysical Union, 82(6):65-65.doi: 10.1029/01eo00038 Ding, X., Jiang, S.Y., Ni, P., et al., 2005.Zircon SIMS U-Pb Geochronology of Host Granitoids in Wushan and Yongping Copper Deposits, Jiangxi Province.Geological Journal of China Universities, 11(3):383-389(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200503009.htm Du, A.D., He, H.L., Yin, N.W., et al., 1994.A Study on the Rhenium-Osmium Geochronometry of Molybdenites.Acta Geologica Sinica, 68(4):339-347(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXW199502003.htm Du, A.D., Wu, S.Q., Sun, D.Z., et al., 2004.Preparation and Certification of Re-Os Dating Reference Materials: Molybdenites HLP and JDC.Geostandards and Geoanalytical Research, 28(1):41-52.doi: 10.1111/j.1751-908x.2004.tb01042.x Govindaraju, K., 1994.Compilation of Working Values and Sample Description for 383 Geostandards.Geostandards and Geoanalytical Research, 18:1-158.doi: 10.1111/j.1751-908x.1994.tb00526.x Gu, M.G., Feng, L.X., Hu, Y.H., et al., 2011.LA-ICP-MS U-Pb Dating of Zircons from Guangshan and Zhaxi Plutons in Shaoxing Area, Zhejiang Province: Constraint on the Ore-Forming Epoch of the Lizhu Iron Ore Deposit.Geological Bulletin of China, 30(8):1212-1219(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD201108005.htm Harris, N.B.W., Pearce, J.A., Tindle, A.G., 1986.Geochemical Characteristics of Collision-Zone Magmatism.Geological Society, London, Special Publications, 19(1):67-81.doi: 10.1144/gsl.sp.1986.019.01.04 He, G.J., Yang, X.C., Wu, G.M., et al., 2011.A Study of Ore Mineral Characteristics and Metallogenic Stages of the Yinshan Ag-Pb-Zn Polymetallic Ore Deposit, Northwest Zhejiang Province.Acta Geoscientica Sinica, 32(3):304-312(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB201103007.htm Hu, Y.Z., Li, Z.L., Mao, J.R., et al., 2013.Ore Texture and Structure and Compositions of Yinshan Polymetallic Ore Deposit in Chun'an County from the Northwestern Zhejiang Province of the Southeastern China and Its Implication for Mineralized Mechanism.Acta Petrologica Sinica, 29(10):3623-3636(in Chinese with English abstract). https://www.researchgate.net/publication/35294928_The_influence_of_saprolite_composition_texture_and_structure_on_groundwater_flow_in_the_Piedmont_Province_Henry_County_Virginia Hua, R.M., Chen, P.R., Zhang, W.L., et al., 2003.Metallogenic Systems Related to Mesozoic and Cenozoic Granitoids in South China.Science in China(Series D), 33(4):335-343(in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB201103007.htm Hua, R.M., Chen, P.R., Zhang, W.L., et al., 2005.Three Major Metallogenic Events in Mesozoic in South China.Mineral Deposits, 24(2):99-107(in Chinese with English abstract). https://www.researchgate.net/publication/284690423_Three_major_metallogenic_events_in_Mesozoic_in_South_China Huang, A.J., Wen, Z.G., Liu, S.B., et al., 2013.Re-Os Isotopic Dating of Molybdenite from the Taqian W-Mo Deposit in Leping County, Jiangxi Province and Its Geological Implications.Acta Petrologica et Mineralogica, 