Geoscience ›› 2021, Vol. 35 ›› Issue (02): 535-551.DOI: 10.19657/j.geoscience.1000-8527.2020.105
• Petrology • Previous Articles Next Articles
KOU Guanyu1(), ZHOU Ye2, ZHENG Yuanchuan1, YU Jiaxing1
Received:
2020-09-23
Revised:
2020-10-15
Online:
2021-04-25
Published:
2021-05-25
CLC Number:
KOU Guanyu, ZHOU Ye, ZHENG Yuanchuan, YU Jiaxing. Genesis of Eocene Porphyry in Masjed Daghi, Iran: Evidence from Spectrographic, U-Pb Dating and Geochemical Characteristics[J]. Geoscience, 2021, 35(02): 535-551.
矿区 | 成矿带 | 吨位 /Mt | 品味 | 围岩 | 含矿斑岩 | 成矿类型 | 矿产 | 年龄/Ma | 参考 文献 |
---|---|---|---|---|---|---|---|---|---|
马斯杰德达吉 (Masjed Daghi) | 阿哈尔— 乔勒法 (Ahar-Jolfa) 斑岩成矿带 | 340 | 0.27%Cu, 0.006%Mo, 0.32×10-6Au (20 Mt金矿体) | 始新世安山岩、 火山碎屑岩 | 二长闪长岩 | 脉状,散布状 | Cu+Mo+ Au | 20.46± 3.55 | [ |
松贡 (Sungun) | 阿哈尔— 乔勒法斑岩 成矿带 | 850 | 0.62% Cu, 0.01% Mo | 白垩纪沉积物、 始新世火山岩 | 二长岩-石 英二长岩, 花岗闪长岩 | 脉状,散布状, 矽卡岩 | Cu+Mo | 21 | [ |
萨尔切什梅 (Sar Cheshmeh) | 克尔曼 (Kerman) 斑岩成矿带 | 1 200 | 0.6% Cu, 0.02% Mo | 始新世安山岩、 玄武岩、火山 碎屑岩 | 花岗闪长岩 | 脉状,散布状 | Cu+Mo | 7~13 | [ |
梅杜克 (Meiduk) | 克尔曼斑岩 成矿带 | 500 | 0.8% Cu, 0.007% Mo | 始新世安山岩、玄 武岩、火山碎屑岩 | 花岗闪长岩 | 脉状,散布状 | Cu+Mo | 9~12 | [ |
Table 1 Characteristics of major Iranian porphyry deposits and their ages
矿区 | 成矿带 | 吨位 /Mt | 品味 | 围岩 | 含矿斑岩 | 成矿类型 | 矿产 | 年龄/Ma | 参考 文献 |
---|---|---|---|---|---|---|---|---|---|
马斯杰德达吉 (Masjed Daghi) | 阿哈尔— 乔勒法 (Ahar-Jolfa) 斑岩成矿带 | 340 | 0.27%Cu, 0.006%Mo, 0.32×10-6Au (20 Mt金矿体) | 始新世安山岩、 火山碎屑岩 | 二长闪长岩 | 脉状,散布状 | Cu+Mo+ Au | 20.46± 3.55 | [ |
松贡 (Sungun) | 阿哈尔— 乔勒法斑岩 成矿带 | 850 | 0.62% Cu, 0.01% Mo | 白垩纪沉积物、 始新世火山岩 | 二长岩-石 英二长岩, 花岗闪长岩 | 脉状,散布状, 矽卡岩 | Cu+Mo | 21 | [ |
萨尔切什梅 (Sar Cheshmeh) | 克尔曼 (Kerman) 斑岩成矿带 | 1 200 | 0.6% Cu, 0.02% Mo | 始新世安山岩、 玄武岩、火山 碎屑岩 | 花岗闪长岩 | 脉状,散布状 | Cu+Mo | 7~13 | [ |
梅杜克 (Meiduk) | 克尔曼斑岩 成矿带 | 500 | 0.8% Cu, 0.007% Mo | 始新世安山岩、玄 武岩、火山碎屑岩 | 花岗闪长岩 | 脉状,散布状 | Cu+Mo | 9~12 | [ |
编号 | 含量/10-6 | 同位素比值 | 年龄/Ma | ||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | Pb | 207Pb/206Pb (1σ) | 207Pb/235U (1σ) | 206Pb/238U (1σ) | 207Pb/206Pb (1σ) | 207Pb/235U (1σ) | 206Pb/238U (1σ) | |||
1 | 75.40 | 153.40 | 1.91 | 0.194 8(0.030 5) | 0.207 8(0.029 0) | 0.008 7(0.000 5) | 2 783.65(259.26) | 191.70(24.37) | 56.16(3.37) | ||
2 | 68.81 | 171.28 | 1.98 | 0.187 4(0.049 7) | 0.184 5(0.039 0) | 0.008 1(0.000 3) | 2 720.38(451.70) | 171.89(33.43) | 52.30(1.92) | ||
3 | 69.74 | 135.25 | 1.76 | 0.293 1(0.064 7) | 0.327 9(0.071 2) | 0.008 6(0.000 4) | 3 434.27(349.00) | 287.94(54.50) | 55.33(2.25) | ||
4 | 76.72 | 249.94 | 3.35 | 0.235 8(0.071 6) | 0.344 1(0.124 7) | 0.009 8(0.001 0) | 3 091.67(504.76) | 300.31(94.44) | 63.14(6.53) | ||
5 | 146.88 | 348.51 | 3.77 | 0.069 5(0.005 5) | 0.079 8(0.006 4) | 0.008 7(0.000 3) | 922.22(195.37) | 78.00(6.01) | 55.90(1.78) | ||
6 | 94.40 | 172.80 | 2.76 | 0.240 8(0.036 7) | 0.292 2(0.034 0) | 0.010 0(0.000 7) | 3 125.01(245.07) | 260.33(26.74) | 63.85(4.29) | ||
7 | 140.27 | 215.30 | 2.34 | 0.179 8(0.048 1) | 0.196 7(0.066 2) | 0.007 8(0.000 3) | 2 650.31(458.34) | 182.37(56.21) | 50.23(2.09) | ||
8 | 96.24 | 170.61 | 1.83 | 0.010 8(0.015 2) | 0.012 2(0.015 9) | 0.008 4(0.000 3) | - | 12.33(15.91) | 53.91(1.93) | ||
9 | 293.68 | 538.35 | 5.80 | 0.059 9(0.010 4) | 0.068 9(0.011 9) | 0.008 2(0.000 3) | 611.13(381.44) | 67.69(11.33) | 52.87(2.08) | ||
10 | 121.63 | 318.14 | 5.06 | 0.206 5(0.071 8) | 0.250 4(0.077 3) | 0.009 4(0.000 4) | 2 878.7(596.43) | 226.92(62.83) | 60.06(2.43) | ||
11 | 146.05 | 368.76 | 3.64 | 0.148 1(0.060 6) | 0.140 4(0.049 9) | 0.007 9(0.000 2) | 2 324.39(761.88) | 133.44(44.44) | 50.92(1.55) | ||
12 | 119.76 | 263.15 | 2.83 | 0.080 8(0.006 3) | 0.097 0(0.009 0) | 0.008 4(0.000 3) | 1 216.67(155.09) | 93.96(8.37) | 54.09(2.05) | ||
13 | 79.83 | 163.51 | 1.70 | 0.246 7(0.041 0) | 0.242 9(0.035 5) | 0.008 3(0.000 3) | 3 164.82(266.67) | 220.76(28.99) | 53.01(2.12) | ||
14 | 113.20 | 331.29 | 3.34 | 0.095 5(0.012 7) | 0.103 4(0.011 1) | 0.008 8(0.000 5) | 1 536.73(251.85) | 99.89(10.23) | 56.37(3.35) | ||
15 | 133.43 | 282.62 | 3.01 | 0.100 5(0.016 6) | 0.106 5(0.015 0) | 0.008 5(0.000 4) | 1 633.02(311.11) | 102.80(13.81) | 54.35(2.27) |
Table 2 LA-ICP-MS zircon U-Pb data of the Masjed Daghi porphyry sample (MAD-13-483)
编号 | 含量/10-6 | 同位素比值 | 年龄/Ma | ||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | Pb | 207Pb/206Pb (1σ) | 207Pb/235U (1σ) | 206Pb/238U (1σ) | 207Pb/206Pb (1σ) | 207Pb/235U (1σ) | 206Pb/238U (1σ) | |||
