Earth Science Frontiers ›› 2020, Vol. 27 ›› Issue (5): 151-170.DOI: 10.13745/j.esf.sf.2020.5.42
Previous Articles Next Articles
SHEN Junfeng(), LI Shengrong, XU Kexin, WANG Yehan, ZHANG Shiquan, XU Yuanquan, HE Zeyu, CHI Lei, WU Jinchao
Received:
2020-04-25
Revised:
2020-05-20
Online:
2020-09-25
Published:
2020-09-25
CLC Number:
SHEN Junfeng, LI Shengrong, XU Kexin, WANG Yehan, ZHANG Shiquan, XU Yuanquan, HE Zeyu, CHI Lei, WU Jinchao. Uplifting and denudation of the Chifeng-Chaoyang gold ore zone in western Liaoning Province since the Early Cretaceous and the implication[J]. Earth Science Frontiers, 2020, 27(5): 151-170.
Fig.1 The geological map of the north margin of the North China Craton (based on the 2013 1∶5000000 metallogenic domain map of China and the 20151∶2500000 tectonic map of intrusive rocks in China)
样号 | wB/% | |||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SiO2 | Al2O3 | TiO2 | Cr2O3 | Fe2O3 | FeO | MnO | NiO | MgO | CaO | Na2O | K2O | Total | ||||||||||||||||||||||
DS-01 | 36.68 | 15.53 | 2.69 | 0.03 | 3.14 | 14.79 | 0.22 | 0.00 | 10.22 | 0.09 | 0.16 | 9.32 | 93.84 | |||||||||||||||||||||
DS-02 | 37.78 | 15.24 | 3.57 | 0.07 | 3.46 | 14.98 | 0.33 | 0.00 | 9.81 | 0.03 | 0.12 | 9.35 | 94.74 | |||||||||||||||||||||
DS-03 | 37.22 | 14.89 | 3.52 | 0.02 | 3.32 | 14.44 | 0.33 | 0.00 | 9.95 | 0.04 | 0.13 | 9.32 | 94.17 | |||||||||||||||||||||
DS-04 | 37.67 | 15.48 | 2.73 | 0.02 | 3.32 | 14.32 | 0.35 | 0.00 | 10.52 | 0.07 | 0.07 | 9.06 | 93.61 | |||||||||||||||||||||
DS-05 | 37.20 | 15.29 | 2.70 | 0.03 | 3.35 | 14.42 | 0.30 | 0.03 | 9.94 | 0.07 | 0.05 | 8.99 | 92.37 | |||||||||||||||||||||
DS-06 | 36.96 | 14.47 | 2.70 | 0.08 | 3.26 | 14.73 | 0.36 | 0.09 | 10.56 | 0.10 | 0.19 | 8.65 | 94.14 | |||||||||||||||||||||
DS-07 | 36.92 | 14.63 | 3.12 | 0.06 | 3.17 | 16.43 | 0.36 | 0.01 | 10.95 | 0.09 | 0.09 | 9.16 | 95.00 | |||||||||||||||||||||
DS-08 | 37.00 | 14.54 | 3.23 | 0.10 | 3.22 | 16.68 | 0.33 | 0.01 | 10.74 | 0.06 | 0.14 | 9.13 | 95.18 | |||||||||||||||||||||
DS-09 | 37.27 | 15.05 | 2.81 | 0.09 | 3.24 | 15.54 | 0.30 | 0.00 | 10.76 | 0.10 | 0.11 | 9.16 | 94.41 | |||||||||||||||||||||
DS-10 | 37.15 | 14.69 | 3.15 | 0.08 | 3.22 | 16.46 | 0.42 | 0.01 | 10.67 | 0.08 | 0.11 | 9.26 | 95.29 | |||||||||||||||||||||
DS-11 | 37.04 | 14.90 | 2.35 | 0.06 | 2.98 | 15.81 | 0.27 | 0.01 | 11.45 | 0.10 | 0.12 | 9.18 | 94.26 | |||||||||||||||||||||
DS-12 | 39.34 | 14.60 | 4.02 | 0.03 | 2.49 | 8.74 | 0.06 | 0.02 | 16.63 | 0.19 | 0.40 | 7.74 | 94.24 | |||||||||||||||||||||
DS-13 | 37.71 | 13.65 | 4.14 | 0.09 | 2.47 | 9.64 | 0.14 | 0.00 | 15.81 | 0.24 | 0.41 | 8.31 | 92.62 | |||||||||||||||||||||
DS-14 | 37.09 | 14.16 | 4.64 | 0.07 | 2.48 | 9.37 | 0.11 | 0.02 | 15.04 | 0.09 | 0.31 | 8.56 | 91.94 | |||||||||||||||||||||
DS-15 | 39.03 | 14.29 | 4.32 | 0.03 | 2.67 | 9.73 | 0.06 | 0.03 | 15.73 | 0.18 | 0.33 | 8.07 | 94.46 | |||||||||||||||||||||
DS-16 | 37.12 | 14.55 | 4.47 | 0.07 | 2.50 | 11.16 | 0.11 | 0.04 | 15.65 | 0.22 | 0.31 | 8.96 | 95.17 | |||||||||||||||||||||
DS-17 | 37.10 | 14.65 | 3.35 | 0.00 | 3.17 | 14.71 | 0.83 | 0.03 | 10.50 | 0.02 | 0.12 | 9.38 | 93.86 | |||||||||||||||||||||
DS-18 | 37.64 | 14.27 | 3.05 | 0.02 | 3.14 | 13.98 | 0.72 | 0.00 | 11.14 | 0.08 | 0.12 | 9.18 | 93.34 | |||||||||||||||||||||
DS-19 | 37.81 | 15.26 | 3.01 | 0.05 | 3.21 | 13.87 | 1.07 | 0.04 | 10.26 | 0.02 | 0.10 | 9.49 | 94.18 | |||||||||||||||||||||
DS-20 | 36.94 | 14.19 | 3.42 | 0.00 | 3.11 | 13.84 | 0.97 | 0.05 | 10.97 | 0.03 | 0.08 | 9.11 | 92.69 | |||||||||||||||||||||
DS-21 | 37.28 | 14.53 | 3.18 | 0.03 | 3.08 | 15.00 | 0.90 | 0.00 | 11.15 | 0.01 | 0.09 | 9.38 | 94.65 | |||||||||||||||||||||
DS-22 | 37.08 | 15.16 | 3.18 | 0.05 | 3.13 | 14.92 | 0.57 | 0.00 | 11.03 | 0.03 | 0.14 | 9.27 | 94.56 | |||||||||||||||||||||
DS-23 | 37.53 | 15.10 | 3.47 | 0.03 | 3.24 | 13.67 | 0.74 | 0.01 | 10.88 | 0.02 | 0.08 | 9.09 | 93.86 | |||||||||||||||||||||
DS-24 | 37.20 | 15.21 | 3.35 | 0.01 | 3.26 | 14.25 | 0.71 | 0.00 | 10.79 | 0.07 | 0.08 | 9.04 | 93.96 | |||||||||||||||||||||
DS-25 | 36.33 | 14.52 | 3.49 | 0.03 | 3.27 | 13.65 | 0.69 | 0.05 | 10.09 | 0.10 | 0.14 | 8.49 | 90.85 | |||||||||||||||||||||
DS-26 | 36.04 | 14.27 | 3.24 | 0.05 | 3.22 | 14.48 | 0.73 | 0.05 | 10.15 | 0.09 | 0.12 | 8.64 | 91.06 | |||||||||||||||||||||
DM-01 | 36.32 | 14.01 | 5.37 | 0.04 | 3.21 | 13.11 | 0.37 | 0.07 | 11.71 | 0.03 | 0.55 | 7.97 | 92.76 | |||||||||||||||||||||
DM-02 | 36.17 | 13.82 | 5.00 | 0.04 | 3.17 | 13.37 | 0.37 | 0.00 | 11.88 | 0.06 | 0.35 | 8.22 | 92.45 | |||||||||||||||||||||
DM-03 | 35.92 | 13.11 | 4.81 | 0.04 | 3.76 | 17.68 | 0.53 | 0.00 | 8.14 | 0.10 | 0.14 | 8.61 | 92.84 | |||||||||||||||||||||
DM-04 | 37.11 | 15.20 | 2.73 | 0.00 | 3.27 | 16.72 | 0.62 | 0.00 | 10.25 | 0.03 | 0.07 | 9.22 | 95.21 | |||||||||||||||||||||
DM-05 | 37.08 | 14.92 | 2.42 | 0.01 | 3.12 | 16.30 | 0.58 | 0.00 | 10.65 | 0.06 | 0.12 | 9.19 | 94.43 | |||||||||||||||||||||
DM-06 | 36.92 | 15.00 | 2.47 | 0.00 | 3.05 | 16.73 | 0.62 | 0.01 | 10.77 | 0.05 | 0.11 | 9.22 | 94.95 | |||||||||||||||||||||
DM-07 | 36.71 | 14.90 | 2.60 | 0.02 | 3.22 | 16.17 | 0.65 | 0.02 | 10.36 | 0.13 | 0.11 | 8.89 | 93.78 | |||||||||||||||||||||
DM-08 | 37.39 | 14.88 | 2.86 | 0.04 | 3.37 | 16.16 | 0.63 | 0.00 | 10.24 | 0.07 | 0.13 | 8.98 | 94.76 | |||||||||||||||||||||
DM-09 | 37.54 | 12.98 | 4.40 | 0.01 | 3.19 | 13.62 | 0.30 | 0.00 | 12.37 | 0.01 | 0.16 | 8.67 | 93.25 | |||||||||||||||||||||
DM-10 | 38.06 | 12.56 | 4.32 | 0.02 | 3.14 | 13.03 | 0.24 | 0.07 | 12.80 | 0.03 | 0.09 | 8.80 | 93.17 | |||||||||||||||||||||
DM-11 | 36.64 | 12.72 | 4.28 | 0.03 | 3.19 | 13.27 | 0.25 | 0.02 | 11.81 | 0.11 | 0.13 | 8.29 | 90.74 | |||||||||||||||||||||
DM-12 | 36.75 | 12.68 | 4.27 | 0.02 | 3.16 | 13.39 | 0.23 | 0.05 | 11.87 | 0.13 | 0.18 | 8.40 | 91.11 | |||||||||||||||||||||
DM-13 | 35.37 | 12.92 | 5.27 | 0.10 | 2.90 | 10.87 | 0.56 | 0.01 | 13.22 | 0.88 | 0.53 | 6.40 | 89.03 | |||||||||||||||||||||
DM-14 | 35.64 | 13.07 | 5.38 | 0.07 | 2.90 | 10.51 | 0.51 | 0.00 | 13.27 | 0.73 | 0.43 | 6.36 | 88.85 | |||||||||||||||||||||