32(4):496-504(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201304007.htm Huang, L.C., Jiang, S.Y., 2012.Zircon U-Pb Geochronology, Geochemistry and Petrogenesis of the Porphyric-Like Muscovite Granite in the Dahutang Tungsten Deposit, Jiangxi Province.Acta Petrologica Sinica, 28(12):3887-3900(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201212008.htm Jian, P., Liu, D.Y., Sun, X.M., 2003.SHRIMP Dating of Carboniferous Jinshajiang Ophiolite in Western Yunnan and Sichuan:Geochronological Constraints on the Evolution of the Paleo-Tethys Oceanic Crust.Acta Geologica Sinica, 77(2): 217-228 (in Chinese with English abstract). https://www.researchgate.net/publication/291106957_SHRIMP_dating_of_carboniferous_Jinshajiang_ophiolite_in_western_Yunnan_and_Sichuan_Geochronological_constraints_on_the_evolution_of_the_Paleo-Tethys_oceanic_crust Li, F.L., Xie, Y., Zhou, H.W., et al., 2011a.Petrogenesis and Geodynamic Setting of Early Cretaceous Dykes in the Chun'an Area, Zhejiang Province.Journal of Mineralogy and Petrology, 31(3):55-65 (in Chinese with English abstract). https://www.researchgate.net/publication/289640123_Petrogenesis_and_gedynamic_setting_of_early_cretaceous_dykes_in_the_Chun'an_area_Zhejiang_Province Li, F.L., Zhou, H.W., Tang, Z.C., et al., 2011b.U-Pb Ages, Geochemistry and Tectonic Implications of Mafic Dyke Swarms in Mugua, Chun'an County, Zhejiang Province.Geochimica, 40(1):22-34(in Chinese with English abstract). https://www.researchgate.net/profile/Yilong_Li2/publication/289640123_Petrogenesis_and_gedynamic_setting_of_early_cretaceous_dykes_in_the_Chun%27an_area_Zhejiang_Province/links/5697866a08aec79ee32b3504.pdf?origin=publication_detail Li, S., Yang, X.Y., Sun, W.D., 2012.Ages and Zircon Hf Isotope Geochemistry of the Dengjiawu Mo Deposit in Shexian, South Anhui Province.Acta Petrologica Sinica, 28(12):3980-3992(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201212015.htm Li, S., Yang, X.Y., Sun, W.D., et al., 2014.Zircon Dating, Hf Isotope Composition, Geochemistry and Their Prospecting Signification of the Langqiao Intrusion in Jingxian County, South Anhui Province.Acta Geologica Sinica, 88(8):1561-1578 (in Chinese with English abstract). http://d.wanfangdata.com.cn/CitedResourceRss.ashx?ID=NSTLQK_NSTL_QKJJ026563309&Title=Metamorphic+zircon+formation+by+solid-state+recrystallization+of+protolith+igneous+zircon Li, X.F., Yasushi Watanabe, Qu, W.J., 2007.Textures and Geochemical Characteristics of Granitic Rocks in the Yongping Climax-Type Cu-Mo Deposit, Jiangxi, Southeastern China, and Their Alteration, Mineralization and Tectonic Regime.Acta Petrologica Sinica, 23(10):2353-2365(in Chinese with English abstract). https://www.researchgate.net/publication/279908699_Textures_and_geochemical_characteristics_of_granitic_rocks_in_the_Yongping_climax-type_Cu-Mo_deposit_Jiangxi_southeastern_China_and_their_alteration_mineralization_and_tectonic_regime Li, X.H., 2000.Cretaceous Magmatism and Lithospheric Extension in Southeast China.Journal of Asian Earth Sciences, 18(3):293-305.doi: 