1 | 75.40 | 153.40 | 1.91 | 0.194 8(0.030 5) | 0.207 8(0.029 0) | 0.008 7(0.000 5) | 2 783.65(259.26) | 191.70(24.37) | 56.16(3.37) | ||
2 | 68.81 | 171.28 | 1.98 | 0.187 4(0.049 7) | 0.184 5(0.039 0) | 0.008 1(0.000 3) | 2 720.38(451.70) | 171.89(33.43) | 52.30(1.92) | ||
3 | 69.74 | 135.25 | 1.76 | 0.293 1(0.064 7) | 0.327 9(0.071 2) | 0.008 6(0.000 4) | 3 434.27(349.00) | 287.94(54.50) | 55.33(2.25) | ||
4 | 76.72 | 249.94 | 3.35 | 0.235 8(0.071 6) | 0.344 1(0.124 7) | 0.009 8(0.001 0) | 3 091.67(504.76) | 300.31(94.44) | 63.14(6.53) | ||
5 | 146.88 | 348.51 | 3.77 | 0.069 5(0.005 5) | 0.079 8(0.006 4) | 0.008 7(0.000 3) | 922.22(195.37) | 78.00(6.01) | 55.90(1.78) | ||
6 | 94.40 | 172.80 | 2.76 | 0.240 8(0.036 7) | 0.292 2(0.034 0) | 0.010 0(0.000 7) | 3 125.01(245.07) | 260.33(26.74) | 63.85(4.29) | ||
7 | 140.27 | 215.30 | 2.34 | 0.179 8(0.048 1) | 0.196 7(0.066 2) | 0.007 8(0.000 3) | 2 650.31(458.34) | 182.37(56.21) | 50.23(2.09) | ||
8 | 96.24 | 170.61 | 1.83 | 0.010 8(0.015 2) | 0.012 2(0.015 9) | 0.008 4(0.000 3) | - | 12.33(15.91) | 53.91(1.93) | ||
9 | 293.68 | 538.35 | 5.80 | 0.059 9(0.010 4) | 0.068 9(0.011 9) | 0.008 2(0.000 3) | 611.13(381.44) | 67.69(11.33) | 52.87(2.08) | ||
10 | 121.63 | 318.14 | 5.06 | 0.206 5(0.071 8) | 0.250 4(0.077 3) | 0.009 4(0.000 4) | 2 878.7(596.43) | 226.92(62.83) | 60.06(2.43) | ||
11 | 146.05 | 368.76 | 3.64 | 0.148 1(0.060 6) | 0.140 4(0.049 9) | 0.007 9(0.000 2) | 2 324.39(761.88) | 133.44(44.44) | 50.92(1.55) | ||
12 | 119.76 | 263.15 | 2.83 | 0.080 8(0.006 3) | 0.097 0(0.009 0) | 0.008 4(0.000 3) | 1 216.67(155.09) | 93.96(8.37) | 54.09(2.05) | ||
13 | 79.83 | 163.51 | 1.70 | 0.246 7(0.041 0) | 0.242 9(0.035 5) | 0.008 3(0.000 3) | 3 164.82(266.67) | 220.76(28.99) | 53.01(2.12) | ||
14 | 113.20 | 331.29 | 3.34 | 0.095 5(0.012 7) | 0.103 4(0.011 1) | 0.008 8(0.000 5) | 1 536.73(251.85) | 99.89(10.23) | 56.37(3.35) | ||
15 | 133.43 | 282.62 | 3.01 | 0.100 5(0.016 6) | 0.106 5(0.015 0) | 0.008 5(0.000 4) | 1 633.02(311.11) | 102.80(13.81) | 54.35(2.27) |
点号 | SiO2 | TiO2 | Al2O3 | FeO | MnO | MgO | CaO | Na2O | K2O | F | Cl | Cr2O3 | P2O5 | Al/(Ca+ Na+K) | K2O+ Na2O+CaO | An | Ab | Or |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
pl-1 | 60.13 | 0.020 | 24.47 | 0.168 | 0.019 | - | 5.926 | 8.322 | 0.264 | 0.092 | - | - | 0.007 | 1.26 | 14.512 | 27.82 | 70.70 | 1.47 |
pl-2 | 59.39 | - | 25.75 | 0.203 | 0.027 | 0.008 | 7.112 | 7.598 | 0.189 | 0.050 | - | - | 0.011 | 1.34 | 14.899 | 33.72 | 65.20 | 1.06 |
pl-3 | 59.86 | 0.025 | 24.82 | 0.336 | 0.034 | - | 6.706 | 7.961 | 0.253 | - | - | 0.005 | 0.022 | 1.27 | 14.920 | 31.31 | 67.27 | 1.40 |
pl-4 | 60.12 | 0.048 | 24.82 | 0.149 | 0.034 | - | 6.491 | 8.185 | 0.277 | 0.078 | 0.001 | - | 0.019 | 1.26 | 14.953 | 30.00 | 68.46 | 1.52 |
pl-5 | 60.03 | - | 24.49 | 0.133 | - | 0.024 | 6.349 | 7.803 | 0.270 | - | 0.006 | - | - | 1.29 | 14.422 | 30.53 | 67.91 | 1.54 |
pl2-1 | 58.20 | - | 25.78 | 0.140 | - | - | 7.565 | 7.453 | 0.186 | - | 0.002 | - | 0.011 | 1.33 | 15.204 | 35.56 | 63.39 | 1.04 |
pl2-2 | 58.65 | 0.048 | 25.21 | 0.155 | 0.050 | - | 7.047 | 7.563 | 0.224 | 0.050 | 0.003 | - | 0.022 | 1.32 | 14.834 | 33.55 | 65.17 | 1.26 |
pl2-3 | 57.07 | 0.002 | 26.57 | 0.102 | 0.053 | 0.006 | 8.688 | 6.746 | 0.186 | - | - | - | - | 1.38 | 15.620 | 41.14 | 57.80 | 1.04 |
pl2-4 | 58.74 | 0.041 | 25.95 | 0.193 | - | 0.006 | 7.778 | 7.369 | 0.172 | 0.100 | - | 0.037 | - | 1.33 | 15.319 | 36.48 | 62.55 | 0.96 |
pl2-5 | 63.46 | - | 22.51 | 0.073 | - | - | 3.711 | 9.676 | 0.335 | - | - | - | 0.019 | 1.14 | 13.722 | 17.16 | 80.99 | 1.84 |
pl3-1 | 56.98 | - | 26.76 | 0.235 | 0.011 | - | 8.552 | 6.855 | 0.178 | - | 0.006 | - | - | 1.39 | 15.585 | 40.39 | 58.59 | 1.00 |
pl3-2 | 55.45 | 0.016 | 25.47 | 0.082 | 0.034 | 0.041 | 7.649 | 7.179 | 0.184 | 0.036 | 0.011 | - | 0.019 | 1.34 | 15.012 | 36.66 | 62.28 | 1.05 |
pl3-3 | 55.74 | 0.005 | 26.26 | 0.133 | 0.023 | 0.243 | 7.638 | 6.516 | 0.729 | - | 0.007 | - | 0.015 | 1.42 | 14.883 | 37.63 | 58.09 | 4.27 |
pl3-4 | 57.19 | 0.014 | 25.88 | 0.101 | 0.019 | 0.103 | 7.080 | 6.841 | 0.482 | - | 0.008 | - | - | 1.42 | 14.403 | 35.34 | 61.79 | 2.86 |
pl3-5 | 64.91 | - | 22.01 | 0.086 | 0.030 | 0.061 | 1.655 | 9.476 | 1.787 | 0.035 | - | 0.057 | - | 1.15 | 12.918 | 7.90 | 81.92 | 10.16 |
Table 3 Representative EPMA major element compositions (%) of feldspars from the Masjed Daghi porphyry sample (MAD-13-483)
