Zircon U-Pb geochronological and Hf isotopic constraints on petrogenesis of Tieshan and Jinshandian plutons in the southeastern Hubei Province
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摘要:
长江中下游是中国东部中生代大规模成矿的重要地区之一，是我国东部一个重要的Cu-Fe-Au-Mo多金属成矿区带。本文以鄂东南地区铁山岩体和金山店岩体为研究对像，利用原位LA-ICP-MS锆石U-Pb测年和锆石Hf同位素分析方法，探讨该地区岩体成因以及岩浆作用与成矿作用。铁山石英闪长岩LA-ICP-MS锆石U-Pb年龄加权平均值为138.9±0.96Ma(样品jls1-110)、138.2±0.94Ma(样品jls3)、131.0±1.2Ma(样品jls4)和118.9±1.2Ma(样品jls5)，金山店石英闪长岩LA-ICP-MS锆石U-Pb年龄加权平均值为128.6±0.88Ma(样品jsd)，为早白垩世、燕山晚期。铁山岩体石英闪长岩εHf(0)为负值，εHf(t)为负值(-17.3707~-8.31555)，一阶段Hf模式年龄(tDM1)平均为1.33Ga，二阶段Hf模式年龄(tDM2)平均为2.03Ga；金山店岩体石英闪长岩εHf(0)为负值，εHf(t)为负值(-7.81135~-3.45982)，一阶段Hf模式年龄(tDM1)平均为1.03Ga，二阶段Hf模式年龄(tDM2)平均为1.56Ga。铁山和金山店石英闪长岩样品中锆石Hf同位素组成特征显示该地区为岩体形成时有壳源物质参加的这一可能性，为长江中下游壳源岩浆提供补充。在结合已有的岩石学、地球化学以及矿床同位素年龄资料基础上，可以推断出鄂东南地区早白垩世矽卡岩型铁矿床形成于岩石圈伸展-减薄环境。
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关键词:
- LA-ICP-MS锆石U-Pb测年 /
- 锆石Hf同位素分析 /
- 矽卡岩型铁矿床 /
- 晚中生代 /
- 鄂东南地区
Abstract:During the Late Mesozoic, extensive magmatism and associated ore deposits were developed in the Middle-Lower Yangtze River metallogenic belt, East China. As the Tieshan and Jinshandian quartz diorite in the southeastern Hubei Province examples, we performed in situ zircon U-Pb dating and Hf isotopic analyses on 5 samples. Twenty-six zircons in the quartz diorite from the Tieshan sample jls1-110 yield excellent concordant results with a weighted mean 206Pb/238U age of 138.9±0.96Ma (n=26, MSWD=0.82). Zircons from Tieshan sample jls3 yield excellent concordant results with a weighted mean 206Pb/238U age of 138.2±0.94Ma (n=24, MSWD=0.85). Zircons from Tieshan sample jls4 yield excellent concordant results with a weighted mean 206Pb/238U age of 131.0±1.2Ma (n=11, MSWD=0.94). Zircons from Tieshan sample jls5 yield excellent concordant results with a weighted mean 206Pb/238U age of 118.9±1.2Ma (n=14, MSWD=1.20). Zircons from Jinshandian sample jsd yield excellent concordant results with a weighted mean 206Pb/238U age of 128.6±0.88Ma (n=22, MSWD=0.98). εHf(0) and εHf(t) values of the Tieshan quartz diorite are minus. Hf model age of the first stage (tDM1) is 1.33Ga and the age of the second stage (tDM2) is 2.03Ga. εHf(0) and εHf(t) values of the Jinshandina quartz diorite are minus. Hf model age of the first stage (tDM1) is 1.03Ga and the age of the second stage (tDM2) is 1.56Ga. Hf isotopic compositions from the Tieshan and Jinshandian quartz diorites show that maybe the curst-derived materials joined in the rock body forming supplement for the crust-derived magma of the Middle-Lower Yangtze River. Based on the datum of petrology, geochemistry and ore isotope ages, we can infer that the skarn type iron deposits of the Early Cretaceous in the southeastern Hubei Province formed on the environment of lithospheric extending and thinning.
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Key words:
- Zircon U-Pb dating /
- Hf isotopes /
- Skarn type iron deposit /
- Late Mesozoic /
- southeastern Hubei Province
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图 1
扬子板块东部七大岩浆源区示意图(据Mao et al.，2011)
Figure 1.
Schematic illustration of the seven magmatic regions from the eastern Yangtze craton(after Mao et al.，2011)
图 2
鄂东南地区地质图以及岩体年龄(据舒全安等，1992)
Figure 2.
Geological map and pluton ages from the southeastern Hubei Province(after Shu et al.，1992)
图 3
鄂东南地区铁山和金山店石英闪长岩锆石阴极发光(CL)图像
Figure 3.
Characteristics of zircon shape and LA-ICP-MS testing data for the Tieshan and Jinshandian quartz diorites
图 4
鄂东南地区铁山样品jls1-110石英闪长岩LA-ICP-MS 锆石U-Pb一致曲线图
Figure 4.
U-Pb concordia diagrams showing LA-ICP-MS data of sample jls1-110 for the Tieshan quartz diorite
图 5
鄂东南地区铁山样品jls3石英闪长岩LA-ICP-MS 锆石U-Pb一致曲线图
Figure 5.
U-Pb concordia diagrams showing LA-ICP-MS data of sample jls3 for the Tieshan quartz diorite
图 6
鄂东南地区铁山样品jls4石英闪长岩LA-ICP-MS 锆石U-Pb一致曲线图
Figure 6.
U-Pb concordia diagrams showing LA-ICP-MS data of sample jls4 for the Tieshan quartz diorite
图 7
鄂东南地区铁山样品jls5石英闪长岩LA-ICP-MS 锆石U-Pb一致曲线图
Figure 7.
U-Pb concordia diagrams showing LA-ICP-MS data of sample jls5 for the Tieshan quartz diorite
图 8
鄂东南地区金山店样品jsd石英闪长岩LA-ICP-MS 锆石U-Pb一致曲线图
Figure 8.
U-Pb concordia diagrams showing LA-ICP-MS data of sample jsd for the Jinshandian quartz diorite
表 1
鄂东南地区铁山和金山店石英闪上岩LA-ICP-MS锆石U-Pb年龄测定结果
Table 1.
Zircon U-Pb dating ages for the Tieshan and Jinshandian quartz diorites in the southeastern Hubei Province
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表 2
鄂东南地区铁山和金山店石英闪长岩Hf同位素分析结果
Table 2.