10.1016/s1367-9120(99)00060-7 Li, X.H., Chen, Z.G., Liu, D.Y., et al., 2003.Jurassic Gabbro-Granite-Syenite Suites from Southern Jiangxi Province, SE China:Age, Origin, and Tectonic Significance.International Geology Review, 45(10):898-921.doi: 10.2747/0020-6814.45.10.898 Li, X.H., Li, W.X., Li, Z.X., 2007.On the Genetic Classification and Tectonic Implications of the Early Yanshanian Granitoids in the Nanling Range, South China.Chinese Science Bulletin, 52(14):1873-1885.doi: 10.1007/s11434-007-0259-0 Li, Y.J., Wei, J.H., Wu, G., et al., 2011.Re-Os Dating of Molybdenite from the Maoduan Lead-Zinc Polymetallic Deposit in Southwestern Zhejiang Province and Its Geological Significance.Earth Science, 36(2):289-298(in Chinese with English abstract). https://www.researchgate.net/publication/286546465_Re-Os_dating_of_molybdenite_from_the_Maoduan_lead-zinc_polymetallic_deposit_in_southwestern_Zhejiang_Province_and_its_geological_significance Li, Z.L., Zhou, J., Mao, J.R., et al., 2013.Age and Geochemistry of the Granitic Porphyry from the Northwestern Zhejiang Province, SE China, and Its Geological Significance.Acta Petrologica Sinica, 29(10):3607-3622(in Chinese with English abstract). https://www.researchgate.net/publication/304816027_Age_and_Geochemistry_of_the_Granitic_Porphyry_from_the_Northwestern_Zhejiang_Province_SE_China_and_Its_Geological_Significance Li, Z.L., Zhou, J., Mao, J.R., et al., 2013.Zircon U-Pb Geochronology and Geochemistry of Two Episodes of Granitoids from the Northwestern Zhejiang Province, SE China:Implication for Magmatic Evolution and Tectonic Transition.Lithos, 179:334-352.doi: 10.1016/j.lithos.2013.07.014 Liu, S.B., Wang, C.H., Liu, Z.Q., et al., 2014.Northeast Jiangxi Taqian-Fuchun Metallogenic Belt Magmatite Time Limit and Sequence Division and Its Significance.Rock and Mineral Analysis, 33(4):598-611(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YKCS201404024.htm Liu, Y.S., Zong, K.Q., Kelemen, P.B., et al., 2008.Geochemistry and Magmatic History of Eclogites and Ultramafic Rocks from the Chinese Continental Scientific Drill Hole:Subduction and Ultrahigh-Pressure Metamorphism of Lower Crustal Cumulates.Chemical Geology, 247(1-2):133-153.doi: 10.1016/j.chemgeo.2007.10.016 Maniar, P.D., Piccoli, P.M., 1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin, 101(5):635-643.doi:10.1130/0016-7606(1989)101＜0635:tdog＞2.3.co; 2 Mao, J.R., Yutaka Takahashi, Li, Z.L., et al., 2009.Correlation of Meso-Cenozoic Tectono-Magmatism between SE China and Japan.Geological Bulletin of China, 28(7):844-856(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200907006.htm Mao, J.W., Chen, M.H., Yuan, S.D., et al., 2011.Geological Characteristics of the Qinhang (or Shihang) Metallogenic Belt in South China and Spatial-Temporal Distribution Regularity of Mineral Deposits.Acta Geologica Sinica, 85(5):636-658(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201105006.htm Mao, J.W., Zhang, Z.C., Zhang, Z.H., et al., 1999.Re-Os Isotopic Dating of Molybdenites in the Xiaoliugou W (Mo) Deposit in