点号 | SiO2 | TiO2 | Al2O3 | FeO | MnO | MgO | CaO | Na2O | K2O | F | Cl | Cr2O3 | P2O5 | Al/(Ca+ Na+K) | K2O+ Na2O+CaO | An | Ab | Or |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
pl-1 | 60.13 | 0.020 | 24.47 | 0.168 | 0.019 | - | 5.926 | 8.322 | 0.264 | 0.092 | - | - | 0.007 | 1.26 | 14.512 | 27.82 | 70.70 | 1.47 |
pl-2 | 59.39 | - | 25.75 | 0.203 | 0.027 | 0.008 | 7.112 | 7.598 | 0.189 | 0.050 | - | - | 0.011 | 1.34 | 14.899 | 33.72 | 65.20 | 1.06 |
pl-3 | 59.86 | 0.025 | 24.82 | 0.336 | 0.034 | - | 6.706 | 7.961 | 0.253 | - | - | 0.005 | 0.022 | 1.27 | 14.920 | 31.31 | 67.27 | 1.40 |
pl-4 | 60.12 | 0.048 | 24.82 | 0.149 | 0.034 | - | 6.491 | 8.185 | 0.277 | 0.078 | 0.001 | - | 0.019 | 1.26 | 14.953 | 30.00 | 68.46 | 1.52 |
pl-5 | 60.03 | - | 24.49 | 0.133 | - | 0.024 | 6.349 | 7.803 | 0.270 | - | 0.006 | - | - | 1.29 | 14.422 | 30.53 | 67.91 | 1.54 |
pl2-1 | 58.20 | - | 25.78 | 0.140 | - | - | 7.565 | 7.453 | 0.186 | - | 0.002 | - | 0.011 | 1.33 | 15.204 | 35.56 | 63.39 | 1.04 |
pl2-2 | 58.65 | 0.048 | 25.21 | 0.155 | 0.050 | - | 7.047 | 7.563 | 0.224 | 0.050 | 0.003 | - | 0.022 | 1.32 | 14.834 | 33.55 | 65.17 | 1.26 |
pl2-3 | 57.07 | 0.002 | 26.57 | 0.102 | 0.053 | 0.006 | 8.688 | 6.746 | 0.186 | - | - | - | - | 1.38 | 15.620 | 41.14 | 57.80 | 1.04 |
pl2-4 | 58.74 | 0.041 | 25.95 | 0.193 | - | 0.006 | 7.778 | 7.369 | 0.172 | 0.100 | - | 0.037 | - | 1.33 | 15.319 | 36.48 | 62.55 | 0.96 |
pl2-5 | 63.46 | - | 22.51 | 0.073 | - | - | 3.711 | 9.676 | 0.335 | - | - | - | 0.019 | 1.14 | 13.722 | 17.16 | 80.99 | 1.84 |
pl3-1 | 56.98 | - | 26.76 | 0.235 | 0.011 | - | 8.552 | 6.855 | 0.178 | - | 0.006 | - | - | 1.39 | 15.585 | 40.39 | 58.59 | 1.00 |
pl3-2 | 55.45 | 0.016 | 25.47 | 0.082 | 0.034 | 0.041 | 7.649 | 7.179 | 0.184 | 0.036 | 0.011 | - | 0.019 | 1.34 | 15.012 | 36.66 | 62.28 | 1.05 |
pl3-3 | 55.74 | 0.005 | 26.26 | 0.133 | 0.023 | 0.243 | 7.638 | 6.516 | 0.729 | - | 0.007 | - | 0.015 | 1.42 | 14.883 | 37.63 | 58.09 | 4.27 |
pl3-4 | 57.19 | 0.014 | 25.88 | 0.101 | 0.019 | 0.103 | 7.080 | 6.841 | 0.482 | - | 0.008 | - | - | 1.42 | 14.403 | 35.34 | 61.79 | 2.86 |
pl3-5 | 64.91 | - | 22.01 | 0.086 | 0.030 | 0.061 | 1.655 | 9.476 | 1.787 | 0.035 | - | 0.057 | - | 1.15 | 12.918 | 7.90 | 81.92 | 10.16 |
Fig.9 SiO2 vs.(CaO+Na2O+K2O) (a), and An vs. Al / (Ca+Na+K) (b) diagrams of feldspars from the Masjed Daghi porphyry sample (MAD-13-483) (modified after Zarasvandi et al.[44])
编号 | SiO2 | Na2O | K2O | Cr2O3 | Al2O3 | MgO | CaO | MnO | P2O5 | FeO | TiO2 | NiO | 总量 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1 | 98.284 | 0.014 | 0.014 | - | - | 0.002 | 0.008 | 0.036 | - | 0.004 | 0.009 | 0.027 | 98.398 |
2 | 99.230 | 0.026 | 0.004 | 0.018 | 0.021 | - | 0.008 | - | - | - | - | 0.035 | 99.342 |
3 | 98.447 | 0.029 | 0.018 | 0.023 | 0.009 | - | 0.010 | - | - | 0.046 | - | - | 98.582 |
4 | 98.328 | 0.066 | 0.016 | 0.551 | 0.036 | 0.018 | 0.025 | 0.031 | - | - | - | - | 99.071 |
5 | 99.503 | 0.021 | 0.009 | - | 0.030 | - | 0.023 | - | - | - | 0.005 | 0.069 | 99.660 |
6 | 99.292 | 0.008 | - | 0.005 | 0.02 | - | 0.013 | - | 0.019 | - | 0.007 | - | 99.364 |
7 | 98.809 | - | - | 0.005 | 0.021 | - | - | - | 0.010 | 0.031 | 0.020 | 0.017 | 98.913 |
8 | 99.059 | 0.015 | 0.007 | - | 0.054 | 0.011 | - | - | - | - | 0.060 | 0.007 | 99.213 |
9 | 98.805 | 0.005 | - | - | - | - | 0.017 | 0.014 | 0.001 | 0.023 | 0.017 | 0.017 | 98.899 |
10 | 98.965 | 0.003 | - | 0.041 | 0.071 | - | 0.010 | - | 0.033 | - | 0.061 | - | 99.184 |
Table 4 Representative EPMA major element compositions (%) of quartz from the Masjed Daghi porphyry sample (MAD-13-483)
编号 | SiO2 | Na2O | K2O | Cr2O3 | Al2O3 | MgO | CaO | MnO | P2O5 | FeO | TiO2 | NiO | 总量 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1 | 98.284 | 0.014 | 0.014 | - | - | 0.002 | 0.008 | 0.036 | - | 0.004 | 0.009 | 0.027 | 98.398 |
2 | 99.230 | 0.026 | 0.004 | 0.018 | 0.021 | - | 0.008 | - | - | - | - | 0.035 | 99.342 |
3 | 98.447 | 0.029 | 0.018 | 0.023 | 0.009 | - | 0.010 | - | - | 0.046 | - | - | 98.582 |
4 | 98.328 | 0.066 | 0.016 | 0.551 | 0.036 | 0.018 | 0.025 | 0.031 | - | - | - | - | 99.071 |
5 | 99.503 | 0.021 | 0.009 | - | 0.030 | - | 0.023 | - | - | - | 0.005 | 0.069 | 99.660 |
6 | 99.292 | 0.008 | - | 0.005 | 0.02 | - | 0.013 | - | 0.019 | - | 0.007 | - | 99.364 |
7 | 98.809 | - | - | 0.005 | 0.021 | - | - | - | 0.010 | 0.031 | 0.020 | 0.017 | 98.913 |