DM-15 | 36.08 | 12.96 | 5.35 | 0.04 | 2.90 | 10.91 | 0.59 | 0.03 | 13.48 | 1.11 | 0.59 | 6.55 | 90.59 | |||||||||||||||||||||
DM-16 | 36.58 | 12.90 | 5.29 | 0.03 | 2.97 | 11.23 | 0.54 | 0.00 | 13.23 | 0.48 | 0.36 | 7.33 | 90.96 | |||||||||||||||||||||
DM-17 | 36.41 | 12.87 | 5.28 | 0.05 | 2.84 | 11.31 | 0.57 | 0.00 | 13.62 | 0.62 | 0.44 | 7.73 | 91.75 | |||||||||||||||||||||
样号 | 以O=22为基础计算的阳离子数 | |||||||||||||||||||||||||||||||||
Si | Al | Ti | Cr | Fe3+ | Fe2+ | Mn | Ni | Mg | Ca | Na | K | Zn | Total | |||||||||||||||||||||
DS-01 | 5.67 | 2.83 | 0.31 | 0.00 | 0.36 | 1.91 | 0.03 | 0.00 | 2.35 | 0.01 | 0.05 | 1.84 | 0.00 | 15.37 | ||||||||||||||||||||
DS-02 | 5.72 | 2.72 | 0.41 | 0.01 | 0.39 | 1.90 | 0.04 | 0.00 | 2.21 | 0.01 | 0.04 | 1.80 | 0.00 | 15.24 | ||||||||||||||||||||
DS-03 | 5.72 | 2.70 | 0.41 | 0.00 | 0.38 | 1.86 | 0.04 | 0.00 | 2.28 | 0.01 | 0.04 | 1.83 | 0.00 | 15.26 | ||||||||||||||||||||
DS-04 | 5.74 | 2.78 | 0.31 | 0.00 | 0.38 | 1.82 | 0.05 | 0.00 | 2.39 | 0.01 | 0.02 | 1.76 | 0.00 | 15.26 | ||||||||||||||||||||
DS-05 | 5.75 | 2.78 | 0.31 | 0.00 | 0.39 | 1.86 | 0.04 | 0.00 | 2.29 | 0.01 | 0.01 | 1.77 | 0.00 | 15.24 | ||||||||||||||||||||
DS-06 | 5.74 | 2.65 | 0.31 | 0.01 | 0.38 | 1.91 | 0.05 | 0.01 | 2.45 | 0.02 | 0.06 | 1.71 | 0.00 | 15.31 | ||||||||||||||||||||
DS-07 | 5.62 | 2.63 | 0.36 | 0.01 | 0.36 | 2.09 | 0.05 | 0.00 | 2.48 | 0.01 | 0.03 | 1.78 | 0.00 | 15.42 | ||||||||||||||||||||
DS-08 | 5.63 | 2.61 | 0.37 | 0.01 | 0.37 | 2.12 | 0.04 | 0.00 | 2.43 | 0.01 | 0.04 | 1.77 | 0.00 | 15.41 | ||||||||||||||||||||
DS-09 | 5.68 | 2.70 | 0.32 | 0.01 | 0.37 | 1.98 | 0.04 | 0.00 | 2.44 | 0.02 | 0.03 | 1.78 | 0.00 | 15.37 | ||||||||||||||||||||
DS-10 | 5.64 | 2.63 | 0.36 | 0.01 | 0.37 | 2.09 | 0.05 | 0.00 | 2.41 | 0.01 | 0.03 | 1.79 | 0.00 | 15.41 | ||||||||||||||||||||
DS-11 | 5.63 | 2.68 | 0.27 | 0.01 | 0.34 | 2.02 | 0.03 | 0.00 | 2.61 | 0.02 | 0.04 | 1.79 | 0.00 | 15.47 | ||||||||||||||||||||
DS-12 | 5.73 | 2.51 | 0.44 | 0.00 | 0.27 | 1.06 | 0.01 | 0.00 | 3.61 | 0.03 | 0.11 | 1.44 | 0.00 | 15.21 | ||||||||||||||||||||
DS-13 | 5.67 | 2.42 | 0.47 | 0.01 | 0.28 | 1.21 | 0.02 | 0.00 | 3.54 | 0.04 | 0.12 | 1.59 | 0.00 | 15.36 | ||||||||||||||||||||
DS-14 | 5.62 | 2.53 | 0.53 | 0.01 | 0.28 | 1.19 | 0.01 | 0.00 | 3.39 | 0.01 | 0.09 | 1.65 | 0.00 | 15.32 | ||||||||||||||||||||
DS-15 | 5.72 | 2.47 | 0.48 | 0.00 | 0.29 | 1.19 | 0.01 | 0.00 | 3.43 | 0.03 | 0.09 | 1.51 | 0.00 | 15.22 | ||||||||||||||||||||
DS-16 | 5.50 | 2.54 | 0.50 | 0.01 | 0.28 | 1.38 | 0.01 | 0.00 | 3.45 | 0.03 | 0.09 | 1.69 | 0.00 | 15.49 | ||||||||||||||||||||
DS-17 | 5.69 | 2.65 | 0.39 | 0.00 | 0.37 | 1.89 | 0.11 | 0.00 | 2.40 | 0.00 | 0.04 | 1.83 | 0.00 | 15.35 | ||||||||||||||||||||
DS-18 | 5.77 | 2.58 | 0.35 | 0.00 | 0.36 | 1.79 | 0.09 | 0.00 | 2.54 | 0.01 | 0.04 | 1.79 | 0.00 | 15.33 | ||||||||||||||||||||
DS-19 | 5.75 | 2.73 | 0.34 | 0.01 | 0.37 | 1.76 | 0.14 | 0.01 | 2.32 | 0.00 | 0.03 | 1.84 | 0.00 | 15.29 | ||||||||||||||||||||
DS-20 | 5.71 | 2.59 | 0.40 | 0.00 | 0.36 | 1.79 | 0.13 | 0.01 | 2.53 | 0.00 | 0.02 | 1.80 | 0.00 | 15.33 | ||||||||||||||||||||
DS-21 | 5.67 | 2.61 | 0.36 | 0.00 | 0.35 | 1.91 | 0.12 | 0.00 | 2.53 | 0.00 | 0.03 | 1.82 | 0.00 | 15.41 | ||||||||||||||||||||
DS-22 | 5.63 | 2.71 | 0.36 | 0.01 | 0.36 | 1.90 | 0.07 | 0.00 | 2.50 | 0.01 | 0.04 | 1.80 | 0.00 | 15.38 | ||||||||||||||||||||
DS-23 | 5.70 | 2.70 | 0.40 | 0.00 | 0.37 | 1.74 | 0.10 | 0.00 | 2.46 | 0.00 | 0.02 | 1.76 | 0.00 | 15.26 | ||||||||||||||||||||
DS-24 | 5.66 | 2.73 | 0.38 | 0.00 | 0.37 | 1.81 | 0.09 | 0.00 | 2.45 | 0.01 | 0.02 | 1.75 | 0.00 | 15.29 | ||||||||||||||||||||
DS-25 | 5.71 | 2.69 | 0.41 | 0.00 | 0.39 | 1.79 | 0.09 | 0.01 | 2.36 | 0.02 | 0.04 | 1.70 | 0.00 | 15.21 | ||||||||||||||||||||
DS-26 | 5.69 | 2.65 | 0.38 | 0.01 | 0.38 | 1.91 | 0.10 | 0.01 | 2.38 | 0.02 | 0.04 | 1.74 | 0.00 | 15.30 | ||||||||||||||||||||
DM-01 | 5.57 | 2.53 | 0.62 | 0.00 | 0.37 | 1.68 | 0.05 | 0.01 | 2.67 | 0.00 | 0.16 | 1.56 | 0.00 | 15.22 | ||||||||||||||||||||
DM-02 | 5.57 | 2.51 | 0.58 | 0.00 | 0.37 | 1.72 | 0.05 | 0.00 | 2.73 | 0.01 | 0.11 | 1.62 | 0.00 | 15.27 | ||||||||||||||||||||
DM-03 | 5.66 | 2.43 | 0.57 | 0.00 | 0.45 | 2.33 | 0.07 | 0.00 | 1.91 | 0.02 | 0.04 | 1.73 | 0.00 | 15.21 | ||||||||||||||||||||
DM-04 | 5.65 | 2.72 | 0.31 | 0.00 | 0.37 | 2.13 | 0.08 | 0.00 | 2.32 | 0.00 | 0.02 | 1.79 | 0.00 | 15.40 | ||||||||||||||||||||
DM-05 | 5.68 | 2.69 | 0.28 | 0.00 | 0.36 | 2.09 | 0.08 | 0.00 | 2.43 | 0.01 | 0.03 | 1.79 | 0.00 | 15.43 | ||||||||||||||||||||
DM-06 | 5.64 | 2.70 | 0.28 | 0.00 | 0.35 | 2.13 | 0.08 | 0.00 | 2.45 | 0.01 | 0.03 | 1.80 | 0.00 | 15.47 | ||||||||||||||||||||
DM-07 | 5.66 | 2.71 | 0.30 | 0.00 | 0.37 | 2.08 | 0.09 | 0.00 | 2.38 | 0.02 | 0.03 | 1.75 | 0.00 | 15.39 | ||||||||||||||||||||
DM-08 | 5.69 | 2.67 | 0.33 | 0.01 | 0.39 | 2.06 | 0.08 | 0.00 | 2.32 | 0.01 | 0.04 | 1.74 | 0.00 | 15.34 | ||||||||||||||||||||
DM-09 | 5.74 | 2.34 | 0.51 | 0.00 | 0.37 | 1.74 | 0.04 | 0.00 | 2.81 | 0.00 | 0.05 | 1.69 | 0.00 | 15.28 | ||||||||||||||||||||
DM-10 | 5.80 | 2.26 | 0.49 | 0.00 | 0.36 | 1.66 | 0.03 | 0.01 | 2.91 | 0.01 | 0.03 | 1.71 | 0.00 | 15.26 | ||||||||||||||||||||
DM-11 | 5.75 | 2.35 | 0.50 | 0.00 | 0.38 | 1.74 | 0.03 | 0.00 | 2.76 | 0.02 | 0.04 | 1.66 | 0.00 | 15.23 | ||||||||||||||||||||
DM-12 | 5.75 | 2.34 | 0.50 | 0.00 | 0.37 | 1.75 | 0.03 | 0.01 | 2.76 | 0.02 | 0.05 | 1.68 | 0.00 | 15.26 | ||||||||||||||||||||
DM-13 | 5.57 | 2.40 | 0.62 | 0.01 | 0.34 | 1.43 | 0.08 | 0.00 | 3.10 | 0.15 | 0.16 | 1.29 | 0.00 | 15.15 | ||||||||||||||||||||
DM-14 | 5.60 | 2.42 | 0.63 | 0.01 | 0.34 | 1.38 | 0.07 | 0.00 | 3.10 | 0.12 | 0.13 | 1.27 | 0.00 | 15.08 | ||||||||||||||||||||
DM-15 | 5.59 | 2.36 | 0.62 | 0.00 | 0.34 | 1.41 | 0.08 | 0.00 | 3.11 | 0.18 | 0.18 | 1.29 | 0.00 | 15.17 | ||||||||||||||||||||
DM-16 | 5.65 | 2.35 | 0.61 | 0.00 | 0.35 | 1.45 | 0.07 | 0.00 | 3.05 | 0.08 | 0.11 | 1.44 | 0.00 | 15.16 | ||||||||||||||||||||
DM-17 | 5.60 | 2.33 | 0.61 | 0.01 | 0.33 | 1.45 | 0.07 | 0.00 | 3.12 | 0.10 | 0.13 | 1.52 | 0.00 | 15.28 | ||||||||||||||||||||