Summary of Hf isotopic and geochemical compositions for the Tieshan and Jinshandian quartz diorites in the southeastern Hubei Province
测点号 
2σ εHf(0) εHf(t) 2σ tDM1
(Ga)tDM2
(Ga)fLu/Hf 
jls1-110-01 0.036848 0.001418 0.282238 0.000028 -18.9 -15.8900 1.003772230 1.45 2.20 -0.95728 0.282234060 jls1-110-02 0.040184 0.001555 0.282299 0.000026 -16.7 -13.8101 0.909537029 1.36 2.07 -0.95317 0.282295339 jls1-110-03 0.038128 0.001422 0.282197 0.000021 -20.3 -17.3707 0.760098748 1.50 2.29 -0.95717 0.282193444 jls1-110-04 0.031337 0.001233 0.282225 0.000019 -19.3 -16.4161 0.668997882 1.46 2.23 -0.96287 0.282221671 jls1-110-05 0.039348 0.001602 0.282232 0.000016 -19.1 -16.1595 0.579526810 1.46 2.22 -0.95174 0.282228304 jls1-110-06 0.033919 0.001260 0.282251 0.000019 -18.4 -15.4429 0.686611811 1.42 2.17 -0.96203 0.282247318 jls1-110-07 0.025635 0.000874 0.282266 0.000017 -17.9 -14.8062 0.593726359 1.39 2.14 -0.97368 0.282264076 jls1-110-08 0.028194 0.001078 0.282207 0.000020 -20.0 -17.0388 0.690833364 1.48 2.27 -0.96754 0.282204687 jls1-110-09 0.020768 0.000829 0.282279 0.000026 -17.4 -14.3860 0.929072268 1.37 2.11 -0.97502 0.282277197 jls1-110-10 0.034524 0.001334 0.282310 0.000027 -16.3 -13.3770 0.961960777 1.34 2.04 -0.95981 0.282306340 jls1-110-11 0.028645 0.001163 0.282307 0.000028 -16.4 -13.5261 0.994828069 1.34 2.05 -0.96498 0.282303986 jls1-110-12 0.033720 0.001338 0.282248 0.000026 -18.5 -15.6241 0.906947343 1.43 2.18 -0.95970 0.282244679 jls1-110-13 0.040410 0.001631 0.282235 0.000020 -19.0 -16.1221 0.692078751 1.46 2.21 -0.95087 0.282230601 jls1-110-14 0.017804 0.000720 0.282241 0.000016 -18.8 -15.805 0.578711323 1.42 2.20 -0.97830 0.282238946 jls1-110-15 0.078289 0.003033 0.282304 0.000027 -16.6 -13.8244 0.949566110 1.41 2.07 -0.90863 0.282296175 jls1-110-16 0.025138 0.001005 0.282261 0.000016 -18.1 -15.1191 0.560429010 1.40 2.15 -0.96973 0.282258333 jls1-110-17 0.020891 0.000870 0.282268 0.000019 -17.8 -14.8957 0.666010052 1.38 2.14 -0.97379 0.282265271 jls1-110-18 0.048317 0.001897 0.282251 0.000018 -18.4 -15.6017 0.631875064 1.45 2.18 -0.94287 0.282245932 jls1-110-19 0.016014 0.000663 0.282248 0.000016 -18.5 -15.5884 0.551636271 1.40 2.18 -0.98002 0.282246309 jls1-110-20 0.032131 0.001280 0.282270 0.000018 -17.7 -14.8199 0.626329027 1.40 2.13 -0.96145 0.282266793 jls-1-110-21 0.052618 0.001976 0.282240 0.000022 -18.8 -15.9265 0.762948906 1.46 2.20 -0.94049 0.282234891 jls1-110-22 0.083001 0.002940 0.282219 0.000020 -19.6 -16.7988 0.722722313 1.54 2.26 -0.91145 0.282211472 jls1-110-24 0.017319 0.000627 0.282225 0.000018 -19.4 -16.3941 0.644622998 1.44 2.23 -0.98111 0.282222912 jls1-110-25 0.021427 0.000943 0.282273 0.000021 -17.6 -14.7404 0.733044361 1.38 2.13 -0.97160 0.282270900 jls1-110-26 0.022160 0.000976 0.282216 0.000026 -19.7 -16.7726 0.933556536 1.46 2.25 -0.97060 0.282213453 jls3-01 0.020529 0.000753 0.282374 0.000020 -14.1 -11.0484 0.692728278 1.23 1.90 -0.97733 0.282371544 jls3-02 0.017467 0.000652 0.282372 0.000018 -14.2 -11.1542 0.620431616 1.23 1.90 -0.98036 0.282369795 jls3-03 0.009996 0.000402 0.282355 0.000017 -14.7 -11.6718 0.593795797 1.25 1.94 -0.98789 0.282353921 jls3-04 0.030182 0.001119 0.282370 0.000020 -14.2 -11.2253 0.717276779 1.25 1.91 -0.96629 0.282367165 jls3-05 0.014749 0.000548 0.282408 0.000021 -12.9 -9.78444 0.741159122 1.18 1.82 -0.98349 0.282406654 jls3-06 0.014261 0.000585 0.282410 0.000021 -12.8 -9.82895 0.727607640 1.18 1.82 -0.98237 0.282408500 jls3-07 0.023261 0.000940 0.282339 0.000018 -15.3 -12.4054 0.649764801 1.29 1.98 -0.97170 0.282336288 jls3-08 0.017108 0.000714 0.282337 0.000020 -15.4 -12.4683 0.693118761 1.28 1.98 -0.97848 0.282335131 jls3-09 0.008944 0.000361 0.282368 0.000017 -14.3 -11.2605 0.602878848 1.23 1.91 -0.98913 0.282366789 jls3-10 0.015478 0.000628 0.282382 0.000018 -13.8 -10.8730 0.636363588 1.22 1.88 -0.98108 0.282380229 jls3-12 0.008122 0.000342 0.282343 0.000019 -15.2 -12.2522 0.658545572 1.26 1.97 -0.98970 0.282341861 jls3-13 0.015653 0.000609 0.282455 0.000017 -11.2 -8.31555 0.618953082 1.12 1.72 -0.98165 0.282453145 jls3-14 0.015297 0.000659 0.282356 0.000018 -14.7 -11.7124 0.620574404 1.25 1.94 -0.98016 0.282354636 jls3-15 0.007291 0.000300 0.282385 0.000016 -13.7 -10.7260 0.558518019 1.20 1.87 -0.99095 0.282383763 jls3-16 0.010358 0.000430 0.282371 0.000017 -14.2 -11.2427 0.585958928 1.23 1.91 -0.98706 0.282369778 jls3-17 0.014136 0.000571 0.282382 0.000015 -13.8 -10.8176 0.536064153 1.23 1.88 -0.98281 0.282380551 jls3-18 0.030243 0.001085 0.282352 0.000019 -14.9 -11.8975 0.681280607 1.27 1.95 -0.96730 0.282348785 jls3-19 0.016521 0.000582 0.282404 0.000019 -13.0 -10.1078 0.657889545 1.19 1.83 -0.98247 0.282402481 jls3-20 0.052815 0.001897 0.282386 0.000019 -13.6 -10.7475 0.662473258 1.25 1.88 -0.94286 0.282381292 jls3-21 0.006750 0.000248 0.282358 0.000018 -14.6 -11.6226 0.654219131 1.24 1.93 -0.99253 0.282357797 jls3-22 0.003556 0.000145 0.282356 0.000015 -14.7 -11.6693 0.527453000 1.24 1.94 -0.99562 0.282355235 jls3-23 0.021421 0.000852 0.282372 0.000019 -14.2 -11.2082 0.682000890 1.24 1.90 -0.97435 0.282369512 jls3-24 0.023351 0.000896 0.282352 0.000020 -14.8 -11.8609 0.690460101 1.27 1.95 -0.97302 0.282349817 jls3-25 0.015110 0.000612 0.282399 0.000020 -13.2 -10.1638 0.700368923 1.19 1.84 -0.98157 0.282397792 jls-4-04 0.021475 0.000498 0.282348 0.000046 -15.0 -12.2278 1.639843631 1.26 1.96 -0.98501 0.282346893 jls-4-05 0.019334 0.000586 0.282227 0.000040 -19.3 -16.4595 1.417379473 1.43 2.23 -0.98235 0.282225405 jls-4-07 0.051187 0.001485 0.282362 0.000041 -14.5 -11.7304 1.441985526 1.27 1.93 -0.95527 0.282357852 jls-4-13 0.086738 0.002557 0.282227 0.000043 -19.3 -16.7146 1.513983052 1.51 2.24 -0.92299 0.282220675 jls5-01 0.049520 0.000971 0.282431 0.000029 -12.0 -9.53336 1.024251836 1.16 1.78 -0.97074 0.282429271 jls5-05 0.035502 0.000766 0.282345 0.000021 -15.1 -12.4588 0.728797190 1.27 1.97 -0.97694 0.282342845 jls5-07 0.060148 0.001738 0.282379 0.000026 -13.9 -11.4750 0.928837058 1.26 1.91 -0.94764 0.282375001 jls5-10 0.098264 0.002408 0.282362 0.000030 -14.5 -12.0353 1.046960323 1.31 1.94 -0.92747 0.282356058 jls5-12 0.042758 0.001286 0.282326 0.000025 -15.8 -13.2387 0.898081910 1.32 2.02 -0.96125 0.282323281 jls5-13 0.004880 0.000172 0.282381 0.000017 -13.8 -11.2046 0.584978383 1.20 1.89 -0.99482 0.282380784 jls5-14 0.104018 0.003487 0.282252 0.000043 -18.4 -16.0546 1.507035127 1.51 2.19 -0.89498 0.282244296 jls5-15 0.031585 0.001087 0.282375 0.000038 -14.0 -11.5479 1.331265890 1.24 1.91 -0.96725 0.282372939 jls5-17 0.126953 0.003165 0.282177 0.000034 -21.0 -18.6515 1.210390660 1.61 2.36 -0.90467 0.282169643 jls5-18 0.012946 0.000487 0.282369 0.000024 -14.3 -11.7103 0.857485304 1.23 1.92 -0.98532 0.282367730 jls5-19 0.069351 0.002170 0.282411 0.000038 -12.8 -10.336 1.361415896 1.23 1.83 -0.93463 0.282405959 jls5-21 0.043273 0.001047 0.282301 0.000024 -16.7 -14.1377 0.838970801 1.34 2.08 -0.96845 0.282298485 jls5-22 0.054582 0.001357 0.282312 0.000030 -16.3 -13.7862 1.055086299 1.34 2.05 -0.95914 0.282309043 jls5-24 0.028994 0.000864 0.282373 0.000036 -14.1 -11.5753 1.275746983 1.24 1.91 -0.97397 0.282370924 jsd-01 0.024148 0.000723 0.282476 0.000024 -10.5 -7.76231 0.844596512 1.09 1.68 -0.97822 0.282474372 jsd-02 0.024087 0.000752 0.282567 0.000021 -7.20 -4.51838 0.755266780 0.96 1.47 -0.97734 0.282565455 jsd-03 0.037138 0.001181 0.282560 0.000022 -7.50 -4.80546 0.785460906 0.98 1.49 -0.96443 0.282556718 jsd-04 0.036671 0.001120 0.282564 0.000020 -7.40 -4.67469 0.694765948 0.98 1.48 -0.96627 0.282561036 jsd-05 0.033885 0.001135 0.282564 0.000021 -7.30 -4.58857 0.739809065 0.98 1.48 -0.96580 0.282561608 jsd-06 0.068672 0.002529 0.282493 0.000036 -9.90 -7.21926 1.280218992 1.12 1.65 -0.92383 0.282486619 jsd-07 0.025181 0.000808 0.282576 0.000029 -6.90 -4.13102 1.033098457 0.95 1.45 -0.97567 0.282573921 jsd-08 0.017534 0.000580 0.282556 0.000025 -7.60 -4.83246 0.900201634 0.97 1.49 -0.98252 0.282554713 jsd-09 0.027726 0.000868 0.282597 0.000018 -6.20 -3.45982 0.624907938 0.92 1.40 -0.97384 0.282595380 jsd-10 0.034929 0.001265 0.282547 0.000021 -7.90 -5.26351 0.737820371 1.00 1.52 -0.96189 0.282544391 jsd-12 0.043001 0.001632 0.282506 0.000026 -9.40 -6.65041 0.910502172 1.074 1.61 -0.95084 0.282501458 jsd-13 0.021361 0.000693 0.282494 0.000020 -9.80 -6.95783 0.720021763 1.06 1.63 -0.97912 0.282492768 jsd-14 0.032287 0.001135 0.282510 0.000020 -9.30 -6.56144 0.692864362 1.05 1.60 -0.96581 0.282507078 jsd-15 0.041032 0.001444 0.282511 0.000017 -9.20 -6.52332 0.583912729 1.06 1.60 -0.95651 0.282507535 jsd-16 0.045046 0.001615 0.282525 0.000021 -8.70 -6.07706 0.746477226 1.05 1.57 -0.95134 0.282521392 jsd-17 0.034825 0.001381 0.282527 0.000022 -8.70 -5.98516 0.777885960 1.04 1.56 -0.95841 0.282523990 jsd-18 0.032950 0.001195 0.282485 0.000020 -10.1 -7.45880 0.711829921 1.09 1.66 -0.96399 0.282482331 jsd-19 0.026804 0.001021 0.282491 0.000024 -9.90 -7.21456 0.833901958 1.08 1.64 -0.96925 0.282488615 jsd-20 0.027609 0.001018 0.282501 0.000030 -9.60 -6.90765 1.071177134 1.06 1.62 -0.96934 0.282498533 jsd-21 0.037789 0.001332 0.282518 0.000021 -9.00 -6.25129 0.736340743 1.05 1.58 -0.95988 0.282515225 jsd-22 0.020047 0.000670 0.282536 0.000021 -8.30 -5.59833 0.741224955 1.00 1.54 -0.97983 0.282534304 jsd-23 0.011934 0.000464 0.282473 0.000026 -10.6 -7.81135 0.921123743 1.09 1.68 -0.98602 0.282471744
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表 3
鄂东南地区岩浆岩锆石U-Pb年龄
Table 3.