the Northern Qilian Mountains and Its Geological Significance.Geochimica et Cosmochimica Acta, 63(11-12):1815-1818.doi: 10.1016/s0016-7037(99)00165-9 Pearce, J.A., Harris, N.B.W., Tindle, A.G., 1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology, 25(4):956-983.doi: 10.1093/petrology/25.4.956 Qin, Y., Wang, D.H., Wu, L.B., et al., 2010.Zircon SHRIMP U-Pb Dating of the Mineralized Porphyry in the Dongyuan W Deposit in Anhui Province and Its Geological Significance.Acta Geologica Sinica, 84(4):479-484 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201004003.htm Qiu, J.T., Yu, X.Q., Zhang, D.H., et al., 2011.LA-ICP-MS Zircon U-Pb Dating of the Tongcun Porphyry in Kaihua County, Western Zhejiang Province, and its Geological Significance.Geological Bulletin of China, 30(9):1360-1368(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201109004.htm Rickwood, P.C., 1989.Boundary Lines within Petrologic Diagrams Which Use Oxides of Major and Minor Elements.Lithos, 22(4):247-263.doi: 10.1016/0024-4937(89)90028-5 Selby, D., Creaser, R.A., 2001a.Re-Os Geochronology and Systematics in Molybdenite from the Endako Porphyry Molybdenum Deposit, British Columbia, Canada.Economic Geology, 96(1):197-204.doi: 10.2113/gsecongeo.96.1.197 Selby, D., Creaser, R.A., 2001b.Late and Mid-Cretaceous Mineralization in the Northern Canadian Cordillera:Constraints from Re-Os Molybdenite Dates.Economic Geology, 96(6):1461-1467.doi: 10.2113/96.6.1461 Selby, D., Creaser, R.A., Hart, C.J.R., et al., 2002.Absolute Timing of Sulfide and Gold Mineralization:A Comparison of Re-Os Molybdenite and Ar-Ar Mica Methods from the Tintina Gold Belt, Alaska.Geology, 30(9):791-794.doi:10.1130/0091-7613(2002)030＜0791:atosag＞2.0.co; 2 Shirey, S.B., Walker, R.J., 1995.Carius Tube Digestion for Low-Blank Rhenium-Osmium Analysis.Analytical Chemistry, 67(13):2136-2141.doi: 10.1021/ac00109a036 Smoliar, M.I., Walker, R.J., Morgan, J.W., 1996.Re-Os Ages of Group IIA, IVA, and IVB Iron Meteorites.Science, 271(5252):1099-1102.doi: 10.1126/science.271.5252.1099 Song, B., Zhang, Y.H., Wan, Y.S., et al., 2002.Mount Making and Procedure of the SHRIMP Dating.Geological Review, 48(Suppl.1):26-30 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP2002S1006.htm Stein, H.J., Markey, R.J., Morgan, J.W., et al., 1997.Highly Precise and Accurate Re-Os Ages for Molybdenite from the East Qinling Molybdenum Belt, Shaanxi Province, China.Economic Geology, 92(7-8):827-835.doi: 10.2113/gsecongeo.92.7-8.827 Stein, H.J., Markey, R.J., Morgan, J.W., et al., 2001.The Remarkable Re-Os Chronometer in Molybdenite: How and Why It Works.Terra Nova, 13(6):479-486.doi: 10.1046/j.1365-3121.2001.00395.x Stein, H.J., Sundblad, K., Markey, R.J., et al., 1998.Re-Os Ages for Archean Molybdenite and Pyrite, Kuittila-Kivisuo, Finland and Proterozoic Molybdenite, Kabeliai, Lithuania:Testing the Chronometer in a Metamorphic and Metasomatic Setting.Mineralium Deposita, 33(4):329-345.doi: 10.1007/s001260050153 Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes.Geological