样号 | AlIV | AlVI | Fe3++AlVI+Ti | Fe2++Mn | Mg/(Fe+Mg) | p/MPa | h/km | |||||||||||||||||||||||||||
DS-01 | 2.33 | 0.5 | 1.17 | 1.94 | 0.55 | 204 | 7.70 | |||||||||||||||||||||||||||
DS-02 | 2.28 | 0.43 | 1.23 | 1.94 | 0.54 | 17 | 6.43 | |||||||||||||||||||||||||||
DS-03 | 2.28 | 0.42 | 1.21 | 1.90 | 0.55 | 164 | 6.22 | |||||||||||||||||||||||||||
DS-04 | 2.26 | 0.52 | 1.21 | 1.87 | 0.57 | 189 | 7.14 | |||||||||||||||||||||||||||
DS-05 | 2.25 | 0.54 | 1.24 | 1.90 | 0.55 | 191 | 7.21 | |||||||||||||||||||||||||||
DS-06 | 2.26 | 0.39 | 1.09 | 1.96 | 0.56 | 15 | 5.66 | |||||||||||||||||||||||||||
DS-07 | 2.38 | 0.25 | 0.97 | 2.14 | 0.54 | 143 | 5.40 | |||||||||||||||||||||||||||
DS-08 | 2.37 | 0.24 | 0.98 | 2.16 | 0.53 | 137 | 5.18 | |||||||||||||||||||||||||||
DS-09 | 2.32 | 0.38 | 1.07 | 2.02 | 0.55 | 165 | 6.25 | |||||||||||||||||||||||||||
DS-10 | 2.36 | 0.27 | 1.00 | 2.14 | 0.54 | 144 | 5.43 | |||||||||||||||||||||||||||
DS-11 | 2.34 | 0.34 | 0.95 | 2.05 | 0.56 | 16 | 6.04 | |||||||||||||||||||||||||||
DS-12 | 2.27 | 0.24 | 0.95 | 1.07 | 0.77 | 106 | 4.02 | |||||||||||||||||||||||||||
DS-13 | 2.33 | 0.09 | 0.83 | 1.23 | 0.74 | 80 | 3.02 | |||||||||||||||||||||||||||
DS-14 | 2.38 | 0.14 | 0.96 | 1.20 | 0.74 | 113 | 4.26 | |||||||||||||||||||||||||||
DS-15 | 2.28 | 0.19 | 0.96 | 1.20 | 0.74 | 94 | 3.57 | |||||||||||||||||||||||||||
DS-16 | 2.50 | 0.03 | 0.81 | 1.40 | 0.71 | 116 | 4.39 | |||||||||||||||||||||||||||
DS-17 | 2.31 | 0.34 | 1.09 | 1.99 | 0.56 | 149 | 5.63 | |||||||||||||||||||||||||||
DS-18 | 2.23 | 0.34 | 1.06 | 1.88 | 0.59 | 128 | 4.82 | |||||||||||||||||||||||||||
DS-19 | 2.25 | 0.48 | 1.19 | 1.90 | 0.57 | 175 | 6.61 | |||||||||||||||||||||||||||
DS-20 | 2.29 | 0.30 | 1.06 | 1.92 | 0.59 | 130 | 4.93 | |||||||||||||||||||||||||||
DS-21 | 2.33 | 0.28 | 1.00 | 2.03 | 0.57 | 137 | 5.17 | |||||||||||||||||||||||||||
DS-22 | 2.37 | 0.35 | 1.07 | 1.97 | 0.57 | 169 | 6.40 | |||||||||||||||||||||||||||
DS-23 | 2.30 | 0.40 | 1.17 | 1.83 | 0.59 | 166 | 6.28 | |||||||||||||||||||||||||||
DS-24 | 2.34 | 0.39 | 1.15 | 1.90 | 0.57 | 174 | 6.57 | |||||||||||||||||||||||||||
DS-25 | 2.29 | 0.40 | 1.20 | 1.88 | 0.57 | 162 | 6.11 | |||||||||||||||||||||||||||
DS-26 | 2.31 | 0.34 | 1.10 | 2.01 | 0.56 | 151 | 5.69 | |||||||||||||||||||||||||||
DM-01 | 2.43 | 0.10 | 1.08 | 1.73 | 0.61 | 113 | 4.28 | |||||||||||||||||||||||||||
DM-02 | 2.43 | 0.08 | 1.03 | 1.77 | 0.61 | 107 | 4.06 | |||||||||||||||||||||||||||
DM-03 | 2.34 | 0.09 | 1.11 | 2.40 | 0.45 | 85 | 3.20 | |||||||||||||||||||||||||||
DM-04 | 2.35 | 0.37 | 1.06 | 2.21 | 0.52 | 173 | 6.52 | |||||||||||||||||||||||||||
DM-05 | 2.32 | 0.37 | 1.01 | 2.16 | 0.54 | 162 | 6.14 | |||||||||||||||||||||||||||
DM-06 | 2.36 | 0.34 | 0.97 | 2.21 | 0.53 | 165 | 6.23 | |||||||||||||||||||||||||||
DM-07 | 2.34 | 0.36 | 1.04 | 2.17 | 0.53 | 167 | 6.31 | |||||||||||||||||||||||||||
DM-08 | 2.31 | 0.37 | 1.08 | 2.14 | 0.53 | 156 | 5.91 | |||||||||||||||||||||||||||
DM-09 | 2.26 | 0.07 | 0.94 | 1.78 | 0.62 | 55 | 2.07 | |||||||||||||||||||||||||||
DM-10 | 2.20 | 0.06 | 0.91 | 1.69 | 0.64 | 30 | 1.15 | |||||||||||||||||||||||||||
DM-11 | 2.25 | 0.10 | 0.98 | 1.77 | 0.61 | 59 | 2.24 | |||||||||||||||||||||||||||
DM-12 | 2.25 | 0.08 | 0.96 | 1.78 | 0.61 | 55 | 2.07 | |||||||||||||||||||||||||||
DM-13 | 2.43 | -0.03 | 0.94 | 1.51 | 0.68 | 74 | 2.78 | |||||||||||||||||||||||||||
DM-14 | 2.40 | 0.02 | 1.00 | 1.45 | 0.69 | 80 | 3.02 | |||||||||||||||||||||||||||
DM-15 | 2.41 | -0.05 | 0.91 | 1.49 | 0.69 | 63 | 2.39 | |||||||||||||||||||||||||||
DM-16 | 2.35 | 0.00 | 0.96 | 1.52 | 0.68 | 59 | 2.22 | |||||||||||||||||||||||||||
DM-17 | 2.40 | -0.07 | 0.87 | 1.53 | 0.68 | 54 | 2.02 |
Table 1 Compositions of biotite in the Duimiangou and Dashitougou pluton
样号 | wB/% | |||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SiO2 | Al2O3 | TiO2 | Cr2O3 | Fe2O3 | FeO | MnO | NiO | MgO | CaO | Na2O | K2O | Total | ||||||||||||||||||||||
DS-01 | 36.68 | 15.53 | 2.69 | 0.03 | 3.14 | 14.79 | 0.22 | 0.00 | 10.22 | 0.09 | 0.16 | 9.32 | 93.84 | |||||||||||||||||||||
DS-02 | 37.78 | 15.24 | 3.57 | 0.07 | 3.46 | 14.98 | 0.33 | 0.00 | 9.81 | 0.03 | 0.12 | 9.35 | 94.74 | |||||||||||||||||||||
DS-03 | 37.22 | 14.89 | 3.52 | 0.02 | 3.32 | 14.44 | 0.33 | 0.00 | 9.95 | 0.04 | 0.13 | 9.32 | 94.17 | |||||||||||||||||||||
DS-04 | 37.67 | 15.48 | 2.73 | 0.02 | 3.32 | 14.32 | 0.35 | 0.00 | 10.52 | 0.07 | 0.07 | 9.06 | 93.61 | |||||||||||||||||||||
DS-05 | 37.20 | 15.29 | 2.70 | 0.03 | 3.35 | 14.42 | 0.30 | 0.03 | 9.94 | 0.07 | 0.05 | 8.99 | 92.37 | |||||||||||||||||||||
DS-06 | 36.96 | 14.47 | 2.70 | 0.08 | 3.26 | 14.73 | 0.36 | 0.09 | 10.56 | 0.10 | 0.19 | 8.65 | 94.14 | |||||||||||||||||||||
DS-07 | 36.92 | 14.63 | 3.12 | 0.06 | 3.17 | 16.43 | 0.36 | 0.01 | 10.95 | 0.09 | 0.09 | 9.16 | 95.00 | |||||||||||||||||||||
DS-08 | 37.00 | 14.54 | 3.23 | 0.10 | 3.22 | 16.68 | 0.33 | 0.01 | 10.74 | 0.06 | 0.14 | 9.13 | 95.18 | |||||||||||||||||||||
DS-09 | 37.27 | 15.05 | 2.81 | 0.09 | 3.24 | 15.54 | 0.30 | 0.00 | 10.76 | 0.10 | 0.11 | 9.16 | 94.41 | |||||||||||||||||||||
DS-10 | 37.15 | 14.69 | 3.15 | 0.08 | 3.22 | 16.46 | 0.42 | 0.01 | 10.67 | 0.08 | 0.11 | 9.26 | 95.29 | |||||||||||||||||||||
DS-11 | 37.04 | 14.90 | 2.35 | 0.06 | 2.98 | 15.81 | 0.27 | 0.01 | 11.45 | 0.10 | 0.12 | 9.18 | 94.26 | |||||||||||||||||||||
DS-12 | 39.34 | 14.60 | 4.02 | 0.03 | 2.49 | 8.74 | 0.06 | 0.02 | 16.63 | 0.19 | 0.40 | 7.74 | 94.24 | |||||||||||||||||||||
DS-13 | 37.71 | 13.65 | 4.14 | 0.09 | 2.47 | 9.64 | 0.14 | 0.00 | 15.81 | 0.24 | 0.41 | 8.31 | 92.62 | |||||||||||||||||||||
DS-14 | 37.09 | 14.16 | 4.64 | 0.07 | 2.48 | 9.37 | 0.11 | 0.02 | 15.04 | 0.09 | 0.31 | 8.56 | 91.94 | |||||||||||||||||||||
DS-15 | 39.03 | 14.29 | 4.32 | 0.03 | 2.67 | 9.73 | 0.06 | 0.03 | 15.73 | 0.18 | 0.33 | 8.07 | 94.46 | |||||||||||||||||||||
DS-16 | 37.12 | 14.55 | 4.47 | 0.07 | 2.50 | 11.16 | 0.11 | 0.04 | 15.65 | 0.22 | 0.31 | 8.96 | 95.17 | |||||||||||||||||||||
DS-17 | 37.10 | 14.65 | 3.35 | 0.00 | 3.17 | 14.71 | 0.83 | 0.03 | 10.50 | 0.02 | 0.12 | 9.38 | 93.86 | |||||||||||||||||||||