Zircon U-Pb ages for magmas from the southeastern Hubei Province
岩体名称 岩性 测试方法 年龄(Ma) 资料来源 灵乡 石英闪长岩 SHRIMP锆石U-Pb 141.1±0.7 Li et al.，2009 鄂城 石英闪长岩 SHRIMP锆石U-Pb 143.0±2.0 Xie et al.，2011a 花岗岩 SHRIMP锆石U-Pb 130.0±1.0~127.0±1.0 程潮 石英闪长岩 SHRIMP锆石U-Pb 129.0±2.0 金山店 石英闪长岩 SHRIMP锆石U-Pb 127.0±2.0 谢桂青，2009 花岗岩 SHRIMP锆石U-Pb 133.0±1.0 王保山 闪长岩 SHRIMP锆石U-Pb 132.4±1.3 Li et al.，2009 铁山 石英闪长岩 SHRIMP锆石U-Pb 142.0±3.0 Xie et al.，2011a 花岗岩 LA-ICP-MS锆石U-Pb 137.0±2.0 石英闪长岩 SHRIMP锆石U-Pb 135.8±2.4 Li et al.，2009 阳新 石英闪长岩 SHRIMP锆石U-Pb 142.0±2.0 Xie et al.，2011b 花岗斑岩 SHRIMP锆石U-Pb 141.0±2.0 石英闪长岩 SHRIMP锆石U-Pb 139.0±1.0 Li et al.，2009 石英二长闪长岩 SHRIMP锆石U-Pb 138.5±2.5 Li et al.，2010 闪长岩 Cameca SIMS U-Pb 141.0±1.0 丰山洞 花岗闪长斑岩 SHRIMP锆石U-Pb 146.0±2.0 Xie et al.，2007 铜山口 花岗闪长斑岩 Cameca SIMS U-Pb 146.0±1.3 城门山 花岗闪长斑岩 Cameca SIMS U-Pb 144.5±1.2 武山 花岗闪长斑岩 Cameca SIMS U-Pb 146.1±1.0 Xie et al.，2011a 东雷塆 花岗闪长斑岩 Cameca SIMS U-Pb 146.0±1.0 邓家山 花岗闪长斑岩 Cameca SIMS U-Pb 145.4±1.0
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Amelin Y, Lee DC, Halliday AN and Pidgeon RT. 1999. Nature of the Earth’s earliest crust from hafnium isotopes in single detrital zircons. Nature, 399: 252-255 doi: 10.1038/20426
Amelin Y, Lee DC and Halliday AN. 2000. Early-Middle Archean crustal evolution deduced from Lu-Hf and U-Pb isotopic studies of single zircon grains. Geochimica et Cosmochimica Acta, 64: 4205-4225 doi: 10.1016/S0016-7037(00)00493-2
Andersen T. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology, 192: 59-79 doi: 10.1016/S0009-2541(02)00195-X
Chang YF, Liu XP and Wu YC. 1991. Fe-Cu Metallogenic Belt in the Middle-Lower Reaches of the Yangtze River Area. Beijing: Geological Publishing House, 1-379 (in Chinese)
Chen JF, Yan J, Xie Z, Xu X and Xing F. 2001. Nd and Sr isotopic compositions of igneous rocks from the Lower Yangtze region in eastern China: Constraints on sources. Physics and Chemistry of the Earth (A), 26: 719-731 doi: 10.1016/S1464-1895(01)00122-3
Chu N and Taylor RN, Chavagnac V, Nesbitt RW, Boella RM, Milton JA, German CR, Bayon G and Burton K. 2002. Hf isotope ration analysis using multi-collector inductively coupled plasma mass spectrometry: An evaluation of isobaric interference corrections. Journal of Analytical Atomic Spectrometry, 17: 1567-1574 doi: 10.1039/b206707b
Deng JF, Ye DL, Zhao HL and Tang HP. 1992. Volcanism, Deep Internal Processes and Basin Formation in the Lower Reaches of Yangtze River. Wuhan: China University of Geosciences Press, 1-184 (in Chinese)
Deng JF, Mo XX, Zhao HL, Luo ZH, Zhao GC and Dai SQ. 1999. The Yanshanian lithosphere asthemosphere catastrophe and metallogenic environment in East China. Mineral Deposits, 18(4): 309-315 (in Chinese with English abstract)
Deng J, Wang QF, Huang DH and Gao BF. 2004. Structural control of ore-forming fluid activities in shallow crust of Tongling ore concentration area in Yanshanian Period. Mineral Deposits, 23(3): 399-404 (in Chinese with English abstract)
Di YJ, Zhao HL, Zhang YQ, Zhao JH and Yang L. 2003. Petrographic evidences for magma mixing in the granitoids from Tongling area, Anhui Province. Beijing Geology, 15(1): 12-17 (in Chinese with English abstract)
Du YS and Lee HK. 2004. Discovery of gabbroic xenoliths from Early Cretaceous intrusions in Tongling, Anhui Province, China and its geologic significance. Geological Journal of China Universities, 10(3): 332-342 (in Chinese with English abstract)
Du YS, Qin XL and Tian SH. 2004a. Mesozoic magmatic to hydrothermal process in the Tongguanshan ore field, Tongling, Anhui Province, China: Evidence from xenoliths and their hosts. Acta Petrologica Sinica, 20(2): 339-350 (in Chinese with English abstract)
Du YS, Qin XL and Lee HK. 2004b. Mesozoic mantle-derived magma underplating in Tongling, Anhui Province: Evidence from megacrysts and zenoliths. Acta Petrologica et Mineralogica, 23(2): 109-116(in Chinese with English abstract)
Du YS, Li ST, Cao Y, Qin XL and Lou YE. 2007. Uafc-related origin of the Late Jurassic to Early Cretaceous intrusions in the Tongguanshan ore field, Tongling, Anhui Province, East China. Geoscience, 21(1): 71-77 (in Chinese with English abstract)
Gao S, Liu XM, Yuan HL, Hattendorf B, Gunther D, Chen L and Hu SH. 2002. Analysis of forty-two major and trace elements of USGS and NIST SRM Glasses by LA-ICP-MS. Geostand Newsl, 22: 181-195
Griffin WL, Wang X, Jackson SE, Pearson NJ and O’Reilly SY. 2002. Zircon geochemistry and magma mixing, SE China: In situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes. Lithos, 61: 237-269 doi: 10.1016/S0024-4937(02)00082-8
Grimmer JC, Ratschbacher L and McWilliams M. 2003. When did the ultrahigh-pressure rocks reach the surface? A 207Pb/206Pb zircon, 40Ar/39Ar white mica, Si-in-white mica, single-grain provenance study of Dabie Shan synorogenic foreland sediments. Chemical Geology, 197: 87-110 doi: 10.1016/S0009-2541(02)00321-2
Hou KJ, Li YH, Zou TR, Qu XM, Shi YR and Xie GQ. 2007. Laser ablation-MC-ICP-MS technique for Hf isotope microanalysis of zircon and its geologicl applications. Acta Petrologica Sinica, 23(10): 2595-2604(in Chinese with English abstract)
Iizuka T and Hirata T. 2005. Improvements of precision and accuracy in situ Hf isotope microanalysis of zircon using the laser ablation-MC-ICP-MS technique. Chemical Geology, 220: 121-137 doi: 10.1016/j.chemgeo.2005.03.010