8 | 99.059 | 0.015 | 0.007 | - | 0.054 | 0.011 | - | - | - | - | 0.060 | 0.007 | 99.213 |
9 | 98.805 | 0.005 | - | - | - | - | 0.017 | 0.014 | 0.001 | 0.023 | 0.017 | 0.017 | 98.899 |
10 | 98.965 | 0.003 | - | 0.041 | 0.071 | - | 0.010 | - | 0.033 | - | 0.061 | - | 99.184 |
编号 | ZrO2 | Ce | Lu | Hf | Ce4+/Ce3+ |
---|---|---|---|---|---|
1 | 94.81 | 8.11 | 46.06 | 9 356.71 | 217.45 |
2 | 91.12 | 7.79 | 39.15 | 8 914.20 | 197.24 |
3 | 91.85 | 8.05 | 43.98 | 8 085.89 | 152.12 |
4 | 89.97 | 15.67 | 57.84 | 9 701.81 | 543.19 |
5 | 91.74 | 16.01 | 36.09 | 9 968.56 | 433.31 |
6 | 93.38 | 10.37 | 47.34 | 9 335.95 | 471.77 |
7 | 90.77 | 11.96 | 41.65 | 8 920.27 | 247.08 |
8 | 90.30 | 14.09 | 33.20 | 8 615.26 | 496.12 |
9 | 94.94 | 31.78 | 103.09 | 10 190.34 | 252.40 |
10 | 91.64 | 14.42 | 60.42 | 9 956.50 | 205.69 |
11 | 90.89 | 15.00 | 49.37 | 9 846.30 | 481.46 |
12 | 91.52 | 12.52 | 44.18 | 10 053.70 | 324.96 |
13 | 89.70 | 10.29 | 37.67 | 9 252.59 | 259.83 |
14 | 88.98 | 13.53 | 71.74 | 9 965.00 | 469.19 |
15 | 94.64 | 15.40 | 58.59 | 9 799.83 | 204.75 |
Table 5 Representative zircon major (%) and trace element (10-6) compositions of the Masjed Daghi porphyry sample (MAD-13-483)
编号 | ZrO2 | Ce | Lu | Hf | Ce4+/Ce3+ |
---|---|---|---|---|---|
1 | 94.81 | 8.11 | 46.06 | 9 356.71 | 217.45 |
2 | 91.12 | 7.79 | 39.15 | 8 914.20 | 197.24 |
3 | 91.85 | 8.05 | 43.98 | 8 085.89 | 152.12 |
4 | 89.97 | 15.67 | 57.84 | 9 701.81 | 543.19 |
5 | 91.74 | 16.01 | 36.09 | 9 968.56 | 433.31 |
6 | 93.38 | 10.37 | 47.34 | 9 335.95 | 471.77 |
7 | 90.77 | 11.96 | 41.65 | 8 920.27 | 247.08 |
8 | 90.30 | 14.09 | 33.20 | 8 615.26 | 496.12 |
9 | 94.94 | 31.78 | 103.09 | 10 190.34 | 252.40 |
10 | 91.64 | 14.42 | 60.42 | 9 956.50 | 205.69 |
11 | 90.89 | 15.00 | 49.37 | 9 846.30 | 481.46 |
12 | 91.52 | 12.52 | 44.18 | 10 053.70 | 324.96 |
13 | 89.70 | 10.29 | 37.67 | 9 252.59 | 259.83 |
14 | 88.98 | 13.53 | 71.74 | 9 965.00 | 469.19 |
15 | 94.64 | 15.40 | 58.59 | 9 799.83 | 204.75 |
SiO2 | TiO2 | Al2O3 | Fe2O3 | MnO | MgO | CaO | Na2O | K2O |
---|---|---|---|---|---|---|---|---|
63.44 | 0.37 | 14.39 | 1.73 | 0.02 | 2.18 | 3.43 | 3.81 | 4.85 |
P2O5 | LOI | SUM | Na+K | Li | Be | Sc | V | Cr |
0.07 | 4.49 | 98.78 | 8.66 | 11.09 | 0.85 | 7.95 | 84.74 | 15.88 |
Co | Ni | Cu | Zn | Ga | Rb | Sr | Y | Zr |
4.91 | 9.97 | 1 957.96 | 61.28 | 14.64 | 111.64 | 702.24 | 5.81 | 106.83 |
Nb | Sn | Cs | Ba | La | Ce | Pr | Nd | Sm |
8.06 | 0.85 | 1.78 | 1 177.61 | 25.54 | 40.11 | 3.88 | 12.71 | 1.99 |
Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu |
0.66 | 1.37 | 0.18 | 1.05 | 0.19 | 0.59 | 0.09 | 0.58 | 0.09 |
Hf | Ta | Pb | Th | U | Sr/Y | |||
2.67 | 0.46 | 32.99 | 9.78 | 1.83 | 120.78 |
Table 6 Whole-rock major (%) and trace element (10-6) compositions of the porphyry sample(MAD-13-483)
SiO2 | TiO2 | Al2O3 | Fe2O3 | MnO | MgO | CaO | Na2O | K2O |
---|---|---|---|---|---|---|---|---|
63.44 | 0.37 | 14.39 | 1.73 | 0.02 | 2.18 | 3.43 | 3.81 | 4.85 |
P2O5 | LOI | SUM | Na+K | Li | Be | Sc | V | Cr |
0.07 | 4.49 | 98.78 | 8.66 | 11.09 | 0.85 | 7.95 | 84.74 | 15.88 |
Co | Ni | Cu | Zn | Ga | Rb | Sr | Y | Zr |
4.91 | 9.97 | 1 957.96 | 61.28 | 14.64 | 111.64 | 702.24 | 5.81 | 106.83 |
Nb | Sn | Cs | Ba | La | Ce | Pr | Nd | Sm |
8.06 | 0.85 | 1.78 | 1 177.61 | 25.54 | 40.11 | 3.88 | 12.71 | 1.99 |
Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu |
0.66 | 1.37 | 0.18 | 1.05 | 0.19 | 0.59 | 0.09 | 0.58 | 0.09 |
Hf | Ta | Pb | Th | U | Sr/Y | |||
2.67 | 0.46 | 32.99 | 9.78 | 1.83 | 120.78 |
Fig.10 TAS (a), SiO2 vs. K2O (b), and Y vs. Sr/Y(c)classification diagrams of the porphyry sample (MAO-13-483)((a)modified after Middle-most[46], (b) modified after Peccerillo and Taylor [47],(c) modified after Defant et al.[48])
编号 | 年龄/Ma | 176Hf/177Hf(2σ) | 176Lu/177Hf(2σ) | εHf (t) | TDM /Ma | |
---|---|---|---|---|---|---|
1 | 56.16 | 0.283 02(0.000 02) | 0.000 82(0.000 02) | 9.95 | 327.79 | 492.38 |
2 | 52.30 | 0.283 05(0.000 04) | 0.000 86(0.000 01) | 10.90 | 286.45 | 427.92 |
3 | 55.33 | 0.283 03(0.000 03) | 0.000 67(0.000 04) | 10.39 | 308.30 | 463.22 |
4 | 63.14 | 0.283 02(0.000 02) | 0.001 15(0.000 02) | 10.16 | 327.80 | 484.47 |
5 | 55.90 | 0.282 99(0.000 02) | 0.000 98(0.000 01) | 8.87 | 372.20 | 561.78 |
6 | 63.85 | 0.283 02(0.000 02) | 0.000 86(0.000 01) | 10.31 | 320.33 | 475.28 |