DS-18 | 37.64 | 14.27 | 3.05 | 0.02 | 3.14 | 13.98 | 0.72 | 0.00 | 11.14 | 0.08 | 0.12 | 9.18 | 93.34 | |||||||||||||||||||||
DS-19 | 37.81 | 15.26 | 3.01 | 0.05 | 3.21 | 13.87 | 1.07 | 0.04 | 10.26 | 0.02 | 0.10 | 9.49 | 94.18 | |||||||||||||||||||||
DS-20 | 36.94 | 14.19 | 3.42 | 0.00 | 3.11 | 13.84 | 0.97 | 0.05 | 10.97 | 0.03 | 0.08 | 9.11 | 92.69 | |||||||||||||||||||||
DS-21 | 37.28 | 14.53 | 3.18 | 0.03 | 3.08 | 15.00 | 0.90 | 0.00 | 11.15 | 0.01 | 0.09 | 9.38 | 94.65 | |||||||||||||||||||||
DS-22 | 37.08 | 15.16 | 3.18 | 0.05 | 3.13 | 14.92 | 0.57 | 0.00 | 11.03 | 0.03 | 0.14 | 9.27 | 94.56 | |||||||||||||||||||||
DS-23 | 37.53 | 15.10 | 3.47 | 0.03 | 3.24 | 13.67 | 0.74 | 0.01 | 10.88 | 0.02 | 0.08 | 9.09 | 93.86 | |||||||||||||||||||||
DS-24 | 37.20 | 15.21 | 3.35 | 0.01 | 3.26 | 14.25 | 0.71 | 0.00 | 10.79 | 0.07 | 0.08 | 9.04 | 93.96 | |||||||||||||||||||||
DS-25 | 36.33 | 14.52 | 3.49 | 0.03 | 3.27 | 13.65 | 0.69 | 0.05 | 10.09 | 0.10 | 0.14 | 8.49 | 90.85 | |||||||||||||||||||||
DS-26 | 36.04 | 14.27 | 3.24 | 0.05 | 3.22 | 14.48 | 0.73 | 0.05 | 10.15 | 0.09 | 0.12 | 8.64 | 91.06 | |||||||||||||||||||||
DM-01 | 36.32 | 14.01 | 5.37 | 0.04 | 3.21 | 13.11 | 0.37 | 0.07 | 11.71 | 0.03 | 0.55 | 7.97 | 92.76 | |||||||||||||||||||||
DM-02 | 36.17 | 13.82 | 5.00 | 0.04 | 3.17 | 13.37 | 0.37 | 0.00 | 11.88 | 0.06 | 0.35 | 8.22 | 92.45 | |||||||||||||||||||||
DM-03 | 35.92 | 13.11 | 4.81 | 0.04 | 3.76 | 17.68 | 0.53 | 0.00 | 8.14 | 0.10 | 0.14 | 8.61 | 92.84 | |||||||||||||||||||||
DM-04 | 37.11 | 15.20 | 2.73 | 0.00 | 3.27 | 16.72 | 0.62 | 0.00 | 10.25 | 0.03 | 0.07 | 9.22 | 95.21 | |||||||||||||||||||||
DM-05 | 37.08 | 14.92 | 2.42 | 0.01 | 3.12 | 16.30 | 0.58 | 0.00 | 10.65 | 0.06 | 0.12 | 9.19 | 94.43 | |||||||||||||||||||||
DM-06 | 36.92 | 15.00 | 2.47 | 0.00 | 3.05 | 16.73 | 0.62 | 0.01 | 10.77 | 0.05 | 0.11 | 9.22 | 94.95 | |||||||||||||||||||||
DM-07 | 36.71 | 14.90 | 2.60 | 0.02 | 3.22 | 16.17 | 0.65 | 0.02 | 10.36 | 0.13 | 0.11 | 8.89 | 93.78 | |||||||||||||||||||||
DM-08 | 37.39 | 14.88 | 2.86 | 0.04 | 3.37 | 16.16 | 0.63 | 0.00 | 10.24 | 0.07 | 0.13 | 8.98 | 94.76 | |||||||||||||||||||||
DM-09 | 37.54 | 12.98 | 4.40 | 0.01 | 3.19 | 13.62 | 0.30 | 0.00 | 12.37 | 0.01 | 0.16 | 8.67 | 93.25 | |||||||||||||||||||||
DM-10 | 38.06 | 12.56 | 4.32 | 0.02 | 3.14 | 13.03 | 0.24 | 0.07 | 12.80 | 0.03 | 0.09 | 8.80 | 93.17 | |||||||||||||||||||||
DM-11 | 36.64 | 12.72 | 4.28 | 0.03 | 3.19 | 13.27 | 0.25 | 0.02 | 11.81 | 0.11 | 0.13 | 8.29 | 90.74 | |||||||||||||||||||||
DM-12 | 36.75 | 12.68 | 4.27 | 0.02 | 3.16 | 13.39 | 0.23 | 0.05 | 11.87 | 0.13 | 0.18 | 8.40 | 91.11 | |||||||||||||||||||||
DM-13 | 35.37 | 12.92 | 5.27 | 0.10 | 2.90 | 10.87 | 0.56 | 0.01 | 13.22 | 0.88 | 0.53 | 6.40 | 89.03 | |||||||||||||||||||||
DM-14 | 35.64 | 13.07 | 5.38 | 0.07 | 2.90 | 10.51 | 0.51 | 0.00 | 13.27 | 0.73 | 0.43 | 6.36 | 88.85 | |||||||||||||||||||||
DM-15 | 36.08 | 12.96 | 5.35 | 0.04 | 2.90 | 10.91 | 0.59 | 0.03 | 13.48 | 1.11 | 0.59 | 6.55 | 90.59 | |||||||||||||||||||||
DM-16 | 36.58 | 12.90 | 5.29 | 0.03 | 2.97 | 11.23 | 0.54 | 0.00 | 13.23 | 0.48 | 0.36 | 7.33 | 90.96 | |||||||||||||||||||||
DM-17 | 36.41 | 12.87 | 5.28 | 0.05 | 2.84 | 11.31 | 0.57 | 0.00 | 13.62 | 0.62 | 0.44 | 7.73 | 91.75 | |||||||||||||||||||||
样号 | 以O=22为基础计算的阳离子数 | |||||||||||||||||||||||||||||||||
Si | Al | Ti | Cr | Fe3+ | Fe2+ | Mn | Ni | Mg | Ca | Na | K | Zn | Total | |||||||||||||||||||||
DS-01 | 5.67 | 2.83 | 0.31 | 0.00 | 0.36 | 1.91 | 0.03 | 0.00 | 2.35 | 0.01 | 0.05 | 1.84 | 0.00 | 15.37 | ||||||||||||||||||||
DS-02 | 5.72 | 2.72 | 0.41 | 0.01 | 0.39 | 1.90 | 0.04 | 0.00 | 2.21 | 0.01 | 0.04 | 1.80 | 0.00 | 15.24 | ||||||||||||||||||||
DS-03 | 5.72 | 2.70 | 0.41 | 0.00 | 0.38 | 1.86 | 0.04 | 0.00 | 2.28 | 0.01 | 0.04 | 1.83 | 0.00 | 15.26 | ||||||||||||||||||||
DS-04 | 5.74 | 2.78 | 0.31 | 0.00 | 0.38 | 1.82 | 0.05 | 0.00 | 2.39 | 0.01 | 0.02 | 1.76 | 0.00 | 15.26 | ||||||||||||||||||||
DS-05 | 5.75 | 2.78 | 0.31 | 0.00 | 0.39 | 1.86 | 0.04 | 0.00 | 2.29 | 0.01 | 0.01 | 1.77 | 0.00 | 15.24 | ||||||||||||||||||||
DS-06 | 5.74 | 2.65 | 0.31 | 0.01 | 0.38 | 1.91 | 0.05 | 0.01 | 2.45 | 0.02 | 0.06 | 1.71 | 0.00 | 15.31 | ||||||||||||||||||||
DS-07 | 5.62 | 2.63 | 0.36 | 0.01 | 0.36 | 2.09 | 0.05 | 0.00 | 2.48 | 0.01 | 0.03 | 1.78 | 0.00 | 15.42 | ||||||||||||||||||||
DS-08 | 5.63 | 2.61 | 0.37 | 0.01 | 0.37 | 2.12 | 0.04 | 0.00 | 2.43 | 0.01 | 0.04 | 1.77 | 0.00 | 15.41 | ||||||||||||||||||||
DS-09 | 5.68 | 2.70 | 0.32 | 0.01 | 0.37 | 1.98 | 0.04 | 0.00 | 2.44 | 0.02 | 0.03 | 1.78 | 0.00 | 15.37 | ||||||||||||||||||||
DS-10 | 5.64 | 2.63 | 0.36 | 0.01 | 0.37 | 2.09 | 0.05 | 0.00 | 2.41 | 0.01 | 0.03 | 1.79 | 0.00 | 15.41 | ||||||||||||||||||||
DS-11 | 5.63 | 2.68 | 0.27 | 0.01 | 0.34 | 2.02 | 0.03 | 0.00 | 2.61 | 0.02 | 0.04 | 1.79 | 0.00 | 15.47 | ||||||||||||||||||||
DS-12 | 5.73 | 2.51 | 0.44 | 0.00 | 0.27 | 1.06 | 0.01 | 0.00 | 3.61 | 0.03 | 0.11 | 1.44 | 0.00 | 15.21 | ||||||||||||||||||||
DS-13 | 5.67 | 2.42 | 0.47 | 0.01 | 0.28 | 1.21 | 0.02 | 0.00 | 3.54 | 0.04 | 0.12 | 1.59 | 0.00 | 15.36 | ||||||||||||||||||||
DS-14 | 5.62 | 2.53 | 0.53 | 0.01 | 0.28 | 1.19 | 0.01 | 0.00 | 3.39 | 0.01 | 0.09 | 1.65 | 0.00 | 15.32 | ||||||||||||||||||||
DS-15 | 5.72 | 2.47 | 0.48 | 0.00 | 0.29 | 1.19 | 0.01 | 0.00 | 3.43 | 0.03 | 0.09 | 1.51 | 0.00 | 15.22 | ||||||||||||||||||||
DS-16 | 5.50 | 2.54 | 0.50 | 0.01 | 0.28 | 1.38 | 0.01 | 0.00 | 3.45 | 0.03 | 0.09 | 1.69 | 0.00 | 15.49 | ||||||||||||||||||||
DS-17 | 5.69 | 2.65 | 0.39 | 0.00 | 0.37 | 1.89 | 0.11 | 0.00 | 2.40 | 0.00 | 0.04 | 1.83 | 0.00 | 15.35 | ||||||||||||||||||||
DS-18 | 5.77 | 2.58 | 0.35 | 0.00 | 0.36 | 1.79 | 0.09 | 0.00 | 2.54 | 0.01 | 0.04 | 1.79 | 0.00 | 15.33 | ||||||||||||||||||||
DS-19 | 5.75 | 2.73 | 0.34 | 0.01 | 0.37 | 1.76 | 0.14 | 0.01 | 2.32 | 0.00 | 0.03 | 1.84 | 0.00 | 15.29 | ||||||||||||||||||||
DS-20 | 5.71 | 2.59 | 0.40 | 0.00 | 0.36 | 1.79 | 0.13 | 0.01 | 2.53 | 0.00 | 0.02 | 1.80 | 0.00 | 15.33 | ||||||||||||||||||||