Jahn BM, Wu FY, Lo CH and Tsai CH. 1999. Crust-mantle interaction induced by deep subduction of the continental crust: Geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie complex, central China. Chemical Geology, 157:119-146 doi: 10.1016/S0009-2541(98)00197-1
Li JW, Pei RF and Mei YX. 2004. Vertical zoing of orefield structures in Tongling ore concentration area, Anhui Province. Mineral Deposits, 23(2): 206-215 (in Chinese with English abstract)
Li JW, Pei RF, Zhang DQ, Mei YX, Zang WS, Meng XG, Zeng PS, Li TJ and Di YJ. 2007. Geochemical characteristics of the Yanshanian intermediate-acid intrusive rocks in the Tongling mineralization concentration area, Anhui Province, and their geological implications. Acta Geoscientica Sinica, 28(1): 11-22 (in Chinese with English abstract)
Li JW, Zhao XF, Zhou MF, Vasconcelos, P, Ma CQ, Deng XD, Zhao YX and Wu G. 2008. Origin of the Tongshankou porphyry-skarn Cu-Mo deposit, eastern Yangtze craton, Eastern China: Geochronological, geochemical, and Sr-Nd-Hf isotopic constraints. Mineralium Deposita, 43: 319-336
Li JW, Zhao XF, Zhou MF, Ma CQ, Souza de ZS and Vasconcelos P. 2009. Late Mesozoic magmatism from the Daye region, eastern China: U-Pb ages, petrogenesis, and geodynamic implications. Contributions to Mineralogy and Petrology, 157: 383-409 doi: 10.1007/s00410-008-0341-x
Li JW, Deng XD, Zhou MF, Liu YS, Zhao XF and Guo JL. 2010. Laser ablation ICP-MS titanite U-Th-Pb dating of hydrothermal ore deposits: A case study of the Tonglushan Cu-Fe-Au skarn deposit, SE Hubei Province, China. Chemical Geology, 270: 56-57 doi: 10.1016/j.chemgeo.2009.11.005
Liu LM, Wang ZC and Peng SL. 2002. Application of comprehensive informationism prediction for ore prospecting in deeper and outer of mines with critical reserves: An example from the Fenghuangshan copper mine, Tongling. Chinese Journal of Geology, 37 (4): 444-452(in Chinese with English abstract)
Liu WC, Gao DZ and Chu GZ. 1996. The Analysis of Structure Deformation and the Metallogenic Prediction in the Middle and Lower Yangtze Reachers. Beijing: Geological Publishing House, 1-133 (in Chinese)
Liu XM, Gao S, Yuan HL, Hattendorf B, Günther D, Chen L and Hu SH. 2002. Analysis of 42 major and trace elements in glass standard reference materials by 193nm LA-ICP-MS. Acta Petrologica Sinica, 18(3): 408-418 (in Chinese with English abstract)
Ludwig KR. 1991. Isoplot 2A plotting and regression program for radiogenic isotope data. US Geological Survey Open File Report, 39: 91-445
Ma CQ, Yang KG, Tang ZH and Li ZT. 1994. Magma Dynamics of Granitoids: Theory, Method and a Case Study of the Eastern Hubei Granitoids. Wuhan: Press of China University of Geosciences, 1-260 (in Chinese with English abstract)
Ma CQ, Li ZC, Ehlers C, Yang KG and Wang RJ. 1998. A postcollisional magmatic plumbing system: Mesozoic granitoid plutons from the Dabieshan high-pressure and ultrahigh-pressure metamorphic zone, east-central China. Lithos, 45: 431-456 doi: 10.1016/S0024-4937(98)00043-7
Mao JR, Su YX and Chen SY. 1990. Intermediate-acid Intrusion in the Middle-Lower Reaches of Yangtze River and Relevant Mineralization. Beijing: Geological Publishing House, 1-191 (in Chinese)
Mao JW, Hua RM and Li XB. 1999. A preliminary study of large-scale metallogenesis and large clusters of mineral deposits. Mineral Deposits, 18: 39-43 (in Chinese with English abstract)
Mao JW, Wang YT, Bernd L, Yu JJ, Du AD, Mei YX, Li YF, Zang WS, Holly JS and Zhou TF. 2006. Molybdenite Re-Os and albite 40Ar/39Ar dating of Cu-Au-Mo and magnetite porphyry systems in the Yangtze River Valley and metalogenic implications. Ore Geology Reviews, 29: 307-324 doi: 10.1016/j.oregeorev.2005.11.001
Mao JW, Hu RZ, Chen YC and Wang YT. 2006. Large Scale Ore Forming Events and Large Ore Dense Areas. Beijing: Geological Publishing House, Ⅰ-Ⅶ (in Chinese)
Mao JW, Xie GQ, Duan C, Pirajno F, Ishiyama D and Chen YC. 2011. A tectono-genetic model for porphyry-skarn-stratabound Cu-Au-Mo-Fe and magnetite-apatite deposits along the Middle-Lower Yangtze River Valley, Eastern China. Ore Geology Reviews, 43: 294-314 doi: 10.1016/j.oregeorev.2011.07.010
Mao ZL, Lai JQ, Peng SL, Shao YJ and Yang B. 2004. The chemical characteristics and significances of the Fenghuangshan copper deposit in Tongling, Anhui Province. Geology and Prospecting, 40(2): 28-31 (in Chinese with English abstract)
Nowell GM, Kempton PD, Noble SB, Eitton J, Saunders AD, Maboney JJ and Taylor RN. 1998. High precision Hf isotope measurements of MORB and OIB by thermal ionization mass spectrometry: Insights into the depleted mantle. Chemical Geology, 149: 211-233 doi: 10.1016/S0009-2541(98)00036-9
Pan Y and Dong P. 1999. The Lower Changjiang (Yangzi/Yangtze River) metallogenic belt, East China: Intrusion- and wall rock-hosted Cu-Fe-Au, Mo, Zn, Pb, Ag deposits. Ore Geology Review, 15: 177-242 doi: 10.1016/S0169-1368(99)00022-0
Pei RF. 1995. Model of Mineral Deposits. Beijing: Geological Publishing House, 262-264 (in Chinese)
Pei RF and Hong DW. 1995. The granites of South China and their metallogeny. Episodes, 18: 77-86
Petford N and Gallagher K. 2001. Partial melting of mafic (amphibiotic) lower cruster by periodic influx of basaltic magma. Earth and Planetary Science Letters, 193(3-4): 483-499 doi: 10.1016/S0012-821X(01)00481-2