7 | 50.23 | 0.283 07(0.000 02) | 0.000 76(0.000 01) | 11.72 | 251.33 | 373.71 |
8 | 53.91 | 0.283 02(0.000 02) | 0.000 79(0.000 03) | 9.80 | 331.75 | 500.52 |
9 | 52.87 | 0.282 87(0.000 07) | 0.001 53(0.000 02) | 4.47 | 553.33 | 841.47 |
10 | 60.06 | 0.282 98(0.000 07) | 0.000 84(0.000 01) | 8.52 | 388.31 | 586.92 |
11 | 50.92 | 0.283 12(0.000 02) | 0.000 94(0.000 01) | 13.50 | 181.36 | 259.74 |
12 | 54.09 | 0.283 03(0.000 02) | 0.001 06(0.000 02) | 10.44 | 308.08 | 459.43 |
13 | 53.01 | 0.283 03(0.000 02) | 0.000 94(0.000 01) | 10.42 | 307.13 | 459.82 |
14 | 56.37 | 0.283 03(0.000 02) | 0.000 90(0.000 01) | 10.41 | 310.16 | 463.05 |
15 | 54.35 | 0.283 04(0.000 03) | 0.000 83(0.000 01) | 10.61 | 299.63 | 448.19 |
16 | 54.00 | 0.283 05(0.000 03) | 0.000 62(0.000 04) | 11.13 | 277.45 | 414.72 |
17 | 54.00 | 0.282 99(0.000 03) | 0.000 90(0.000 03) | 8.70 | 376.72 | 571.12 |
18 | 54.00 | 0.283 04(0.000 03) | 0.001 23(0.000 02) | 10.49 | 307.20 | 456.16 |
19 | 54.00 | 0.283 04(0.000 03) | 0.000 56(0.000 01) | 10.53 | 300.85 | 453.21 |
20 | 54.00 | 0.283 06(0.000 03) | 0.000 65(0.000 01) | 11.29 | 271.31 | 404.56 |
21 | 54.00 | 0.283 07(0.000 03) | 0.000 84(0.000 01) | 11.56 | 261.58 | 387.17 |
22 | 54.00 | 0.283 06(0.000 02) | 0.000 91(0.000 02) | 11.43 | 266.99 | 395.22 |
23 | 54.00 | 0.283 06(0.000 02) | 0.000 98(0.000 01) | 11.29 | 272.91 | 404.11 |
24 | 54.00 | 0.283 01(0.000 02) | 0.001 38(0.000 01) | 9.69 | 340.61 | 507.45 |
25 | 54.00 | 0.283 03(0.000 02) | 0.001 07(0.000 01) | 10.21 | 317.06 | 473.68 |
Table 7 Zircon Lu-Hf isotope data of the Masjed Daghi porphyry sample (MAD-13-483)
编号 | 年龄/Ma | 176Hf/177Hf(2σ) | 176Lu/177Hf(2σ) | εHf (t) | TDM /Ma | |
---|---|---|---|---|---|---|
1 | 56.16 | 0.283 02(0.000 02) | 0.000 82(0.000 02) | 9.95 | 327.79 | 492.38 |
2 | 52.30 | 0.283 05(0.000 04) | 0.000 86(0.000 01) | 10.90 | 286.45 | 427.92 |
3 | 55.33 | 0.283 03(0.000 03) | 0.000 67(0.000 04) | 10.39 | 308.30 | 463.22 |
4 | 63.14 | 0.283 02(0.000 02) | 0.001 15(0.000 02) | 10.16 | 327.80 | 484.47 |
5 | 55.90 | 0.282 99(0.000 02) | 0.000 98(0.000 01) | 8.87 | 372.20 | 561.78 |
6 | 63.85 | 0.283 02(0.000 02) | 0.000 86(0.000 01) | 10.31 | 320.33 | 475.28 |
7 | 50.23 | 0.283 07(0.000 02) | 0.000 76(0.000 01) | 11.72 | 251.33 | 373.71 |
8 | 53.91 | 0.283 02(0.000 02) | 0.000 79(0.000 03) | 9.80 | 331.75 | 500.52 |
9 | 52.87 | 0.282 87(0.000 07) | 0.001 53(0.000 02) | 4.47 | 553.33 | 841.47 |
10 | 60.06 | 0.282 98(0.000 07) | 0.000 84(0.000 01) | 8.52 | 388.31 | 586.92 |
11 | 50.92 | 0.283 12(0.000 02) | 0.000 94(0.000 01) | 13.50 | 181.36 | 259.74 |
12 | 54.09 | 0.283 03(0.000 02) | 0.001 06(0.000 02) | 10.44 | 308.08 | 459.43 |
13 | 53.01 | 0.283 03(0.000 02) | 0.000 94(0.000 01) | 10.42 | 307.13 | 459.82 |
14 | 56.37 | 0.283 03(0.000 02) | 0.000 90(0.000 01) | 10.41 | 310.16 | 463.05 |
15 | 54.35 | 0.283 04(0.000 03) | 0.000 83(0.000 01) | 10.61 | 299.63 | 448.19 |
16 | 54.00 | 0.283 05(0.000 03) | 0.000 62(0.000 04) | 11.13 | 277.45 | 414.72 |
17 | 54.00 | 0.282 99(0.000 03) | 0.000 90(0.000 03) | 8.70 | 376.72 | 571.12 |
18 | 54.00 | 0.283 04(0.000 03) | 0.001 23(0.000 02) | 10.49 | 307.20 | 456.16 |
19 | 54.00 | 0.283 04(0.000 03) | 0.000 56(0.000 01) | 10.53 | 300.85 | 453.21 |
20 | 54.00 | 0.283 06(0.000 03) | 0.000 65(0.000 01) | 11.29 | 271.31 | 404.56 |
21 | 54.00 | 0.283 07(0.000 03) | 0.000 84(0.000 01) | 11.56 | 261.58 | 387.17 |
22 | 54.00 | 0.283 06(0.000 02) | 0.000 91(0.000 02) | 11.43 | 266.99 | 395.22 |
23 | 54.00 | 0.283 06(0.000 02) | 0.000 98(0.000 01) | 11.29 | 272.91 | 404.11 |
24 | 54.00 | 0.283 01(0.000 02) | 0.001 38(0.000 01) | 9.69 | 340.61 | 507.45 |
25 | 54.00 | 0.283 03(0.000 02) | 0.001 07(0.000 01) | 10.21 | 317.06 | 473.68 |
[1] |
SILLITOE R H. Porphyry copper systems[J]. Economic Geology, 2010,105:3-41.
DOI URL |
[2] |
RICHARDS J P. Postsubduction porphyry Cu-Au and epithermal Au deposits: Products of remelting of subduction-modified lithosphere[J]. Geology, 2009,37(3):247-250.
DOI URL |
[3] | 侯增谦, 郑远川, 杨志明, 等. 大陆碰撞成矿作用:Ⅰ.冈底斯新生代斑岩成矿系统[J]. 矿床地质, 2012,31(4):647-670. |
[4] | 汪啸风, METCSLFE I, 简平, 等. 金沙江缝合带构造地层划分及时代厘定[J]. 中国科学(D辑), 1999,29(4):289-297. |
[5] |
ZHANG Z Y, XIAO W J, JI W Q, et al. Geochemistry, zircon U-Pb and Hf isotope for granitoids, NW Sanandaj-Sirjan zone, Iran: Implications for Mesozoic-Cenozoic episodic magmatism during Neo-Tethyan lithospheric subduction[J]. Gondwana Research, 2018,62:227-245.