DS-21 | 5.67 | 2.61 | 0.36 | 0.00 | 0.35 | 1.91 | 0.12 | 0.00 | 2.53 | 0.00 | 0.03 | 1.82 | 0.00 | 15.41 | ||||||||||||||||||||
DS-22 | 5.63 | 2.71 | 0.36 | 0.01 | 0.36 | 1.90 | 0.07 | 0.00 | 2.50 | 0.01 | 0.04 | 1.80 | 0.00 | 15.38 | ||||||||||||||||||||
DS-23 | 5.70 | 2.70 | 0.40 | 0.00 | 0.37 | 1.74 | 0.10 | 0.00 | 2.46 | 0.00 | 0.02 | 1.76 | 0.00 | 15.26 | ||||||||||||||||||||
DS-24 | 5.66 | 2.73 | 0.38 | 0.00 | 0.37 | 1.81 | 0.09 | 0.00 | 2.45 | 0.01 | 0.02 | 1.75 | 0.00 | 15.29 | ||||||||||||||||||||
DS-25 | 5.71 | 2.69 | 0.41 | 0.00 | 0.39 | 1.79 | 0.09 | 0.01 | 2.36 | 0.02 | 0.04 | 1.70 | 0.00 | 15.21 | ||||||||||||||||||||
DS-26 | 5.69 | 2.65 | 0.38 | 0.01 | 0.38 | 1.91 | 0.10 | 0.01 | 2.38 | 0.02 | 0.04 | 1.74 | 0.00 | 15.30 | ||||||||||||||||||||
DM-01 | 5.57 | 2.53 | 0.62 | 0.00 | 0.37 | 1.68 | 0.05 | 0.01 | 2.67 | 0.00 | 0.16 | 1.56 | 0.00 | 15.22 | ||||||||||||||||||||
DM-02 | 5.57 | 2.51 | 0.58 | 0.00 | 0.37 | 1.72 | 0.05 | 0.00 | 2.73 | 0.01 | 0.11 | 1.62 | 0.00 | 15.27 | ||||||||||||||||||||
DM-03 | 5.66 | 2.43 | 0.57 | 0.00 | 0.45 | 2.33 | 0.07 | 0.00 | 1.91 | 0.02 | 0.04 | 1.73 | 0.00 | 15.21 | ||||||||||||||||||||
DM-04 | 5.65 | 2.72 | 0.31 | 0.00 | 0.37 | 2.13 | 0.08 | 0.00 | 2.32 | 0.00 | 0.02 | 1.79 | 0.00 | 15.40 | ||||||||||||||||||||
DM-05 | 5.68 | 2.69 | 0.28 | 0.00 | 0.36 | 2.09 | 0.08 | 0.00 | 2.43 | 0.01 | 0.03 | 1.79 | 0.00 | 15.43 | ||||||||||||||||||||
DM-06 | 5.64 | 2.70 | 0.28 | 0.00 | 0.35 | 2.13 | 0.08 | 0.00 | 2.45 | 0.01 | 0.03 | 1.80 | 0.00 | 15.47 | ||||||||||||||||||||
DM-07 | 5.66 | 2.71 | 0.30 | 0.00 | 0.37 | 2.08 | 0.09 | 0.00 | 2.38 | 0.02 | 0.03 | 1.75 | 0.00 | 15.39 | ||||||||||||||||||||
DM-08 | 5.69 | 2.67 | 0.33 | 0.01 | 0.39 | 2.06 | 0.08 | 0.00 | 2.32 | 0.01 | 0.04 | 1.74 | 0.00 | 15.34 | ||||||||||||||||||||
DM-09 | 5.74 | 2.34 | 0.51 | 0.00 | 0.37 | 1.74 | 0.04 | 0.00 | 2.81 | 0.00 | 0.05 | 1.69 | 0.00 | 15.28 | ||||||||||||||||||||
DM-10 | 5.80 | 2.26 | 0.49 | 0.00 | 0.36 | 1.66 | 0.03 | 0.01 | 2.91 | 0.01 | 0.03 | 1.71 | 0.00 | 15.26 | ||||||||||||||||||||
DM-11 | 5.75 | 2.35 | 0.50 | 0.00 | 0.38 | 1.74 | 0.03 | 0.00 | 2.76 | 0.02 | 0.04 | 1.66 | 0.00 | 15.23 | ||||||||||||||||||||
DM-12 | 5.75 | 2.34 | 0.50 | 0.00 | 0.37 | 1.75 | 0.03 | 0.01 | 2.76 | 0.02 | 0.05 | 1.68 | 0.00 | 15.26 | ||||||||||||||||||||
DM-13 | 5.57 | 2.40 | 0.62 | 0.01 | 0.34 | 1.43 | 0.08 | 0.00 | 3.10 | 0.15 | 0.16 | 1.29 | 0.00 | 15.15 | ||||||||||||||||||||
DM-14 | 5.60 | 2.42 | 0.63 | 0.01 | 0.34 | 1.38 | 0.07 | 0.00 | 3.10 | 0.12 | 0.13 | 1.27 | 0.00 | 15.08 | ||||||||||||||||||||
DM-15 | 5.59 | 2.36 | 0.62 | 0.00 | 0.34 | 1.41 | 0.08 | 0.00 | 3.11 | 0.18 | 0.18 | 1.29 | 0.00 | 15.17 | ||||||||||||||||||||
DM-16 | 5.65 | 2.35 | 0.61 | 0.00 | 0.35 | 1.45 | 0.07 | 0.00 | 3.05 | 0.08 | 0.11 | 1.44 | 0.00 | 15.16 | ||||||||||||||||||||
DM-17 | 5.60 | 2.33 | 0.61 | 0.01 | 0.33 | 1.45 | 0.07 | 0.00 | 3.12 | 0.10 | 0.13 | 1.52 | 0.00 | 15.28 | ||||||||||||||||||||
样号 | AlIV | AlVI | Fe3++AlVI+Ti | Fe2++Mn | Mg/(Fe+Mg) | p/MPa | h/km | |||||||||||||||||||||||||||
DS-01 | 2.33 | 0.5 | 1.17 | 1.94 | 0.55 | 204 | 7.70 | |||||||||||||||||||||||||||
DS-02 | 2.28 | 0.43 | 1.23 | 1.94 | 0.54 | 17 | 6.43 | |||||||||||||||||||||||||||
DS-03 | 2.28 | 0.42 | 1.21 | 1.90 | 0.55 | 164 | 6.22 | |||||||||||||||||||||||||||
DS-04 | 2.26 | 0.52 | 1.21 | 1.87 | 0.57 | 189 | 7.14 | |||||||||||||||||||||||||||
DS-05 | 2.25 | 0.54 | 1.24 | 1.90 | 0.55 | 191 | 7.21 | |||||||||||||||||||||||||||
DS-06 | 2.26 | 0.39 | 1.09 | 1.96 | 0.56 | 15 | 5.66 | |||||||||||||||||||||||||||
DS-07 | 2.38 | 0.25 | 0.97 | 2.14 | 0.54 | 143 | 5.40 | |||||||||||||||||||||||||||
DS-08 | 2.37 | 0.24 | 0.98 | 2.16 | 0.53 | 137 | 5.18 | |||||||||||||||||||||||||||
DS-09 | 2.32 | 0.38 | 1.07 | 2.02 | 0.55 | 165 | 6.25 | |||||||||||||||||||||||||||
DS-10 | 2.36 | 0.27 | 1.00 | 2.14 | 0.54 | 144 | 5.43 | |||||||||||||||||||||||||||
DS-11 | 2.34 | 0.34 | 0.95 | 2.05 | 0.56 | 16 | 6.04 | |||||||||||||||||||||||||||
DS-12 | 2.27 | 0.24 | 0.95 | 1.07 | 0.77 | 106 | 4.02 | |||||||||||||||||||||||||||
DS-13 | 2.33 | 0.09 | 0.83 | 1.23 | 0.74 | 80 | 3.02 | |||||||||||||||||||||||||||
DS-14 | 2.38 | 0.14 | 0.96 | 1.20 | 0.74 | 113 | 4.26 | |||||||||||||||||||||||||||
DS-15 | 2.28 | 0.19 | 0.96 | 1.20 | 0.74 | 94 | 3.57 | |||||||||||||||||||||||||||
DS-16 | 2.50 | 0.03 | 0.81 | 1.40 | 0.71 | 116 | 4.39 | |||||||||||||||||||||||||||
DS-17 | 2.31 | 0.34 | 1.09 | 1.99 | 0.56 | 149 | 5.63 | |||||||||||||||||||||||||||
DS-18 | 2.23 | 0.34 | 1.06 | 1.88 | 0.59 | 128 | 4.82 | |||||||||||||||||||||||||||
DS-19 | 2.25 | 0.48 | 1.19 | 1.90 | 0.57 | 175 | 6.61 | |||||||||||||||||||||||||||
DS-20 | 2.29 | 0.30 | 1.06 | 1.92 | 0.59 | 130 | 4.93 | |||||||||||||||||||||||||||
DS-21 | 2.33 | 0.28 | 1.00 | 2.03 | 0.57 | 137 | 5.17 | |||||||||||||||||||||||||||
DS-22 | 2.37 | 0.35 | 1.07 | 1.97 | 0.57 | 169 | 6.40 | |||||||||||||||||||||||||||
DS-23 | 2.30 | 0.40 | 1.17 | 1.83 | 0.59 | 166 | 6.28 | |||||||||||||||||||||||||||
DS-24 | 2.34 | 0.39 | 1.15 | 1.90 | 0.57 | 174 | 6.57 | |||||||||||||||||||||||||||
DS-25 | 2.29 | 0.40 | 1.20 | 1.88 | 0.57 | 162 | 6.11 | |||||||||||||||||||||||||||
DS-26 | 2.31 | 0.34 | 1.10 | 2.01 | 0.56 | 151 | 5.69 | |||||||||||||||||||||||||||
DM-01 | 2.43 | 0.10 | 1.08 | 1.73 | 0.61 | 113 | 4.28 | |||||||||||||||||||||||||||
DM-02 | 2.43 | 0.08 | 1.03 | 1.77 | 0.61 | 107 | 4.06 | |||||||||||||||||||||||||||
DM-03 | 2.34 | 0.09 | 1.11 | 2.40 | 0.45 | 85 | 3.20 | |||||||||||||||||||||||||||
DM-04 | 2.35 | 0.37 | 1.06 | 2.21 | 0.52 | 173 | 6.52 | |||||||||||||||||||||||||||
DM-05 | 2.32 | 0.37 | 1.01 | 2.16 | 0.54 | 162 | 6.14 | |||||||||||||||||||||||||||
DM-06 | 2.36 | 0.34 | 0.97 | 2.21 | 0.53 | 165 | 6.23 | |||||||||||||||||||||||||||
DM-07 | 2.34 | 0.36 | 1.04 | 2.17 | 0.53 | 167 | 6.31 | |||||||||||||||||||||||||||
DM-08 | 2.31 | 0.37 | 1.08 | 2.14 | 0.53 | 156 | 5.91 | |||||||||||||||||||||||||||
DM-09 | 2.26 | 0.07 | 0.94 | 1.78 | 0.62 | 55 | 2.07 | |||||||||||||||||||||||||||
DM-10 | 2.20 | 0.06 | 0.91 | 1.69 | 0.64 | 30 | 1.15 | |||||||||||||||||||||||||||