Shao YJ, Peng SL, Liu LM and Wu GG. 2003a. Analysis of the geological condictions of mineralization and the ore-control factors in Fenghuanshan field. Journal of Central South University of Technology, 34(5): 562-566 (in Chinese with English abstract)
Shao YJ, Peng SL, Wu GG and Zhang D. 2003b. The analysis on the rock-forming mechanism of Fenghuanshan rock body in Tongling area. Geology and Prospecting, 39 (5): 39-43 (in Chinese with English abstract)
Shu QA, Chen PL, Cheng JR et al. 1992. Geology of Iron-Copper Deposits in Eastern Hubei Province, China. Beijing: Metallurgic Industry Press, 1-510 (in Chinese)
Sun WD, Xie Z, Chen J, Zhang X, Chai Z, Du A, Zhao J, Zhang C and Zhou T. 2003. Os-Os dating of copper and molybdenite deposits along the Middle and Lower Reaches of the Yangtze River, China. Economic Geology, 98: 175-180
Tang YC, Wu YC, Chu GZ et al. Geology of Copper-gold Polymetallic Deposits in the along-Changjiang Area of Anhui Province. Beijing: Geological Publishing House, 1998: 1-351 (in Chinese)
Tian SH, Du YS, Qin XL, Lee Hyun-koo, Jin SZ, Yin JW and Li ZX. 2001. Mineral inclusion studies of the intermediate-acid intrusive rocks and their rock enclaves in Tongling area, Anhui Province. Earth Science Frontiers, 8(4): 422-428 (in Chinese with English abstract)
Wang Q, Zhao, ZH, Bao ZW, Xu JF, Liu W, Li CF, Bai, ZH and Xiong XL. 2004. Geochemistry and petrogenesis of the Tongshankou and Yinzu adakitic intrusive rocks and the associated porphyry copper-molybdenum mineralization in southeast Hubei, East China. Resource Geology, 54: 137-152 doi: 10.1111/rge.2004.54.issue-2
Wang Q, Wyman DA, Xu JF, Zhao ZH, Jian P, Xiong XL, Bao ZW, Li CF and Bai ZH. 2006. Petrogenesis of Cretaceous adakitic and shoshonitic igneous rocks in the Luzong area, Anhui Province (eastern China): Implications for geodynamics and Cu-Au mineralization. Lithos, 89: 424-446 doi: 10.1016/j.lithos.2005.12.010
Wang QF, Deng J, Huang DH and Zhang Q. 2004. Prognosis and morhpological analysis of subsurface concealed magmatic bodies in Tongling ore concentration area. Mineral Deposits, 23(3): 405-410 (in Chinese with English abstract)
Wang YL, Zhang Q and Wang Y. 2001. Geochemical characteristics of volcanic rocks from Ningwu area, and its significance. Acta Petrologica Sinica, 17(4):565-575 (in Chinese with English abstract)
Wang YL, Wang Y, Zhang Q, Jia XQ and Han S. 2004. The geochemical characteristics of Mesozoic intermediate-acid intrusives of the Tongling area and its metallogenesis-geodynamic implications. Acta Petrologica Sinica, 20(2): 325-338 (in Chinese with English abstract)
Wen G and Wu SB. 1983. Some characteristics of the Fenghuangshan intrusion and its affinity to mineralization. Bulletin of the Chinese Academy of Geological Sciences, 7: 343-349 (in Chinese with English abstract)
Wu CL, Zhou XR, Huang XC, Zhang CG and Huang WM. 1996. 40Ar/39Ar chronology of intrusive rocks from Tongling. Acta Petrologica et Mineralogica, 5(4): 299-306 (in Chinese with English abstract)
Wu GG, Zhang D and Zang WS. 2003. Study on tectonic layering movement and layering mineralization in the Tongling metallogenic cluster. Science in China (Series D), 33 (4): 300-308 (in Chinese)
Wu FY, Yang JH, Liu XM, Li TS, Xie LW and Yang YH. 2005a. Hf isotopes of the 3.8Ga zircons in eastern Hebei Province, China: Implication for early crustal evolution of the North China Croton. Chinese Science Bulletin, 50: 2473-2480
Wu FY, Lin JQ, Wilde SA, Zhang XO and Yang JH. 2005b. Nature and significance of the Early Cretaceous giant igneous event in eastern China. Earth and Planetary Science Letters, 233: 103-119 doi: 10.1016/j.epsl.2005.02.019
Wu FY, Yang JH, Wilde SA and Zhang XO. 2005c. Geochronology, petrogenesis and tectonic implications of Jurassic granites in the Liaodong Peninsula, NE. China Chemical Geology, 221: 127-156 doi: 10.1016/j.chemgeo.2005.04.010
Wu LS and Zou XQ. 1997. Re-Os isotopic age study on the Chengmenshan Cu deposit in Jiangxi Province. Mineral Deposits, 16: 376-381 (in Chinese with English abstract)
Xie GQ, Mao JW, Li RL, Qu WJ, Pirajno F and Du AD. 2007. Re-Os molybdnite and Ar-Ar phlogopite dating of Cu-Fe-Au-Mo(W) deposits in southeastern Hubei, China. Mineralogy and Petrology, 90: 249-270 doi: 10.1007/s00710-006-0176-y
Xie GQ, Mao JW, Li LR and Beirlein F. 2008. Geochemistry and Nd-Sr isotopic studies of Late Mesozoic granitoids in the southeastern Hubei Province, Middle-Lower Yangtze River belt, Eastern China: Petrogenesis and tectonicsetting. Lithos, 104: 216-230 doi: 10.1016/j.lithos.2007.12.008
Xie GQ, Li RL, Jiang GH, Zhao CS and Hou KJ. 2008. Geochemistry and petrogenesis of Late Mesozoic granitoids in southeastern Hubei Province and constrains on the timing of lithospheric thinning, Middle-Lower Reaches of the Yangtze River, Eastern China. Acta Petrologica Sinica, 24(8): 1703-1714 (in Chinese with English abstract)
Xie GQ. 2009. Geochronology and genesis of Late Mesozoic igneous rocks and its relation to skarn Cu-Fe-Au deposits in southeastern Hubei Province, Middle-Lower Reaches of the Yangtze River, Eastern China. Post-Doctor Research Report. Beijing: China University of Geosciences, 1-183 (in Chinese with English abstract)
Xie GQ, Mao JW and Zhao HJ. 2011a. Zircon U-Pb geochronological and Hf isotopic constraints on petrogenesis of Late Mesozoic intrusions in the southeast Hubei Province, Middle-Lower Yangtze River Belt (MLYRB), East China. Lithos, 125: 693-710 doi: 10.1016/j.lithos.2011.04.001