Society, London, Special Publications, 42(1):313-345.doi: 10.1144/gsl.sp.1989.042.01.19 Suzuki, K., Shimizu, H., Masuda, A., 1996.Re-Os Dating of Molybdenites from Ore Deposits in Japan:Implication for the Closure Temperature of the Re-Os System for Molybdenite and the Cooling History of Molybdenum Ore Deposits.Geochimica et Cosmochimica Acta, 60(16):3151-3159.doi: 10.1016/0016-7037(96)00164-0 Tang, Y.W., Xie, Y.L., Li, Y.X., et al., 2013.LA-ICP-MS U-Pb Ages, Geochemical Characteristics of the Zircons from Wushanguan Complex Body in Anji Mining Area, Northwestern Zhejiang and Their Geological Significances.Geological Review, 59(4):702-715(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP201304013.htm Tang, Z.C., Chen, Z.D., Hu, W.J., et al., 2016.Geochronology and Geochemistry of Mesozoic Intrusive Rocks in the Yuhang-Lin'an-Fuyang Region, West Zhejiang and Their Geological Significance.Acta Geologica Sinica, 90(3):451-467 (in Chinese with English abstract). https://www.researchgate.net/profile/Zhiwei_Bao/citations?sorting=citationCount&page=1 Tang, Z.C., Dong, X.F., Hu, W.J., et al., 2014.SHRIMP Zircon U-Pb Dating of Xianlin Granodiorite Rock in Western Zhejiang and Their Geological Significance.Geoscience, 28(5):884-892 (in Chinese with English abstract). doi: 10.1080/00206814.2017.1317220 Wang, J.G., Wang, L.W., Chen, X.Y., et al., 2010.SHRIMP U-Pb Ages of Zircons from Kailingjiao and Lichenjia Granodiorites in Western Zhejiang and Their Geological Implications.Geology in China, 37(6):1559-1565(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI201006003.htm Wang, Y.B., Zeng, Q.D., Qu, W.J., 2013.Three Metallogenic Periods of Molybdenum-Polymetallic in Zhejiang Province and Their Geological Significance.Acta Mineralogica Sinica, 34(Suppl.2):55-56 (in Chinese). https://www.researchgate.net/publication/303186376_Re-Os_Isotopic_Dating_of_Molybdenite_from_the_Shankou_Molybdenum_Deposit_in_Yongding_County_of_Fujian_Province_and_Its_Geological_Significance Watanabe, Y., Stein, H.J., 2000.Re-Os Ages for the Erdenet and Tsagaan Suvarga Porphyry Cu-Mo Deposits, Mongolia, and Tectonic Implications.Economic Geology, 95(7):1537-1542.doi: 10.2113/gsecongeo.95.7.1537 Wu, F.Y., Ji, W.Q., Sun, D.H., et al., 2012.Zircon U-Pb Geochronology and Hf Isotopic Compositions of the Mesozoic Granites in Southern Anhui Province, China.Lithos, 150:6-25.doi: 10.1016/j.lithos.2012.03.020 Wu, R.X., Zheng, Y.F., Wu, Y.B., 2007.Zircon U-Pb Age and Isotope Geochemistry of Neoproterozoic Jingtan Volcanics in South Anhui.Geological Journal of China Universities, 13(2):282-296 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200702011.htm Wu, Y.B., Zheng, Y.F., 2004.Genesis of Zircon and Its Constraint on Interpretation of U-Pb Age.Chinese Science Bulletin, 49(16):1589-1604(in Chinese). doi: 10.1007/BF03184122 Xiang, X.K., Wang, P., Sun, D.M., et al., 2013.Re-Os Isotopic Age of Molybdeinte from the Shimensi Tungsten Polymetallic Deposit in Northern Jiangxi Province and Its Geological Implications.Geological Bulletin