DM-11 | 2.25 | 0.10 | 0.98 | 1.77 | 0.61 | 59 | 2.24 | |||||||||||||||||||||||||||
DM-12 | 2.25 | 0.08 | 0.96 | 1.78 | 0.61 | 55 | 2.07 | |||||||||||||||||||||||||||
DM-13 | 2.43 | -0.03 | 0.94 | 1.51 | 0.68 | 74 | 2.78 | |||||||||||||||||||||||||||
DM-14 | 2.40 | 0.02 | 1.00 | 1.45 | 0.69 | 80 | 3.02 | |||||||||||||||||||||||||||
DM-15 | 2.41 | -0.05 | 0.91 | 1.49 | 0.69 | 63 | 2.39 | |||||||||||||||||||||||||||
DM-16 | 2.35 | 0.00 | 0.96 | 1.52 | 0.68 | 59 | 2.22 | |||||||||||||||||||||||||||
DM-17 | 2.40 | -0.07 | 0.87 | 1.53 | 0.68 | 54 | 2.02 |
[1] | 朱日祥, 徐义刚, 朱光, 等. 华北克拉通破坏[J]. 中国科学: 地球科学, 2012, 42(8):1135-1159. |
[2] | 吴福元, 徐义刚, 朱日祥, 等. 克拉通岩石圈减薄与破坏[J]. 中国科学: 地球科学, 2014, 44(11):2358-2372. |
[3] | 朱日祥, “华北克拉通破坏”重大研究计划结题综述[J]. 中国科学基金, 2018(3):282-290. |
[4] | XU Y G, HUANG X L, MA J L, et al. Crust-mantle interaction during the tectono-thermal reactivation of the North China Craton: constraints from SHRIMP zircon U-Pb chronology and geochemistry of Mesozoic plutons from western Shandong[J]. Contributions to Mineralogy and Petrology, 2004, 147:750-767. |
[5] | 路凤香, 郑建平, 邵济安, 等. 华北东部中生代晚期—新生代软流圈上涌与岩石圈减薄[J]. 地学前缘, 2006, 13(2):86-92. |
[6] | 徐义刚, 李洪颜, 庞崇进, 等. 论华北克拉通破坏的时限[J]. 中国科学: 地球科学, 2009, 4(14):1974-1989. |
[7] | YANG J H, SUN J F, CHEN F K, et al. Sources and petrogenesis of late Triassic dolerite dikes in the Liaodong Peninsula: implications for post-collisional lithosphere thinning of eastern North China Craton[J]. Journal of Petrology, 2007, 48:1973-1997. |
[8] | JIANG N, LIU Y, ZHOU W, et al. Derivation of Mesozoic adakitic magmas from ancient lower crust in the North China craton[J]. Geochimica et Cosmochimica Acta, 2007, 71:2591-2608. |
[9] | 朱日祥, 徐义刚. 西太平洋板块俯冲与华北克拉通破坏[J]. 中国科学: 地球科学, 2019, 49(9):1346-1356. |
[10] | ZHU R X, YANG J H, WU F Y. Timing of destruction of the North China Craton[J]. Lithos, 2012, 149:51-60. |
[11] | YANG J H, WU F Y, CHUNG S L, et al. Rapid exhumation and cooling of the Liaonan metamorphic core complex: inferences from 40Ar/39Ar thermochronology and implications for Late Mesozoic extension in the eastern North China Craton[J]. Geological Society of America Bulletin, 2007, 119:1405-1414. |
[12] |
WU F Y, LIN J Q, SIMON A W, et al. Nature and significance of the early Cretaceous giant igneous event in eastern China[J]. Earth and Planetary Science Letters, 2005, 233:103-119.
DOI URL |
[13] |
GAO S, RUDNICK R L, CARLSON R W. Re-Os evidence for replacement of ancient mantle lithosphere beneath the North China Craton[J]. Earth and Planetary Science Letters, 2002, 198:307-322.
DOI URL |
[14] | GAO S, RUDNICK R L, YUAN H L, et al. Recycling lower continental crust in the North China craton[J]. Nature, 2004, 432:892-897. |
[15] | 徐义刚. 华北岩石圈减薄的时空不均一特征[J]. 高校地质学报, 2004, 10(3):324-331. |
[16] | 李洪颜, 徐义刚, 黄小龙, 等. 华北克拉通北缘晚古生代活化: 山西宁武—静乐盆地上石炭统太原组碎屑锆石U-Pb 测年及Hf 同位素证据[J]. 科学通报, 2009, 54:632-640. |
[17] |
LI S R, SANTOSH M. Geodynamics of heterogeneous gold mineralization in the North China Craton and its relationship to lithospheric destruction[J]. Gondwana Research, 2017, 50:267-292.
DOI URL |
[18] |
CHEN L, JIANG M M, YANG J H, et al. Presence of an intralithospheric discontinuity in the central and western North China Craton: implications for destruction of the craton[J], Geology, 2014, 42(3):223-226.
DOI URL |
[19] |
ZHENG T Y, ZHAO L, ZHU R X. New evidence from seismic imaging for subduction during assembly of the North China Craton[J]. Geology, 2009, 37:395-398.
DOI URL |
[20] | ZHENG T Y, YANG J H, HE Y M, et al. Seismological constraints on the crustal structures generated by continental rejuvenation in northeastern China[J]. Scientific Reports, 2015, 5:14995. |
[21] | CHEN L, WANG T, ZHAO L, et al. Distinct lateral variation of lithospheric thickness in the northeastern North China Craton[J]. Earth and Planetary Science Letters, 2008, 267:56-68. |
[22] |
CHEN L. Lithospheric structure variations between the eastern and central North China Craton from S- and P-receiver function migration[J]. Physics of the Earth and Planetary Interiors, 2009, 173:216-227.
DOI URL |
[23] |
HE C S. Upwelling mantle plume and lithospheric delamination beneath the North China Craton[J]. Physics of The Earth and Planetary Interiors, 2020. DOI: 10.1016/j.pepi.2020.106548.
DOI |
[24] | 邓晋福, 冯艳芳, 刘翠, 等. 太行—燕辽地区燕山期造山过程、 岩浆源区与成矿作用[J]. 中国地质, 2009, 36(3):623-633. |
[25] | LI J W, BI S J, SELBY D, et al. Giant Mesozoic gold provinces related to the destruction of the North China Craton[J]. Earth and Planetary Sciences Letters, 2012, 349/350:26-37. |
[26] |
YANG C X, SANTOSH M. Ancient deep roots for Mesozoic world-class gold deposits in the north China craton: an integrated genetic perspective[J]. Geoscience Frontiers, 2019. DOI: 10.1016/j.gsf.2019.03.002.
DOI |
[27] | ZHAI M G, SANTOSH M. Metallogeny of the North China Craton: link with secular changes in the evolving Earth[J]. Gondwana Research, 2013, 24:275-297. |
[28] | LI S R, SANTOSH M, ZHANG H F, et al. Inhomogeneous lithospheric thinning in the central North China Craton: zircon U-Pb and S-He-Ar isotopic record from magmatism and metallogeny in the Taihang Mountains[J]. Gondwana Research, 2013, 23(1):141-160. |
[29] | LI S R, SANTOSH M. Metallogeny and craton destruction: records from the North China Craton[J]. Ore Geology Reviews, 2014, 56:76-414. |
[30] | LI L, SANTOSH M, LI S R. The “Jiaodong type” gold deposits: characteristics, origin and prospecting[J]. Ore Geology Reviews, 2015, 65:589-611. |
[31] | LI Q, SANTOSH M, LI S R, et al. Petrology, geochemistry and zircon U-Pb and Lu-Hf isotopes of the Cretaceous dykes in the central North China Craton: implications for magma genesis and gold metallogeny[J]. Ore Geology Reviews, 2015, 67:57-77. |
[32] |
SHEN J F, SANTOSH M, LI S R, et al. He-Ar, S, Pb and O isotope geochemistry of the Dabaiyang gold deposit: implications for the relationship between gold metallogeny and destruction of the North China Craton[J]. Ore Geology Reviews, 2019. DOI: 10.1016/j.oregeorev.2019.103229.