Xie GQ, Mao JW, Zhao HJ, Wei KT, Jin SG, Pan HJ and Ke YF. 2011b. Timing of skarn deposits from the Tonglushan ore district, Southeast Hubei Province, Middle-Lower Yangtze River belt and its implication. Ore Geology Reviews, 43(1):62-77 doi: 10.1016/j.oregeorev.2011.05.005
Xing FM and Xu X. 1994. Two A-type granite belts from Anhui. Acta Petrologica Sinica, 10(4): 357-369 (in Chinese with English abstract)
Xing FM and Xu X. 1996. High-potassium calc-alkaline intrusive rocks in Tongling area, Anhui Province. Geochimica, 25(1): 29-38 (in Chinese with English abstract)
Xu HJ, Ma CQ and Ye K. 2007. Early Cretaceous granitoids and their implications for the collapse of the Dabie orogen, eastern China: SHRIMP zircon U-Pb dating and geochemistry. Chemical Geology, 240: 238-259 doi: 10.1016/j.chemgeo.2007.02.018
Xu P, Wu FY, Xie LW and Yang YH. 2004. Hf isotopic compositions of the standard zircon for U-Pb dating. Chinese Science Bulletin, 49: 1642-1648 doi: 10.1007/BF03184136
Yan J, Chen JF and Xu XS. 2008. Geochemistry of Cretaceous mafic rocks from the Lower Yangtze region, eastern China: Characteristics and evolution of the lithospheric mantle. Journal of Asian Earth Science, 33: 177-193 doi: 10.1016/j.jseaes.2007.11.002
Yang ZB, Ding MQ and Yin X. 2003. Magmatic emplacement process inversion and its application to location prediction of ore body. Global Geology, 22(4): 339-343 (in Chinese with English abstract)
Yao PH, Wang KN, Du CL, Lin ZT and Song X. 1993. Records of Chinese Iron Ore Deposits. Beijing: Metallurgic Industry Press, 1-662 (in Chinese)
Yuan HL,Wu FY, Gao S, Liu XM, Xu P and Sun DH. 2003. LA-ICP-MS zircon U-Pb age and REE of Cenozoic pluton in NE China. Chinese Science Bulletin, 48(14): 1511-1520 (in Chinese)
Zhai YS, Yao SZ, Lin XD et al. 1992. Metallogenic regularity of Fe-Cu (-Au) in the Middle-Lower Reaches of the Yangtze-River Area. Beijing: Geological Publishing House, 1-234 (in Chinese)
Zhai YS, Xiong YY, Yao SZ and Lin XD. 1996. Metallogeny of copper and iron deposits in the Eastern Yangtze Carton, east-central China. Ore Geology Review, 11: 229-248 doi: 10.1016/0169-1368(96)00003-0
Zhang D and Li DX. 1999. Study of characteristics of structural deformation with the emplacement of Fenghuangshan pluton, Tongling, Anhui. Acta Geoscientia Sinica, 20(3): 405-410 (in Chinese with English abstract)
Zhang D, Wu GG and Li DX. 2001. Characteristics of contact structural deformation of Fenghuangshan pluton in Tongling, Anhui Province. Earth Science Frontiers, 8(3): 223-229 (in Chinese with English abstract)
Zhang D, Wu GG, Di YJ, Zang WS, Shao YJ, Yu XQ, Zhang XX and Wang QF. 2006. Emplacement dynamics of Fenghuangshan pluton (Tongling, Anhui Province): Constraints from U-Pb SHRIMP dating of zircons and structural deformation. Earth Science-Journal of China University of Geosciences, 31(6): 823-829 (in Chinese with English abstract)
Zhou TF, Yue SC, Yuan F, Liu XD and Zhao Y. 2000. Two series of copper-gold deposits in the Middle and Lower Reaches of the Yangtze River area (MLYRA) and the hydrogen, oxygen, sulfur and lead isotopes of their ore-forming hydrothermal systems. Science in China (Series D), 30(Suppl.): 122-128 (in Chinese)
Zhou TF, Yuan F and Yue SC. 2003. 40Ar-40Ar fast neutron activatinn dating of quartz from the Tongniujing Cu, Mo, Au vein-type hydrothermal deposit, Anhui. Geological Review, 49: 212-216 (in Chinese with English abstract)
Zhou TF, Song MY, Fan Y, Yuan F, Liu J, Wu MA, Qian CC and Lu SM. 2007. Chronology of the Bajiatan intrusions in the Luzong basin, Auhui, and its significance. Acta Petrologica Sinica, 23: 2379-2386 (in Chinese with English abstract)
Zhou TF, Yuan F, YHe SC, Liu XD, Zhang X and Fan Y. 2008.Geochemistry and evolution of ore-forming fluids of the Yueshan Cu-Au skarn-and vein-type deposits, Anhui Province, South China. Ore Geology Reviews, 31: 279-303
Zhou TF, Fan Y and Yuan F. 2008. Advances on petrogensis and metallogeny study of the mineralization belt of the Middle and Lower Reaches of the Yangtze River area. Acta Petrologica Sinica, 24(8): 1665-1678(in Chinese with English abstract)
Zhou XM and Li WX. 2000. Origin of Late Mesozoic igneous rocks in Southeastern China: Implications for lithosphere subduction and underplating of mafic magmas. Tectonophysics, 326: 269-287 doi: 10.1016/S0040-1951(00)00120-7
Zhou XM, Sun T, Shen WZ, Shu LS and Niu YL. 2006. Petrogenesis of Mesozoic granitoids and volcanic rocks in South China: Aresponse to tectonic evolution. Episodes, 29: 26-33
Zhou XR and Ren J. 1994. Mesozoic Granites in the Middle. Lower Reach of Yangtze River. Beijing: Geological Publishing House, 1-118 (in Chinese)
常印佛, 刘湘培, 吴言昌. 1991. 长江中下游铁铜矿成矿带. 北京: 地质出版社, 1-379
邓晋福, 叶德隆, 赵海玲, 汤海平. 1992. 下扬子地区火山作用深部过程盆地形成. 武汉: 中国地质大学出版社, 1-184
邓晋福, 莫宣学, 赵海玲, 罗照华, 赵国春, 戴圣潜. 1999. 中国东部燕山期岩石圈-软流圈系统大灾变与成矿环境. 矿床地质, 18(4): 309-315 http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ199904003.htm
邓军, 王庆飞, 黄定华, 高帮飞. 2004. 铜陵矿集区燕山期地壳浅部成矿流体活动的构造控矿. 矿床地质, 23(3): 399-404 http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200403013.htm
狄永军, 赵海玲, 张贻全, 赵建华, 杨龙. 2003. 安徽铜陵地区燕山期花岗岩类岩石中的岩浆混合结构. 北京地质, 15(1): 12-17 http://www.cnki.com.cn/Article/CJFDTOTAL-JBDZ200301001.htm