of China, 32(11):1824-1831(in Chinese with English abstract). https://www.researchgate.net/publication/284701621_Re-Os_isotopic_dating_of_molybdenite_from_the_Dahutang_tungsten_deposit_in_northwestern_Jiangxi_Province_and_its_geological_implication Xie, Y.L., Tang, Y.W., Li, Y.X., et al., 2012a.Magmatic Intrusive Series and Their Implication for the Ore Prospecting in Anji Exploration Area, Zhejiang Province.Acta Petrologica Sinica, 28(10):3334-3346(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201210022.htm Xie, Y.L., Tang, Y.W., Li, Y.X., et al., 2012b.Petrochemistry, Chronology and Ore-Forming Geological Significance of Fine Crystalline Granite in Anji Polymetallic Deposit of Zhejiang Province.Mineral Deposits, 31(4):891-902(in Chinese with English abstract). http://www.sciencedirect.com/science/article/pii/S1367912017300639 Xing, G.F., Lu, Q.D., Chen, R., et al., 2008.Study on the Ending Time of Late Mesozoic Tectonic Regime Transition in South China—Comparing to the Yanshan Area in North China.Acta Geologica Sinica, 82(4):451-463(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZXE200804003.htm Zhang, J.F., Wang, L.W., Chen, J.H., et al., 2015.Genesis of Highly Fractionated Ma'anshan Rock in Zhejiang and Anhui Provinces Constrained by U-Pb Zircon Geochronology and Geochemistry.Earth Science, 40(1):98-114 (in Chinese with English abstract). https://www.researchgate.net/publication/281720370_Genesis_of_highly_fractionated_Ma'anshan_rock_in_Zhejiang_and_Anhui_Provinces_constrained_by_U-Pb_zircon_geochronology_and_geochemistry Zhang, S.M., Xiao, Y.F., Wang, Q., et al., 2013.Re-Os Dating of Molybdenite from the Tongcun Porphyry Molybdenum Deposit in Western Zhejiang Province and Its Geological Implications.Geology and Exploration, 49(1):50-57 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKT201301007.htm Zhang, Y.Q., Xu, X.B., Jia, D., et al., 2009.Deformation Record of the Change from Indosinian Collision-Related Tectonic System to Yanshanian Subduction-Related Tectonic System in South China during the Early Mesozoic.Earth Science Frontiers, 16(1):234-247 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200901033.htm Zhao, H.L., Di, Y.J., Deng, J.F., et al., 2007. A Comparison of Yanshanian Granitoids between the Zhejiang-Jiangxi-Anhui Border Area and the Dexing and Tongling Mineralization Concentated Areas, with a Discussion on Mineralization.Acta Petrologica et Mineralogica, 26(1):13-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW200701002.htm Zhou, X., Yu, X.Q., Wang, D.E., et al., 2011.Characteristics and Geochronology of the W, Mo-Bearing Granodiorite Porphyry in Dongyuan, Southern Anhui.Geoscience, 25(2):201-210(in Chinese with English abstract). https://www.researchgate.net/publication/290852126_Characteristics_and_geochronology_of_the_W_Mo-bearing_granodiorite_porphyry_in_Dongyuan_southern_Anhui Zhou, X., Yu, X.Q., Yang, H.M., et al., 2012.Petrogenesis and Geochronology of the High Ba-Sr Kaobeijian Granodiorite Porphyry, Jixi County, South Anhui Province.Acta Petrologica Sinica, 28(10):3403-3417 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201210027.htm Zhou, X.M., Sun, T., Shen, W.Z., et al., 2006.Petrogenesis of Mesozoic Granitoids and Volcanic Rocks in South China:A Response to Tectonic.Episodes, 29(1):26-33. https://www.researchgate.net/publication/38440799_Petrogenesis_of_Mesozoic_granitoids_and_volcanic_rocks_in_South_China_A_Response_to_Tectonic_Evolution 丁昕, 蒋少涌, 倪培, 等, 2005.