Research Article

Geochronology and Geochemistry of the Karadaban Bimodal Volcanic Rocks in the Altyn Area, Xinjiang: Implications for the Tectonic Evolution of the Altyn Ocean

Table 1

Major (%) and trace element (ppm) data for the volcanic rocks in the northern Altyn Tagh region.

Rock typeBasaltRhyolite
SampleKB-19KB-23KB-70KB-58KB-26KB-33KB-46KB-76KB-81KB-82KB-132KB-138

SiO245.4346.6544.8044.7476.1468.0675.6471.2572.6068.7868.7071.41
TiO21.793.751.572.980.190.410.260.200.320.650.520.23
Al2O317.4214.4615.4816.9312.7911.5910.319.6014.6013.7912.7314.57
TFe2O312.1917.1211.4913.902.078.304.916.862.644.547.503.06
MnO0.480.500.660.640.060.170.050.280.050.170.220.01
MgO8.744.238.637.670.575.212.766.120.861.332.051.33
CaO6.617.8510.591.290.300.130.270.110.171.080.540.35
Na2O3.102.801.773.115.791.280.190.052.464.270.173.99
K2O0.800.181.440.671.271.302.111.223.804.084.562.81
P2O50.240.530.210.650.030.070.030.040.040.100.050.03
LOI3.111.923.356.870.743.423.413.681.871.201.471.68
Total96.8098.0796.6492.5799.2196.5296.5495.7297.5498.7997.0397.79
A/CNK0.970.760.652.071.123.093.336.031.721.032.061.42
A/NK2.923.013.462.901.173.303.966.851.791.212.441.52
Na2O/K2O3.8915.561.234.684.560.980.090.040.651.050.041.42
Rb31.004.9560.5046.7038.7071.40101.0023.80143.00117.00115.0092.70
Ba1012.00194.00981.00888.00618.00214.00396.00458.00935.00862.0014744.00635.00
Th4.875.084.8811.9024.9015.8013.5011.8028.5030.4022.7024.70
U1.261.941.394.418.244.593.653.127.606.886.846.40
Nb11.5011.7010.9013.0019.4018.5018.3022.6026.5016.1025.3024.70
Ta0.640.700.560.821.651.431.341.531.911.541.922.02
K6607.481494.1511953.235520.0710542.0810791.1117514.8010127.0431543.2433867.4837851.8923325.40
Cr188.00174.70197.00215.304.1318.0014.002.464.2610.004.043.40
Ni98.80112.0093.60118.462.049.566.741.071.934.812.172.51
V297.00264.00275.00315.005.3125.1020.308.516.5175.403.084.97
Co50.2035.3053.9067.900.432.571.280.611.249.660.851.70
La24.7025.6027.6043.7061.2051.0045.2047.2056.9046.0059.7066.80
Ce50.1061.5056.7083.60107.00110.0085.1079.8093.1086.20102.00131.00
Pb36.1044.8044.70283.008.484.065.9918.407.3094.5091.006.18
Pr6.2210.007.9312.9015.3013.2010.309.0213.8010.2015.6015.50
Sr370.00394.00460.00144.00107.0032.1026.6022.6075.8080.70322.00104.00
Nd26.7048.5036.5057.0058.1052.4039.0033.0050.4039.7066.5061.40
P1038.702308.71929.592841.15109.11314.23139.66157.11174.57440.79213.85139.66
Sm5.9212.408.1413.7011.8010.507.917.1710.508.1614.8012.30
Zr116.00295.00107.00289.00372.00363.00261.00439.00442.00225.00527.00334.00
Hf3.238.123.037.4011.5010.507.6511.2012.607.8715.7010.30
Eu1.673.502.294.031.251.280.911.051.311.092.221.38
Ti10728.3522475.589409.7817860.601144.762427.361582.281192.701905.933883.783086.651402.48
Gd5.8711.908.1013.0010.509.778.087.6010.008.3714.7011.70
Tb1.082.291.442.421.931.971.771.631.931.612.782.22
Dy6.0913.108.2314.0010.9011.7011.2010.4012.009.2516.2013.00
Y33.2069.7039.0074.5053.9060.4062.3061.1073.7056.4085.0069.40
Ho1.212.621.502.652.202.382.292.172.511.883.222.56
Er3.587.764.157.376.916.626.546.697.875.9410.007.76
Tm0.521.180.591.101.111.020.961.061.270.921.551.18
Yb3.237.313.517.137.576.136.126.918.175.839.957.51
Lu0.491.130.541.031.130.880.841.081.170.871.521.14
ΣREE137.37208.79167.22263.63296.90278.85226.22214.78270.93226.02320.74335.45
LREE115.31161.50139.16214.93254.65238.38188.42177.24226.01191.35260.82288.38
HREE22.0647.2928.0648.7042.2540.4737.8037.5444.9234.6759.9247.07
LREE/HREE5.233.424.964.416.035.894.994.725.035.524.356.13
La/Nb2.152.192.533.363.152.762.472.092.152.862.362.70
La/Ta38.5336.5749.3753.4937.0935.6633.7330.8529.7929.8731.0933.07
LaN/YbN5.492.515.644.405.805.975.304.905.005.664.306.38
δEu0.860.870.850.910.340.380.350.430.390.400.450.35
δCe0.960.940.930.850.831.020.930.890.790.930.800.96

Note: major elements were obtained by X-ray fluorescence spectrometer (XRF) at the Analytical Laboratory of BRIUG, Beijing, using fused lithium-tetraborate glass pellets. The analytical precision as determined on the Chinese national standard GSR-3 was generally around 1–5%. Trace elements were analyzed using a PerkinElmer ELAN-DRC-e ICP-MS at the Analytical Laboratory of BRIUG, Beijing. The powdered samples (50 mg) were dissolved in high-pressure Teflon bombs using a HF+HNO3 mixture for 48 h, at ~195°C. Rh was used as an internal standard to monitor signal drift during counting. The international standards GBPG-1 and OU-6 and the Chinese national standard GSR-3 were used for analytical quality control, with the precision generally better than 5%.