DOI |
[33] | 朱日祥, 范宏瑞, 李建威, 等. 克拉通破坏型金矿床[J]. 中国科学: 地球科学, 2015, 45(8):1153-1168. |
[34] | 王建平, 刘俊, 刘家军, 等. 黑云母全铝压力计估算胶东西北部玲珑花岗质杂岩剥蚀程度[J]. 矿物学报, 2009, 29(S1):481-482. |
[35] | 张拴宏, 赵越, 刘健, 等. 华北地块北缘晚古生代—中生代花岗岩体侵位深度及其构造意义[J]. 岩石学报, 2007, 23(3):625-638. |
[36] | LIU J L, SHEN L, JI M, et al. The Liaonan/Wanfu Metamorphic core complexes in the Liaodong Peninsula: two stages of exhumation and constraints on the destruction of the North China Craton[J]. Tectonics, 2013, 32:1121-1141. |
[37] | HOLLISTER L S, GRISSOM G C, PETERS E K, et al. Confirmation of the empirical correlation of Al in hornblende with pressure of solidification of calc-alkaline plutons[J]. American Mineralogist, 1987, 72:231-239. |
[38] |
SCHMIDT M W. Amphibole composition in tonalite as a function of pressure: an experimental calibration of the Al-in-hornblende barometer[J]. Contributions to Mineralogy and Petrology, 1992, 110:304-310.
DOI URL |
[39] |
ANDERSON J L, BARTH A P, WOODEN J L, et al. Thermometers and thermobarometers in granitic systems[J]. Reviews in Mineralogy and Geochemistry, 2008, 69:121-142.
DOI URL |
[40] | RIDOFI 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. |
[41] | 陆丽娜, 范宏瑞, 胡芳芳, 等. 胶西北郭家岭花岗闪长岩侵位深度: 来自角闪石温压计和流体包裹体的证据[J]. 岩石学报, 2011, 27(5):1521-1532. |
[42] | 孟子岳, 朱飞霖, 张凯亮. 研究岩浆岩的金钥匙: 角闪石-斜长石矿物温压计[J]. 广东微量元素科学, 2016, 23(1):38-41. |
[43] | 赵越, 翟明国, 陈虹, 等. 华北克拉通及相邻造山带古生代—侏罗纪早期大地构造演化[J]. 中国地质, 2017, 44(1):44-60. |
[44] |
ZHANG S H, ZHAO Y, SONG B, et al. Carboniferous granitic plutons from the northern margin of the North China block: implications for a late Paleozoic active continental margin[J]. Journal of Geological Society, 2007, 164:451-463.
DOI URL |
[45] | 张拴宏, 赵越, 刘建民, 等. 华北地块北缘晚古生代—早中生代岩浆活动期次、 特征及构造背景[J]. 岩石矿物学杂志, 2010(6):824-842. |
[46] | ZHANG S H, ZHAO Y, SONG B, et al. Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive belts from the northern margin of the North China craton: geochronology, petrogenesis and tectonic implications[J]. Geological Society of America Bulletin, 2009, 121(1/2):181-200. |
[47] | YE H, ZHANG S H, ZHAO Y, et al. Petrogenesis and emplacement deformation of the late Triassic Dushan composition batholith in the Yanshan fold and thrust belt: implications for the tectonic settings of the northern margin of the North China Craton during the early Mesozoic[J]. Earth Science Frontiers, 2014, 21(4):275-292. |
[48] |
ZHANG H F, GOLDSTEIN S L, ZHOU X H, et al. Comprehensive refertilization of lithospheric mantle beneath the North China Craton: further Os-Sr-Nd isotopic constraints[J]. Journal of Geological Society, 2009, 166:249-259.
DOI URL |
[49] |
LIU J M, ZHAO Y, SUN Y L, et al. Recognition of the latest Permian to Early Triassic Cu-Mo mineralization on the northern margin of the North China Craton block and geological significance[J]. Gondwana Research, 2010, 17(1):125-134.
DOI URL |
[50] | 贾三石, 王恩德, 付建飞, 等. 冀东—辽西主要金矿矿集区地质特征的差异性与成矿作用的统一性探析[J]. 地质学报, 2011, 85(9):1493-1506. |
[51] | 吴福元, 杨进辉, 张艳斌, 等. 辽西东南部中生代花岗岩时代[J]. 岩石学报, 2006, 22(2):315-325. |
[52] | 江淑娥, 张国仁, 潘玉启, 等. 辽西中生代侵入岩基本特征及与构造运动的关系[J]. 地质与资源, 2010, 19(1):22-31. |
[53] | 段培新, 李长民, 刘翠, 等. 内蒙古赤峰金厂沟梁金矿区花岗岩类年代学、 地球化学特征及其地质意义[J]. 岩石学报, 2014, 30(11):3189-3202. |
[54] | 付乐兵. 华北克拉通北缘赤峰—朝阳地区中生代构造岩浆演化与金成矿[D]. 武汉: 中国地质大学(武汉), 2012. |
[55] | 李荫清, 艾永德. 内蒙古红花沟金矿床的流体包裹体研究[J]. 矿物学报, 1991, 11(4):346-354. |
[56] | 王时麒, 汤葵联. 内蒙赤峰安家营子金矿床成矿流体的物理化学条件研究[J]. 北京大学学报(自然科学版), 1994, 30(4):446-452. |
[57] | 姜能, 张文淮. 内蒙古赤峰莲花山金矿床成矿物理化学条件及成矿机理[J]. 地球化学, 1996, 25(1):73-83. |
[58] |
ZHANG X H, LIU Q, MA Y J, et al. Geology, fluid inclusion, isotope geochemistry, and geochronology of the Paishanlou shear one-hosted gold deposit, North China Craton[J]. Ore geology Reviews, 2005, 26(3/4):325-348.
DOI URL |
[59] | 李永刚, 翟明国, 杨进辉, 等. 内蒙古赤峰安家营子金矿成矿时代以及对华北中生代爆发成矿的意义[J]. 中国科学: 地球科学, 2003, 33(10):960-966. |
[60] | 庞奖励. 二道沟矿床绢云母的39Ar-40Ar年龄及其地质意义[J]. 陕西师范大学学报(自然科学版), 1999, 27(1):103-107. |
[61] | 周乃武. 金厂沟梁金(铜)矿田成矿时代的理顺[J]. 黄金学报, 2000, 2(3):180-185. |
[62] | 苗来成, 范蔚茗, 翟明国, 等. 金厂沟梁—二道沟金矿田内花岗岩类侵入体锆石的离子探针年代学及意义[J]. 岩石学报, 2003, 19(1):71-80. |
[63] | 侯万荣. 内蒙古哈达门沟金矿床与金厂沟梁金矿床对比研究[D]. 北京: 中国地质科学院, 2011. |
[64] | 杨帆, 庞雪娇, 吴猛, 等. 内蒙古赤峰金厂沟梁地区花岗岩类年代学、 地球化学与Hf同位素特征[J]. 地球科学, 2019, 44(10):3209-3222. |
[65] | FU L B, WEI J H, KUSKY M T, et al. The Cretaceous Duimiangou adakite-like intrusion from the Chifeng region, northern North China Craton: crustal contamination of basaltic magma in an intracontinental extensional environment[J]. Lithos, 2012, 134/135:273-288. |
[66] | 骆辉, 赵运起. 辽宁阜新排山楼金矿地质成矿作用[J]. 前寒武纪研究进展, 1997, 20(4):13-24. |
[67] | 罗镇宽, 苗来成, 关康, 等. 辽宁阜新排山楼金矿区岩浆岩锆石定年及其意义[J]. 地球化学, 2001, 30(5):483-490. |
[68] | 王荣湖, 金成洙, 李景春, 等. 排山楼金矿床年龄及其地质意义[J]. 东北大学学报: 自然科学版, 2008, 29(10):1482-1485. |
[69] | 李永刚, 翟明国, 苗来成, 等. 内蒙古赤峰地区安家营子金矿成矿流体研究[J]. 岩石学报, 2004, 20(4):961-968. |
[70] | 王路智. 内蒙敖汉金厂沟梁金矿床地质地球化学特征与成矿机制探讨[D]. 北京: 中国地质大学(北京), 2018. |
[71] | 陈军强. 内蒙赤峰金厂沟梁金矿床地质、 地球化学特征及成因研究[D]. 长春: 吉林大学, 2006. |
[72] | 李俊建, 沈保丰, 骆辉, 等. 辽宁阜新排山楼金矿的成矿年龄[J]. 地质科学, 2001, 36(1):107-111. |
[73] | 聂世嘉, 杨言辰, 韩世炯, 等. 辽宁排山楼金矿床黑云母花岗岩成岩时代及地质意义[J]. 地球科学与环境学报, 2017, 39(2):161-174. |
[74] | 贾三石, 王恩德, 付建飞, 等. 辽西排山楼金矿床微量元素地球化学特征及深部找矿预测研究[J]. 地球化学, 2011, 40(3):266-279. |
[75] | 林文蔚, 彭丽君. 由电子探针分析数据估算角闪石、 黑云母中的Fe3+和Fe2+[J]. 长春地质学院学报, 1994, 24(2):155-162. |
[76] | 骆文娟, 张德会, 孙剑. 河北丰宁撒岱沟门钼矿区成矿岩体球化学特征及其对矿床成因的约束[J]. 地质与勘探, 2010, 46(3):491-505. |
[77] |
MUTCH E J F, BLUNDY J D, TATTITCH B C, et al. An experimental study of amphibole stability in low-pressure granitic magmas and a revised Al-in-hornblende geobarometer[J]. Contributions to Mineralogy and Petrology, 2016, 171:85.
DOI URL |
[78] |
DOU J Z, ZHANG H F, TONG Y, et al. Application of geothermobarometers to Mesozoic granitoids in the Jiaodong Peninsula, eastern China: criteria for selecting methods of pressure estimation and implications for crustal exhumation[J]. Journal of Asian Earth Sciences, 2018, 160:271-286.
DOI URL |
[79] |
ANDERSON J L, SMITH D R. The effects of temperature and f(O2) on the Al in hornblende barometer[J]. American Mineralogist, 1995, 80:549-559.