DOI URL |
[6] |
SHAFIEI B, HASCHKE M, SHAHABPOUR J. Recycling of orogenic arc crust triggers porphyry Cu mineralization in Kerman Cenozoic arc rocks, southeastern Iran[J]. Mineralium Deposita, 2009,44:265-283.
DOI URL |
[7] |
ASADI S, MOORE F, ZARASVANDI A. Discriminating productive and barren porphyry copper deposits in the southeastern part of the central Iranian volcano-plutonic belt, Kerman region, Iran: A review[J]. Earth-Science Reviews, 2014,138:25-46.
DOI URL |
[8] |
IMAMALIPOUR A, MOUSAVI R. Vertical geochemical zonation in the Masjed Daghi porphyry copper-gold deposit, northwestern Iran: implications for exploration of blind mineral deposits[J]. Geochemistry: Exploration, Environment, Analysis, 2017,18:120-131.
DOI URL |
[9] |
ALLEN M B, ARMSTRONG H A. Arabia-Eurasia collision and the forcing of mid-Cenozoic global cooling[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2008,265(1):52-58.
DOI URL |
[10] |
AGARD P, OMRANI J, JOLIVET L, et al. Zagros Orogeny: A subduction-dominated process[J]. Geological Magazine, 2011,148:692-725.
DOI URL |
[11] |
AGHAZADEH M, CASTRO A, BADRZADEH Z, et al. Post-collisional polycyclic plutonism from the Zagros hinterland: the Shaivar Dagh plutonic complex, Alborz belt, Iran[J]. Geological Magazine, 2011,148(5/6):980-1008.
DOI URL |
[12] |
AGARD P, OMRANI J, JOLIVET L, et al. Convergence history across Zagros (Iran): Constraints from collisional and earlier deformation[J]. International Journal of Earth Sciences, 2005,94:401-419.
DOI URL |
[13] |
GOLONKA J. Plate tectonic evolution of the southern margin of Eurasia in the Mesozoic and Cenozoic[J]. Tectonophysics, 2004,381(1/4):235-273.
DOI URL |
[14] |
RICHARDA J P, SPELL T, RAMEH E, et al. High Sr/Y Magmas Reflect Arc Maturity, High Magmatic Water Content, and Porphyry Cu±Mo±Au Potential: Examples from the Tethyan Arcs of Central and Eastern Iran and Western Pakistan[J]. Economic Geology, 2012,107(2):295-332.
DOI URL |
[15] | KIRKHAM R V, DUNNE K P. World Distribution of Porphyry, Porphyry-associated Skarn, and bulk-tonnage epithermal deposits and occurrences[R]. Wotawa:The Geological Survey of Canada, 2000: 1-26. |
[16] | RAZIQUE A, LO GRASSO G, LIVESEY T. Porphyry copper-gold deposits at Reko Diq complex, Chagai Hills Pakistan[M]//9th Biennial Meeting of the Society for Geology Applied to Mineral Deposits. Dublin: SGA, 2007: 125-128. |
[17] |
JAHANGIRI A. Post-collisional Miocene adakitic volcanism in NW Iran: Geochemical and geodynamic implications[J]. Journal of Asian Earth sciences, 2007,30(3/4):433-447.
DOI URL |
[18] |
WATERMAN G C, HAMILTON R L. The Sar Cheshmeh porphyry copper deposit[J]. Economic Geology, 1975,70(3):568-576.
DOI URL |
[19] |
COOKE D R, HOLLINGS P, WALSHE J L. Giant porphyry deposits: characteristics, distribution, and tectonic controls[J]. Economic Geology, 2005,100(5):801-818.
DOI URL |
[20] |
SINGER D A, BERGER V I, MENZIE W D, et al. Porphyry copper deposit density[J]. Economic Geology, 2005,100:491-514.
DOI URL |
[21] | ZARASVANDI A, LIAGHAT S, ZENTILLI M. Geology of the Darreh-Zerreshk and Ali-Abad porphyry copper deposits, central Iran[J]. International Geology Review, 2005(6):620-646. |
[22] |
ZARASVANDI A, LIAGHAT S, ZENTILLI M, et al. 40Ar/39Ar geochronology of alteration and petrogenesis of porphyry copper-related granitoids in the Darreh-Zerreshk and Ali-Abad area, central Iran[J]. Exploration and Mining Geology, 2007,16(1/2):11-24.
DOI URL |
[23] | ZHANG H R, HOU Z Q, SONG Y C, et al. The temporal and spatial distribution of porphyry copper deposits in the eastern Tethyan metallogenic domain: A review[J]. Acta Geologica Sinica, 2009,83(12):1818-1837. |
[24] | SAMANI B. Distribution, setting and metallogenesis of copper deposits in Iran[M]//SAMANI B. Porphyry and Hydrothermal Copper and Gold Deposits: A Global Perspective. Adelaide: PCG Publishing, 1998. |
[25] | MUTSCHLER F E, LUDINGTON S, BOOKSTROM A A. Giant porphyry-related metal camps of the world-a database[R]. Tulsa: U.S.Geological Survey, 1999: 99-566. |
[26] |
AGHAZADEH M, HOU Z Q, BADRZADEH Z, et al. Temporal-spatial distribution and tectonic setting of porphyry copper deposits in Iran: Constraints from zircon U-Pb and molybdenite Re-Os geochronology[J]. Ore Geology Reviews, 2015,70:385-406.
DOI URL |
[27] |
TIEPOLO M, TRIBUZIO R. Petrology and U-Pb zircon geochronology of amphibole-rich cumulates with sanukitic affinity fromHusky Ridge (Northern Victoria Land, Antarctica): Insights into the role of amphibole in the petrogenesis of subduction-related magmas[J]. Journal of Petrology, 2008,49:937-970.
DOI URL |
[28] | MCINNES B I A, EVANS N J, BELOUSOVA E, et al. Timing of mineralization and exhumation processes at the Sar Cheshmeh and Meiduk porphyry Cu deposits, Kerman belt, Iran[M]//CSIRO.7th Biennial SGA Meeting. Athens: Millpress Science, 2003: 1197-1200. |
[29] | SHSHSBPOUR J, KRAMERS J D. Lead isotope data from the Sar-Cheshmeh porphyry copper deposit, Iran[J]. Mineralium Deposita, 1987,22(4):278-281. |
[30] | HASSANZADEH J. Metallogenic and tectonomagmatic events in the SE sector of the Cenozoic active continental margin of central Iran (Shahr e Babak area, Kerman Province)[D]. Los Angeles: University of California, 1993: 204. |
[31] |
TAGHIPOUR N, AFTABI A, MATHUR R. Geology and Re-Os geochronology of mineralization of the Miduk porphyry copper deposit, Iran[J]. Resource Geology, 2008,58(2):143-160.
DOI URL |
[32] | GHORBANI M. Economic Geology of Iran, Mineral Deposits and Natural Resources of Iran[M]. Berlin: Springer, 2013. |
[33] | HASSANPOUR Sh. Metallogeny and mineralization of copper and gold in Arasbaran zone (Eastern Azerbaijan)[D]. Shahid: Shahid Beheshti University, Tehran, 2010. |
[34] |
JAMALI H, MEHRABI B. Relationships between arc maturity and Cu-Mo-Au porphyry and related epithermal mineralization at the Cenozoic Arasbaran magmatic belt[J]. Ore Geology Reviews, 2015,65:487-501.