江西武山和永平铜矿含矿花岗质岩体锆石SIMS U-Pb年代学.高校地质学报, 11(3): 383-389. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200503009.htm 杜安道, 何红蓼, 殷宁万, 等, 1994.辉钼矿的铼-锇同位素地质年龄测定方法研究.地质学报, 68(4): 339-347. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199404003.htm 顾明光, 冯立新, 胡艳华, 等, 2011.浙江绍兴地区广山-栅溪岩体LA-ICP-MS锆石U-Pb定年:对漓渚铁矿成矿时代的限定.地质通报, 30(8): 1212-1219. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201108005.htm 何国锦, 杨晓春, 吴光明, 等, 2011.浙江西北银山银铅锌多金属矿床矿石矿物特征及成矿期次初步研究.地球学报, 32(3): 304-312. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201103007.htm 胡逸洲, 厉子龙, 毛建仁, 等, 2013.浙西北淳安银山地区银铅锌矿床矿石结构构造、矿石成分及成矿机制.岩石学报, 29(10): 3623-3636. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201310024.htm 华仁民, 陈培荣, 张文兰, 等, 2003.华南中、新生代与花岗岩类有关的成矿系统.中国科学(D辑), 33(4): 335-343. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200304005.htm 华仁民, 陈培荣, 张文兰, 等, 2005.论华南地区中生代3次大规模成矿作用.矿床地质, 24(2): 99-107. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200502001.htm 黄安杰, 温祖高, 刘善宝, 等, 2013.江西乐平塔前钨钼矿中辉钼矿Re-Os定年及其地质意义.岩石矿物学杂志, 32(4): 496-504. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201304007.htm 黄兰椿, 蒋少涌, 2012.江西大湖塘钨矿床似斑状白云母花岗岩锆石U-Pb年代学、地球化学及成因研究.岩石学报, 28(12): 3887-3900. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201212008.htm 简平, 刘敦一, 孙晓猛, 2003.滇川西部金沙江石炭纪蛇绿岩SHRIMP测年:古特提斯洋壳演化的同位素年代学制约.地质学报, 77(2): 217-228. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200302017.htm 李福林, 谢瑜, 周汉文, 等, 2011a.浙江淳安早白垩世脉岩地球化学特征及成岩动力学背景.矿物岩石, 31(3): 55-65. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS201103009.htm 李福林, 周汉文, 唐增才, 等, 2011b.浙江淳安木瓜基性岩墙群U-Pb年龄、地球化学特征及意义.地球化学, 40(1): 22-34. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX201101003.htm 李双, 杨晓勇, 孙卫东, 2012.皖南歙县邓家坞钼矿床年代学及Hf同位素地球化学研究.岩石学报, 28(12): 3980-3992. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201212015.htm 李双, 杨晓勇, 孙卫东, 等, 2014.皖南泾县榔桥岩体锆石U-Pb定年、Hf同位素和地球化学特征及其找矿指示意义.地质学报, 88(8): 1561-1578. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201408017.htm 李晓峰, Yasushi, W., 屈文俊, 2007.江西永平铜矿花岗质岩石的岩石结构、地球化学特征及其成矿意义.岩石学报, 23(10): 2353-2365. doi: 10.3969/j.issn.1000-0569.2007.10.004 李艳军, 魏俊浩, 伍刚, 等, 2011.浙西南毛断铅锌多金属矿床辉钼矿Re-Os年代学及地质意义.地球科学, 36(2): 289-298. http://earth-science.net/WebPage/Article.aspx?id=2092 厉子龙, 周静, 毛建仁, 等, 2013.浙西北木瓜燕山期花岗斑岩的定年、地球化学特征及其地质意义.岩石学报, 29(10): 3607-3622. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201310023.htm 刘善宝, 王成辉, 刘战庆, 等, 2014.赣东北塔前-赋春成矿带岩浆岩时代限定与序列划分及其意义.岩矿测试, 33(4): 598-611. http://www.cnki.com.cn/Article/CJFDTOTAL-YKCS201404024.htm 毛建仁, 高桥浩, 厉子龙, 等, 2009.中国东南部与日本中-新生代构造-岩浆作用对比研究.地质通报, 28(7): 844-856. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200907006.htm 毛景文, 陈懋弘, 袁顺达, 等, 2011.