杜杨松, 秦新龙, 田世洪. 2004a. 安徽铜陵铜官山矿区中生代岩浆-热液过程: 来自岩石包体及其寄主岩的证据. 岩石学报, 20(2): 339-350 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20040232&journal_id=ysxb
杜杨松, 李炫具. 2004b. 安徽铜陵岩浆岩中辉长质岩石包体的发现及其地质意义. 高校地质学报, 10(3): 332-342 http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200403003.htm
杜杨松, 秦新龙, 李炫具. 2004c. 安徽铜陵地区中生代幔源岩浆底侵作用-来自矿物巨晶和岩石包体的证据. 岩石矿物学杂志, 23(2): 109-116 http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200402001.htm
杜杨松, 李顺庭, 曹毅, 秦新龙, 楼亚儿. 2007. 安徽铜陵铜官山矿区中生代侵入岩的形成过程-岩浆底侵、同化混染和分离结晶. 现代地质, 21(1): 71-77 http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200701007.htm
侯可军, 李延河, 邹天人, 曲晓明, 石玉若, 谢桂青. 2007. LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用. 岩石学报, 23(10): 2595-2604 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=200701025&journal_id=ysxb
李进文, 裴荣富, 梅燕雄. 2004. 铜陵矿集区矿田构造垂直分布. 矿床地质, 23(2): 206-215 http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200402008.htm
李进文, 裴荣富, 张德全, 梅燕雄, 臧文栓, 孟祥贵, 曾普胜, 李铁军, 狄永军. 2007. 铜陵矿集区燕山期中酸性侵入岩地球化学特征及其地质意义. 地球学报, 28(1): 11-22 http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200701002.htm
刘亮明, 王志超, 彭省临. 2002. 综合信息论在储量危急矿山深部找矿中的应用-以铜陵凤凰山铜矿为例. 地质科学, 37(4): 444-452 http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200204007.htm
刘文灿, 高德臻, 储国正. 1996. 安徽铜陵地区构造变形分析及成矿预测. 北京: 地质出版社, 1-133
柳小明, 高山, 袁洪林, Hattendorf B , Günther D , 陈亮, 胡圣红. 2002. 193nm LA-ICP-MS对国际地质标准参考物质中42种主元素和微量元素的分析. 岩石学报, 18(3): 408-418 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20020346&journal_id=ysxb
马昌前, 杨坤光, 唐仲华, 李增田. 1994. 花岗岩类岩浆动力学-理论方法及鄂东花岗岩类例析. 武汉: 中国地质大学出版社, 1-260
毛景文, 华仁民, 李晓波. 1999. 浅议大规模成矿作用与大型矿集区. 矿床地质, 18: 39-43 http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ199904000.htm
毛景文, 胡瑞忠, 陈毓川, 王义天. 2006. 大规模成矿作用与大型矿集区. 北京: 地质出版社, Ⅰ-Ⅶ
毛建仁等. 1990. 长江中下游地区中酸性侵入岩与成矿关系. 北京: 地质出版社, 1-191
毛政利, 赖健清, 彭省临, 邵拥军, 杨斌. 2004. 安徽铜陵凤凰山铜矿床地球化学特征及其意义. 地质与勘探, 40(2): 28-31 http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200402006.htm
裴荣富. 1995. 中国矿床模式. 北京: 地质出版社, 262-264
邵拥军, 彭省临, 刘亮明, 吴淦国. 2003a. 凤凰山矿田成矿地质条件和控矿因素分析. 中南工业大学学报(自然科学版), 34(5): 562-566 http://www.cnki.com.cn/Article/CJFDTOTAL-ZNGD200305025.htm
邵拥军, 彭省临, 吴淦国, 张达. 2003b. 铜陵凤凰山岩体成岩机制探讨. 地质与勘探, 39(5): 39-43 http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200305009.htm
舒全安, 陈培良, 程建荣等. 1992. 鄂东铁铜矿产地质. 北京: 冶金工业出版社, 1-510
唐永成, 吴言昌, 储国正等. 1998. 安徽沿江地区铜金多金属矿床地质. 北京: 地质出版社, 1-351
田世洪, 杜杨松, 秦新龙, 李炫具, 金尚中, 尹京武, 李赞熙. 2001. 安徽铜陵地区中酸性侵入岩及其岩石包体中的矿物包裹体研究. 地学前缘, 8(4): 422-428 http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200104035.htm
王庆飞, 邓军, 黄定华, 张强. 2004. 铜陵矿集区浅层隐伏岩体预测及其形态分析. 矿床地质, 23(3): 405-410 http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200403014.htm
王元龙, 张旗, 王焰. 2001. 宁芜火山岩的地球化学特征及其意义. 岩石学报, 17(4): 565-575 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20010472&journal_id=ysxb
王元龙, 王焰, 张旗, 贾秀琴, 韩松. 2004. 铜陵地区中生代中酸性侵入岩的地质地球化学特征及其成矿-地球动力学意义. 岩石学报, 20(2): 325-338 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20040231&flag=1
闻广, 吴思本. 1983. 安徽铜陵凤凰山岩体若干特征与成矿关系. 中国地质科学院院报, 7: 343-349 http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB198303000.htm
吴才来, 周珣若, 黄许陈, 张成火, 黄文明. 1996. 铜陵地区中酸性侵入岩年代学研究. 岩石矿物学杂志, 5(4): 299-306 http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW604.001.htm
吴淦国, 张达, 臧文栓. 2003. 铜陵矿集区构造滑脱及分层成矿特征研究. 中国科学(D辑), 33(4): 300-308 http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200304001.htm
吴良士, 邹晓秋. 1997. 江西城门山铜矿床Re-Os同位素年龄研究. 矿床地质, 16: 376-381
谢桂青, 李瑞玲, 蒋国豪, 赵财胜, 侯可军. 2008. 鄂东南地区晚中生代侵入岩的地球化学和成因及对岩石圈减薄时限的制约. 岩石学报, 24(8): 1703-1714 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20080804&journal_id=ysxb
谢桂青. 2009. 中国东部长江中下游湖北省中生代火成岩年代学与成因及其与矽卡岩型铜-铁-金矿床的关系. 博士后出站报告.北京:中国地质大学, 1-183
邢凤鸣, 徐祥. 1994. 安徽两条A型花岗岩带. 岩石学报, 10(4): 357-369 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=19940437&journal_id=ysxb
邢凤鸣, 徐祥. 1996. 铜陵地区高钾钙碱系列侵入岩. 地球化学, 25(1): 29-38 http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX601.003.htm
杨中宝, 丁美青, 银霞. 2003. 岩浆侵位过程的反演及其在矿体定位预测中的应用——以安徽铜陵凤凰山矿田为例. 世界地质, 22(4): 339-343 http://www.cnki.com.cn/Article/CJFDTOTAL-SJDZ200304005.htm
姚培慧, 王可南, 杜春林, 林镇泰, 宋雄. 1993. 中国铁矿志.北京: 冶金工业出版社, 1-662
袁洪林, 吴福元, 高山, 柳小明, 徐平, 孙德有. 2003. 东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析. 科学通报, 48 (14): 1511-1520 http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200314007.htm
翟裕生, 姚书振, 林新多等. 1992. 长江中下游地区铁铜(金)成矿规律. 北京: 地质出版社, 1-234
张达, 李东旭. 1999. 铜陵凤凰山岩体侵位构造变形特征. 地球学报, 20(3): 405-410 http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB199903004.htm
张达, 吴淦国, 李东旭. 2001. 铜陵凤凰山岩体接触带构造变形特征. 地学前缘, 8(3): 223-229 http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200103037.htm
张达, 吴淦国, 狄永军, 臧文栓, 邵拥军, 余心起, 张祥信, 汪群峰. 2006. 铜陵凤凰山岩体SHRIMP锆石U-Pb年龄与构造变形及其对岩体侵位动力学背景的制约. 地球科学-中国地质大学学报, 31(6): 823-829 http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200606010.htm
周涛发, 岳书仓, 袁峰, 刘晓东, 赵勇. 2000. 长江中下游两个系列铜、金矿床及其成矿流体系统的氢、氧、硫、铅同位素研究. 中国科学(D), 30(增刊): 122-128 http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2000S1015.htm
周涛发, 袁峰, 岳书仓. 2003. 安庆铜牛井热液脉型铜、钼、金矿床石英的40Ar-39Ar快中子活化年龄. 地质论评, 49: 212-216
周涛发, 宋明义, 范裕, 袁峰, 刘瑁, 吴明安, 钱存超, 陆三明. 2007.安微庐枞火山岩盆地中巴架滩岩体的岩石地球化学特征及成因.岩石学报, 23: 2379-2386
周涛发, 范裕, 袁峰. 2008. 长江中下游成矿带成岩成矿作用研究进展. 岩石学报, 24(8): 1665-1678 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20080801&journal_id=ysxb
周珣若, 任进. 1994. 长江中下游中生代花岗岩. 北京: 地质出版社, 1-118
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