DOI URL |
[35] | YADOLLAHI R, KANANIAN A, MAANIJOU M, et al. Genesis of adakitic magmatism in Masjed Daghi region in Julfa, eastern Azarbaijan[J]. Iranian Journal of Crystallography and Mineralogy, 2011,19:297-310. |
[36] | ROBERT M, JOHANNES M, MARIA O, et al. Major Cu, Au and Mo deposits of the Lesser Caucasus: Products of diverse geodynamic settings[M]//9th Swiss Geoscience Meeting, Mineralogy-Petrology-Geochemistry. Zurich: Swiss Academy of Science, 2011. |
[37] |
AKBARPOUR A, GHOLAMI N, AZIZI H, et al. Cluster and R-mode factor analyses on soil geochemical data of Masjed-Daghi exploration area, northwestern Iran[J]. Arabian Journal of Geosciences, 2012,6(9):3397-3408.
DOI URL |
[38] | FARJANDI F, FAIZIEV A, MOKHTAR F, et al. The application of biogeochemistry for gold exploration in the Masjed-Daghi, Julfa, NW Iran[J]. Arabian Journal of Geosciences, 2013,7(5):1435-1446. |
[39] |
ATALOU S, NAZAFATI N, LOYFI M, et al. Fluid inclusion investigations of the Masjed Daghi copper-gold porphyry-epithermal mineralization, east Azerbaijan province, NW Iran[J]. Open Journal of Geology, 2017,7(8):1110-1127.
DOI URL |
[40] | 彭文世, 刘高魁. 矿物红外光谱图集[M]. 北京: 科学出版社, 1982. |
[41] | 张彦龙, 李兴远. 黄陵花岗岩体长石的XRD、红外光谱特征及其意义[J]. 中山大学研究生学刊(自然科学: 医学版), 2015,36(1):46-56. |
[42] | 罗军燕, 李胜荣, 杨苏明, 等. 石英傅立叶变换漫反射红外光谱在成矿作用研究中的应用——以山西繁峙义兴寨金矿床为例[J]. 矿物岩石, 2009,29(1):27-34. |
[43] | DEER W A, HOWIE R A, ZUSSMAN J. An Introduction to the Rock-forming Minerals[M]. London: The Mineralogical Society, 2013: 248-251. |
[44] |
ZARASVANDI A, HEIDARI M, RAITH J, et al. Geochemical characteristics of collisional and pre-collisional porphyry copper systems in Kerman Cenozoic Magmatic Arc, Iran: Using plagioclase, biotite and amphibole chemistry[J]. Lithos, 2019,326/327:279-297.
DOI URL |
[45] |
ZHOU Y, XU B, HOU Z Q, et al. Petrogenesis of Cenozoic high-Sr/Y shoshonites and associated mafic microgranular enclaves in an intracontinental setting: Implications for porphyry Cu-Au mineralization in western Yunnan, China[J]. Lithos, 2019,324/325:39-54.
DOI URL |
[46] |
MIDDLEMOST E A K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994,37:215-224.
DOI URL |
[47] |
PECCERILLO A, TAYLOR S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976,58:63-81.
DOI URL |
[48] | DEFANT M J, XU J F, KEPEZHINSKAS P, et al. Adakites: Some variations on a theme[J]. Acta Petrologica Sinica, 2002,18(2):129-142. |
[49] |
BISSIG T, CLARK A H, LEE J K W , et al. Petrogenetic and metallogenetic responses to Miocene slab flattening: new constraints from the El Indio-Pascua Au-Ag-Cu belt, Chile/Argentina[J]. Mineralium Deposita, 2003,38(7):844-862.
DOI URL |
[50] | KAY S M, MPODOZIS C, COIRA B. Neogene magmatism, tectonism, and mineral deposits of the Central Andes (22° to 33° S latitude)[M]//SKINNER B J. Geology and Ore Deposits of the Central Andes. Littleton: Society of Economic Geologists, 1999: 27-59. |
[51] |
PERELLO J, CARLOTTO V, ZARATE A, et al. Porphyry-style alteration and mineralization of the Middle Eocene to Early Oligocene Andahuaylas-Yauri Belt, Cuzco Region, Peru[J]. Economic Geology, 2003,98(8):1575-1605.
DOI URL |
[52] |
RICHARDS J P, BOYCE A J, PRINGLE M S. Geologic evolution of the Escondida area, northern Chile: a model for spatial and temporal localization of porphyry cu mineralization[J]. Economic Geology, 2001,96(2):271-306.
DOI URL |
[53] |
SKEWES M A, STERN C R. Genesis of the giant Late Miocene to Pliocene copper deposits of central Chile in the context of Andean magmatic and tectonic evolution[J]. International Geology Review, 1995,37:893-909.
DOI URL |
[54] |
KAY R W, KAY M S. Delamination and delamination magmatism[J]. Tectonophysics, 1993,219(1/3):177-189.
DOI URL |
[55] |
HOU Z Q, ZENG P S, GAO Y F, et al. Himalayan Cu-Mo-Au mineralization in the eastern Indo-Asian collision zone: constraints from Re-Os dating of molybdenite[J]. Mineralium Deposita, 2006,41:33-45.
DOI URL |
[56] |
MOUTHEREAU F, LACOMBE O, VERGE S. Building the Zagros collisional orogen: Timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence[J]. Tectonophysics, 2012,532/535:27-60.
DOI URL |
[57] | ZHANG H R, HOU Z Q, YANG Z M. Metallogenesis and geodynamics of Tethyan metallogenic domain: A review[J]. Mineralium Deposita, 2010,29(1):113-133. |
[58] |
SENGOR A M C, OZEREN M S, KESKIN M, et al. Eastern Turkish high plateau as a small Turkic-type orogen: Implications for post-collisional crust-forming processes in Turkic-type orogens[J]. Earth-Science Reviews, 2008,90:1-48.
DOI URL |
[59] | THIEBLEMONT D, STEIN G, LESCUYER J L. Gisements épithermaux et porphyriques: la connexion adakite Epithermal and porphyry deposits: the adakite connection[J]. Earth and Planetary Sciences, 1997,325(2):103-109. |
[60] | SAJONA F G, MAURY R C. Association of adakites with gold and copper mineralization in the Philippines[J]. Earth and Planetray Sciences, 1998,326(1):27-34. |
[61] |
OYARZUN R, ALVARO MARQUE Z, LILLO J, et al. Giant versus small porphyry copper deposits of Cenozoic age in northern Chile: adakitic versus normal calc-alkaline magmatism[J]. Mineralium Deposita, 2001,36(8):794-798.
DOI URL |
[62] |
MUNGALL J E. Roasting the mantle: Slab melting and the genesis of major Au and Au-rich Cu deposits[J]. Geology, 2002,30(10):915.
DOI URL |
[63] |
SUN W, ZHANG H, LING M X, et al. The genetic association of adakites and Cu-Au ore deposits[J]. International Geology Review, 2010,53(5/6):691-703.
DOI URL |
[64] |
CASTILLO P R, JANNEY P E, SOLIDUM R U. Petrology and geochemistry of Camiguin Island, southern Philippines: insights to the source of adakites and other lavas in a complex arc setting[J]. Contributions to Mineralogy and Petrology, 1999,134(1):33-51.
DOI URL |
[65] |
MACPHERSON C G, DREHER S T, THIRLWALL M F. Adakites without slab melting: High pressure differentiation of island arc magma, Mindanao, the Philippines[J]. Earth and Planetary Science Letters, 2006,243(3/4):581-593.
DOI URL |
[66] |
CHIARADIA M. Adakite-like magmas from fractional crystallization and melting-assimilation of mafic lower crust (Eocene Macuchi arc, Western Cordillera, Ecuador)[J]. Chemical Geology, 2009,265(3/4):468-487.