DOI URL |
[80] | 艾晓玲, 马昌前. 大别山同剥露刘家洼岩体角闪石、 长石的矿物化学[J]. 岩石矿物学, 2000, 20(3):213-219. |
[81] | 张华锋, 李胜荣, 翟明国, 等. 胶东半岛早白垩世地壳隆升剥蚀及其动力学意义[J]. 岩石学报, 2006, 22(2):285-295. |
[82] | 曾令森, 陈晶, 陈振宇, 等. 山东石岛花岗岩复合岩体的侵位深度与苏鲁超高压变质岩的快速折返机理与动力学效应[J]. 岩石学报, 2007, 23(12):3171-3179. |
[83] | 李小伟, 黄雄飞, 黄丹峰, 等. 花岗岩中常用压力计的应用评述[J]. 高校地质学报, 2011, 17(3):415-422. |
[84] | 汪洋. 钙碱性火成岩的角闪石全铝压力计: 回顾、 评价和应用实例[J]. 地质论评, 2014, 60(4):839-850. |
[85] | 黎敦朋, 肖爱芳, 刘文元, 等. 福建省侏罗纪—白垩纪花岗岩角闪石-斜长石矿物温压计的地质意义[J]. 东华理工大学学报(自然科学版), 2014, 37(4):351-359. |
[86] |
UCHIDA E, ENDO S, MAKINO M. Relationship between solidification depth of granitic rocks and formation of hydrothermal ore deposits[J]. Resource Geology, 2007, 57(1):47-56.
DOI URL |
[87] | 康志强, 冯佐海, 王睿, 等. 角闪石黑云母全铝压力计的可靠性对比: 以广西姑婆山—花山花岗岩为例[J]. 桂林理工大学学报, 2010, 30(04):474-479. |
[88] | 刘学龙, 李文昌, 尹光侯, 等. 南格咱岛弧印支期地壳隆升与剥蚀及其地质意义: 来自黑云母矿物压力计的证据[J]. 现代地质, 2013, 27(3):537-546. |
[89] | HAMMARSTRON J M, ZEN E. Aluminum in hornblende: an empirical igneous geobarometer[J]. American Mineralogist, 1986, 71:1297-1313. |
[90] | 龚松林. 角闪石全铝压力计对黄陵岩体古隆升速率的研究[J]. 东华理工学院学报, 2004, 27(1):52-58. |
[91] |
BEANERE. Biotite stability in the porphyry copper environment[J]. Economic Geology, 1974, 69(2):241-256.
DOI URL |
[92] | NACHIT H, IBHI A, ABIA E H, et al. Discrimination between primary magmatic biotite, re-equilibrated biotite and neo-formed biotite[J]. Computes Rendus Geoscience, 2005, 337(16):1415-1420. |
[93] | FOSTER M D. Interpretation of the composition of trioctahedral micas[J]. Geological Survey Professional Paper, 1960, 354:11-49. |
[94] | 吕志成, 段国正, 董光华. 大兴安岭中南段燕山期三类不同成矿花岗岩中黑云母的化学成分特征及其成岩成矿意义[J]. 矿物学报, 2003, 23(2):177-184. |
[95] | 蒋国豪, 胡瑞忠, 谢桂青, 等. 大吉山花岗岩体黑云母地球化学特征及其成岩成矿意义[J]. 矿物岩石, 2005, 25(5):58-61. |
[96] | WONES D R. Significance of the assemblage titanite + magnetite + quartz in granitic rocks[J]. American Mineralogist, 1989, 74(7/8):744-749. |
[97] |
HENRY D J, GUIDOTTI C V, THOMSON J A. The Ti-saturation surface for low-to-medium pressure metapelitic biotites: implications for geothermometry and Ti-substitution mechanisms[J]. American Mineralogist, 2005, 90(2):316-328.
DOI URL |
[98] | MUNGALL J E. Roasting the mantle: slab melting and the genesis of major Au and Au-rich Cu deposits[J]. Geology, 2002, 30(10):915-918. |
[99] |
SUN W D, LIANG H Y, LING M X, et al. The link between reduced porphyry copper deposits and oxidized magmas[J]. Geochimica et Cosmochimica Acta, 2013, 103:263-275.
DOI URL |
[100] | WONES D R, EUGSTER H P. Stability of biotite: experiment theory and application[J]. American Mineralogist, 1965, 50(9):12-28. |
[101] | PARSAPOOR A, KHALILI M, TEPLEY F, et al. Mineral chemistry and isotopic composition of magmatic, re-equilibrated and hydrothermal biotites from Darreh-Zar porphyry copper deposit, Kerman (Southeast of Iran)[J]. Ore Geology Reviews, 2015, 66:200-218. |
[102] | 杨阳, 王晓霞, 于晓卫, 等. 胶西北中生代花岗岩中黑云母和角闪石成分特征及成岩成矿意义[J]. 岩石学报, 2017, 10(3):123-136. |
[103] | 张聚全, 李胜荣, 卢静. 中酸性侵入岩的氧逸度计算[J]. 矿物学报, 2018, 38(1):1-13. |
[104] |
SHABANI A A T, LALONDE A E, WHALEN J B. Composition of biotite from granitic rocks of the Candian Appalachian orogen: a potential tectonomagmatic in-dicator[J]. The Canadian Mineralogist, 2003, 41(6):1381-1396.
DOI URL |
[105] | 刘彬, 马昌前, 刘圆圆, 等. 鄂东南铜山口铜(钼)矿床黑云母矿物化学特征及其对岩石成因与成矿的指示[J]. 岩石矿物学杂志, 2010, 29(2):151-165. |
[106] | 侯增谦, 郑远川, 耿元生. 克拉通边缘岩石圈金属再富集与金-钼-稀土元素成矿作用[J]. 矿床地质, 2015, 34(4):641-674. |
[107] |
ZHANG X H, LIU Q, MA Y J, et al. Geology, fluid inclusions, isotope geochemistry, and geochronology of the Paishanlou shear zone-hosted gold deposit, North China Craton[J]. Ore Geology Reviews, 2005, 26(3/4):325-348.
DOI URL |
[108] | 吴福元, 葛文春, 孙德有, 等. 中国东部岩石圈减薄研究中的几个问题[J]. 地学前缘, 2003, 10(3):51-60. |
[109] | 张连昌, 吴华英, 相鹏, 等. 中生代复杂构造体系的成矿过程与成矿作用: 以华北大陆北缘西拉木伦钼铜多金属成矿带为例[J]. 岩石学报, 2010, 26(5):1351-1362. |
[110] | 冯云磊, 袁万明, 郝娜娜, 等. 吉林桦甸市夹皮沟本区金矿剥露历史和矿床保存变化[J]. 地质论评, 2015, 61(1):109-120. |
[111] | 聂逢君, 张进, 严兆彬, 等. 卫境岩体磷灰石裂变径迹年代学与华北北缘晚白垩世剥露事件及铀成矿[J]. 地质学报, 2018, 92(2):313-329. |
[112] | 邵济安, 牛树银, 张履桥, 等. 张宣热隆构造及其成因探讨[J]. 自然科学进展, 2005, 15(6):684-691. |
[113] | 李长平. 华北克拉通北缘张-宣地区中生代金矿床成矿作用及剥蚀保存[D]. 北京: 中国地质大学(北京), 2019. |
[114] |
JIANG N, ZHANG S Q, ZHOU W G, et al. Origin of a Mesozoic granite with A-type characteristics from the North China craton: highly fractionated from I-type magmas?[J]. Contributions to Mineralogy and Petrology, 2009, 158:113-130.
DOI URL |
[115] | 罗照华, 邓晋福, 赵国春, 等. 太行山造山带岩浆活动特征及其造山过程反演[J]. 地球科学: 中国地质大学学报, 1997, 22(3):279-284. |
[116] | 张家声, 徐杰, 万景林, 等. 太行山山前中—新生代伸展拆离构造和年代学[J]. 地质通报, 2002, 21(4/5):207-210. |
[117] | 曹现志. 华北地块中部中新生代构造地貌演变过程与机制[D]. 青岛: 中国海洋大学, 2014. |
[118] | 李庶波, 王岳军, 张玉芝, 等. 南太行山中新生代隆升过程: 磷灰石裂变径迹证据[J]. 大地构造与成矿学, 2015, 39(3):460-469. |
[119] | 刘远. 太行山中部矿床变化保存的裂变径迹热年代学约束[D]. 北京: 中国地质大学(北京), 2019. |
[120] | 柳振江, 王建平, 郑德文, 等. 胶东西北部金矿剥蚀程度及找矿潜力和方向: 来自磷灰石裂变径迹热年代学的证据[J]. 岩石学报, 2010, 26(12):3597-3611. |
[121] | 唐智博, 李理, 时秀朋, 等. 鲁西隆起蒙山晚白垩世—新生代抬升的裂变径迹证据[J]. 中山大学学报(自然科学版), 2011, 50(2):127-133. |
[122] | 郭谱. 鲁西中生代金成矿的地球动力学背景研究[D]. 北京: 中国地质大学(北京), 2014. |
[123] | 吴中海, 吴珍汉. 燕山及邻区晚白垩世以来山脉隆升历史的低温热年代学证据[J]. 地质学报, 2003, 77(3):309-406. |
[124] | 刘武生, 秦明宽, 漆富成, 等. 运用磷灰石裂变径迹分析鄂尔多斯盆地周缘中新生代沉降隆升史[J]. 铀矿地质, 2008, 24(4):221-227. |
[125] | 赵俊峰, 刘池洋, 王晓梅, 等. 吕梁山地区中—新生代隆升演化探讨[J]. 地质论评, 2009, 55(5):663-672. |
[126] | 余心起, 刘俊来, 张德会, 等. 小秦岭文峪花岗岩山体的隆升时代和幅度[J]. 科学通报, 2013, 58(33):3416-3428. |
[127] | 黄惠兰, 常海亮, 付建明, 等. 西华山脉钨矿床的形成压力及有关花岗岩的侵位深度[J]. 矿床地质, 2006, 25(5):562-571. |
[128] | 张德会, 徐九华, 余心起, 等. 成岩成矿深度: 主要影响因素与压力估算方法[J]. 地质通报, 2011, 30(1):112-125. |
[129] | SEEDORFF E, DILLES J H, PROFFETT J R, et al. Porphyry deposits: characteristics and origin of hypogene features[J]. Economic Geology, 2005, 100:251-298. |
[130] | KWAK T A P. W-Sn skarn deposits and related metamorphic skarns and granitoids[M]. Amsterdam: Elsevier, 1987: 451. |
Viewed | ||||||
Full text |
|
|||||
Abstract |
|
|||||