华南地区钦杭成矿带地质特征和矿床时空分布规律.地质学报, 85(5): 636-658. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201105006.htm 秦燕, 王登红, 吴礼彬, 等, 2010.安徽东源钨矿含矿斑岩中的锆石SHRIMP U-Pb年龄及其地质意义.地质学报, 84(4): 479-484. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201004003.htm 邱骏挺, 余心起, 张德会, 等, 2011.浙西开化地区桐村花岗斑岩LA-ICP-MS锆石U-Pb年龄及其地质意义.地质通报, 30(9): 1360-1368. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201109004.htm 宋彪, 张玉海, 万渝生, 等, 2002.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论.地质论评, 48(S1): 26-30. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP2002S1006.htm 唐燕文, 谢玉玲, 李应栩, 等, 2013.浙江安吉多金属矿区坞山关杂岩体锆石LA-ICP-MS U-Pb年龄、地球化学特征及地质意义.地质论评, 59(4): 702-715. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201304013.htm 唐增才, 陈忠大, 胡文杰, 等, 2016.浙西余杭、临安和富阳交界区中生代侵入岩年代学、地球化学特征及其地质意义.地质学报, 90(3): 451-467. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201603003.htm 唐增才, 董学发, 胡文杰, 等, 2014.浙西闲林岩体的锆石SHRIMP U-Pb定年及其地质意义.现代地质, 28(5): 884-892. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201405002.htm 汪建国, 汪隆武, 陈小友, 等, 2010.浙西开岭脚和里陈家花岗闪长岩锆石SHRIMP U-Pb年龄及其地质意义.中国地质, 37(6): 1559-1565. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201006003.htm 王永彬, 曾庆栋, 屈文俊, 2013.浙江省三期钼多金属矿化年龄及其地质意义.矿物学报, 33(S2): 55-56. http://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2013S2031.htm 吴荣新, 郑永飞, 吴元保, 2007.皖南新元古代井潭组火山岩锆石U-Pb定年和同位素地球化学研究.高校地质学报, 13 (2) : 282-296. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200702011.htm 吴元保, 郑永飞, 2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报, 49(16): 1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002 项新葵, 王朋, 孙德明, 等, 2013.赣北石门寺钨多金属矿床辉钼矿Re-Os同位素年龄及其地质意义.地质通报, 32(11): 1824-1831. doi: 10.3969/j.issn.1671-2552.2013.11.015 谢玉玲, 唐燕文, 李应栩, 等, 2012a.浙江安吉铅锌多金属矿床岩浆侵位序列与成矿控制.岩石学报, 28(10): 3334-3346. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201210022.htm 谢玉玲, 唐燕文, 李应栩, 等, 2012b.浙江安吉铅锌多金属矿区细粒花岗岩的岩石化学、年代学及成矿意义探讨.矿床地质, 31(4): 891-902. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201204018.htm 邢光福, 卢清地, 陈荣, 等, 2008.华南晚中生代构造体制转折结束时限研究——兼与华北燕山地区对比.地质学报, 82(4): 451-463. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200804003.htm 张建芳, 汪隆武, 陈津华, 等, 2015.锆石U-Pb年代学和地球化学对浙皖马鞍山高分异岩体成因的约束.地球科学, 40(1): 98-114. http://earth-science.net/WebPage/Article.aspx?id=3023 张世铭, 肖渊甫, 王强, 等, 2013.浙江省桐村钼矿床Re-Os同位素年龄及地质意义.地质与勘探, 49(1) : 50-57. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201301007.htm 张岳桥, 徐先兵, 贾东, 等, 2009.华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录.地学前缘, 16(1): 234-247. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200901033.htm 赵海玲, 狄永军, 邓晋福, 等, 2007.浙赣皖相邻区与德兴、铜陵矿集区燕山期花岗岩类岩石对比研究及其成矿.岩石矿物学杂志, 26(1): 13-20. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200701002.htm 周翔, 余心起, 王德恩, 等, 2011.皖南东源含W、Mo花岗闪长斑岩及成矿年代学研究.现代地质, 25(2): 201-210. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201102003.htm 周翔, 余心起, 杨赫鸣, 等, 2012.皖南绩溪县靠背尖高Ba-Sr花岗闪长斑岩年代学及其成因.岩石学报, 28(10): 3403-3417. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201210027.htm -
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