DOI URL |
[67] |
CHIARADIA M, OTHMAR M, BEATE B, et al. Adakite-like volcanism of Ecuador: lower crust magmatic evolution and recycling[J]. Contributions to Mineralogy and Petrology, 2009,158(5):563-588.
DOI URL |
[68] |
GRIFFIN W L, PEARSON N J, BELOUSOVA E, et al. The Hf isotope composition of cratonic mantle: LAM-MC-ICP-MS analysis of zircon megacrysts in kimberlites[J]. Geochimica et Cosmochimica Acta, 2000,64:133-147.
DOI URL |
[69] | 吴福元, 李献华, 郑永飞, 等. Lu-Hf同位素体系及其岩石学应用[J]. 岩石学报, 2007,23(2):185-220. |
[70] |
TATSUMI Y, HAMILTON D L, NESBITT R W. Chemical characteristics of fluid phase released from a subducted lithosphere and origin of arc magmas: Evidence from high-pressure experiments and natural rocks[J]. Journal of Volcanology and Geothermal Research, 1986,29(1/4):293-309.
DOI URL |
[71] | DAVIDSON J P. Deciphering mantle and crustal signatures in subduction zone magmatism[J]. Geophysical Monograph, 1996,96:251-262. |
[72] |
DE HOOG J C M, MASON P R D, VAN BERGEN M J. Sulfur and chalcophile elements in subduction zones: Constraints from a laser ablation ICP-MS study of melt inclusions from Galunggung Volcano, Indonesia[J]. Geochimica et Cosmochimica Acta, 2001,65:3147-3164.
DOI URL |
[73] |
PEACOCK S M. Large-scale hydration of the lithosphere above subducting slabs[J]. Chemical Geology, 1993,108(1/4):49-59.
DOI URL |
[74] |
ARCULUS R J. Aspects of magma genesis in arcs[J]. Lithos, 1994,33(1/3):189-208.
DOI URL |
[75] | RINGWOOD A E. Petrogenesis in Island Arc Systems[M]//Island Arcs, Deep Sea Trenches and Back-Arc Basins. Washington: Advancing Earth and Space Science, 1977: 311-324. |
[76] |
PERFIT M R, GUST D A, BENCE A E, et al. Chemical characteristics of island-arc basalts: Implications for mantle sources[J]. Chemical Geology, 1980,30:227-256.
DOI URL |
[77] | PEARCE J A. Role of the sub-continental lithosphere in magma genesis at active continental margins[J]. Destructive Plate Margin Magmas, 1983: 230-249. |
[78] |
PLANK T, LANGMUIR C H. An evaluation of the global variations in the major element chemistry of arc basalts[J]. Earth and Planetary Science Letters, 1988,90(4):349-370.
DOI URL |
[79] |
STOLPER E, NEWMAN S. The role of water in the petrogenesis of Mariana trough magmas[J]. Earth and Planetary Science Letters, 1994,121:293-325.
DOI URL |
[80] |
RICHARDS J P. Tectono-magmatic precursors for porphyry Cu (Mo-Au) deposit formation[J]. Economic Geology, 2003,98(8):1515-1533.
DOI URL |
[81] |
VRY V H, WILKINSON J J, SEGUE J, et al. Multistage intrusion, brecciation, and veining at El Teniente, Chile: evolution of a nested porphyry system[J]. Economic Geology, 2010,105(1):119-153.
DOI URL |
[82] |
WILLIAMSON B J, HERRINGTON R J, MORRIS A. Porphyry copper enrichment linked to excess aluminum in plagioclase[J]. Nature Geoscience, 2016,9:237-241.
DOI URL |
[83] | RICHSRDS J P, SHOLEH A. The Tethyan tectonic history and Cu-Au metallogeny of Iran[J]. Society of Economic Geologists, Special Publication, 2016,19:193-212. |
[84] | 侯增谦, 潘小菲, 杨志明, 等. 初论大陆环境斑岩铜矿[J]. 现代地质, 2007,21(2):332-351. |
[85] | ROHRLACH B D, LOUCKS R R. Multi-million-year cyclic ramp-up of volatiles in a lower crustal magma reservoir trapped below the Tampakan copper-gold deposit by Mio-Pliocene crustal compression in the southern Philippines[M]//PORTER T M. Super Porphyry Copper and Gold Deposits—A Global Perspective. Adelaide: PCG Publishing, 2005. |
[86] | LOUCKS R R. Distinctive composition of copper-ore-forming arc magmas[J]. Journal of the Geological Society of Australia, 2014,61(1):5-16. |
[87] |
RICHARDS J P. High Sr/Y arc magmas and porphyry Cu±Mo±Au deposits: just add water[J]. Economic Geology, 2011,106(7):1075-1081.
DOI URL |
[88] |
RICHARDS J P. Magmatic to hydrothermal metal fluxes in convergent and collided margins[J]. Ore Geology Reviews, 2011,40(1):1-26.
DOI URL |
[89] | NANEY M T. Phase equilibria of rock-forming ferromagnesian silicates in granitic systems[J]. American Journal of Sciences, 1983,283(10):993-1033. |
[90] |
RIDOLFI F, RENZULLI A, PUERINI M. Stability and chemical equilibrium of amphibole in calc-alkaline magmas: an overview, new thermobarometric formulations and application to subduction-related volcanoes[J]. Contributions to Mineralogy and Petrology, 2010,160(1):45-66.
DOI URL |
[91] |
BALLHAUS C. Redox states of lithospheric and asthenospheric upper mantle[J]. Contributions to Mineralogy and Petrology, 1993,114(3):331-348.
DOI URL |
[92] |
MOORE G, CARMICHAEL I S E . The hydrous phase equilibria (to 3 kbar) of an andesite and basaltic andesite from western Mexico: constraints on water content and conditions of phenocryst growth[J]. Contributions to Mineralogy and Petrology, 1998,130(3/4):304-319.
DOI URL |
[93] |
MUNTENER O, KELEEMEN P B, GROVE T L. The role of H2O during crystallization of primitive arc magmas under uppermost mantle conditions and genesis of igneous pyroxenites: an experimental study[J]. Contributions to Mineralogy and Petrology, 2001,141(6):643-658.
DOI URL |
[94] |
CLAESON D T, MEURER W P. Fractional crystallization of hydrous basaltic “arc-type” magmas and the formation of amphibole-bearing gabbroic cumulates[J]. Contributions to Mineralogy and Petrology, 2004,147(3):288-304.
DOI URL |
[95] | 陈文明. 论斑岩铜矿的成因[J]. 现代地质, 2002,16(1):1-8. |
[96] |
DAVIDSON J, TURNER S, HANDLEY H, et al. Amphibole “sponge” in arc crust?[J]. Geology, 2007,35(9):787-790.
DOI URL |
[97] |
HOU Z Q, YANG Z M, LU Y J, et al. A genetic linkage between subduction- and collision-related porphyry Cu deposits in continental collision zones[J]. Geology, 2015,43(3):247-250.
DOI URL |
[98] |
WANG R, RICHARDS J P, HOU Z Q, et al. Increased magmatic water content-the key to Oligo-Miocene porphyry Cu-Mo-Au formation in the eastern Gangdese belt, Tibet[J]. Economic Geology, 2014,109(5):1315-1339.
DOI URL |
[99] | 韩吟文, 马振东, 张宏飞, 等. 地球化学[M]. 北京: 地质出版社, 2003: 268-301. |
[100] |
HOU Z Q, ZHOU Y, WANG R, et al. Recycling of metal-fertilized lower continental crust: Origin of non-arc Au-rich porphyry deposits at Cratonic edges[J]. Geology, 2017,45(7):563-566.
DOI URL |
[101] | 鲍新尚, 和文言, 高雪. 滇西北衙金矿床富水岩浆对成矿的制约[J]. 岩石学报, 2017,33(7):2175-2188. |
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