Geoscience ›› 2018, Vol. 32 ›› Issue (06): 1254-1262.DOI: 10.19657/j.geoscience.1000-8527.2018.06.13
• Petrology • Previous Articles Next Articles
MAO Yanli(), WANG Tao(), LI Hongrui, PAN Zhongkui
Received:
2017-11-05
Revised:
2018-03-04
Online:
2018-12-10
Published:
2018-12-20
CLC Number:
MAO Yanli, WANG Tao, LI Hongrui, PAN Zhongkui. Geochemical Characteristics and Tectonic Setting of Meta-mafic Volcanic Rocks from Jixian Group in Liujiaping,Wenxian County, Gansu Province[J]. Geoscience, 2018, 32(06): 1254-1262.
Fig.1 Regional geologic map in Liujiaping of Wenxian County, Gansu Province ((a) after LI et al.[21]; (b) modified from the 1∶50,000 regional geologic map of the Liujiaping, Sanhe, and Chujiaba areas)
样品编号 | SiO2 | TiO2 | Al2O3 | Fe2O3 | FeO | MnO | MgO | CaO |
---|---|---|---|---|---|---|---|---|
PM26-23 | 50.02 | 1.60 | 14.70 | 2.19 | 8.58 | 0.20 | 7.58 | 10.59 |
PM26-35 | 48.78 | 0.96 | 14.12 | 2.75 | 8.53 | 0.17 | 7.73 | 12.44 |
PM26-58 | 48.53 | 1.13 | 13.54 | 2.19 | 9.83 | 0.20 | 7.91 | 11.72 |
PM26-76 | 46.93 | 1.05 | 13.12 | 2.39 | 10.28 | 0.22 | 8.11 | 10.42 |
PM26-82 | 49.13 | 1.09 | 13.48 | 5.00 | 7.93 | 0.18 | 5.62 | 12.75 |
PM26-110 | 48.16 | 1.11 | 14.27 | 3.48 | 9.77 | 0.19 | 6.42 | 11.60 |
样品编号 | Na2O | K2O | P2O5 | 烧失量 | 总量 | A/CNK | FeOT | Mg# |
PM26-23 | 2.22 | 0.02 | 0.18 | 3.04 | 100.92 | 0.64 | 10.55 | 56.15 |
PM26-35 | 1.44 | 0.01 | 0.09 | 2.38 | 99.39 | 0.56 | 11.00 | 55.60 |
PM26-58 | 1.45 | 0.03 | 0.09 | 2.69 | 99.31 | 0.57 | 11.80 | 54.44 |
PM26-76 | 1.57 | 0.02 | 0.08 | 5.57 | 99.75 | 0.61 | 12.43 | 53.77 |
PM26-82 | 0.47 | 0.01 | 0.08 | 5.10 | 100.82 | 0.56 | 12.43 | 44.63 |
PM26-110 | 1.69 | 0.02 | 0.10 | 3.60 | 100.40 | 0.60 | 12.90 | 47.01 |
Table 1 Major element contents (%) and parameters of the Jixian meta-basalts
样品编号 | SiO2 | TiO2 | Al2O3 | Fe2O3 | FeO | MnO | MgO | CaO |
---|---|---|---|---|---|---|---|---|
PM26-23 | 50.02 | 1.60 | 14.70 | 2.19 | 8.58 | 0.20 | 7.58 | 10.59 |
PM26-35 | 48.78 | 0.96 | 14.12 | 2.75 | 8.53 | 0.17 | 7.73 | 12.44 |
PM26-58 | 48.53 | 1.13 | 13.54 | 2.19 | 9.83 | 0.20 | 7.91 | 11.72 |
PM26-76 | 46.93 | 1.05 | 13.12 | 2.39 | 10.28 | 0.22 | 8.11 | 10.42 |
PM26-82 | 49.13 | 1.09 | 13.48 | 5.00 | 7.93 | 0.18 | 5.62 | 12.75 |
PM26-110 | 48.16 | 1.11 | 14.27 | 3.48 | 9.77 | 0.19 | 6.42 | 11.60 |
样品编号 | Na2O | K2O | P2O5 | 烧失量 | 总量 | A/CNK | FeOT | Mg# |
PM26-23 | 2.22 | 0.02 | 0.18 | 3.04 | 100.92 | 0.64 | 10.55 | 56.15 |
PM26-35 | 1.44 | 0.01 | 0.09 | 2.38 | 99.39 | 0.56 | 11.00 | 55.60 |
PM26-58 | 1.45 | 0.03 | 0.09 | 2.69 | 99.31 | 0.57 | 11.80 | 54.44 |
PM26-76 | 1.57 | 0.02 | 0.08 | 5.57 | 99.75 | 0.61 | 12.43 | 53.77 |
PM26-82 | 0.47 | 0.01 | 0.08 | 5.10 | 100.82 | 0.56 | 12.43 | 44.63 |
PM26-110 | 1.69 | 0.02 | 0.10 | 3.60 | 100.40 | 0.60 | 12.90 | 47.01 |
样品编号 | Sr | Rb | Ba | Th | Ta | Nb | Zr | Hf | Ti | Sc | Cr |
---|---|---|---|---|---|---|---|---|---|---|---|
PM26-23 | 86.30 | 6.00 | 10.50 | 8.00 | 4.00 | 8.20 | 108.00 | 7.50 | 9 968.00 | 33.60 | 254.00 |
PM26-35 | 230.00 | 9.00 | 22.80 | 10.10 | 5.00 | 14.00 | 51.00 | 8.10 | 6 394.00 | 35.00 | 184.00 |
PM26-58 | 133.00 | 16.60 | 25.10 | 7.80 | 4.30 | 10.10 | 59.00 | 2.80 | 6 498.00 | 40.40 | 214.00 |
PM26-76 | 125.00 | 45.90 | 28.00 | 9.90 | 5.30 | 9.90 | 48.00 | 5.60 | 7 067.00 | 37.20 | 131.00 |
PM26-82 | 226.00 | 72.30 | 8.30 | 8.40 | 3.80 | 8.60 | 56.10 | 9.70 | 7 493.00 | 31.40 | 130.00 |
PM26-110 | 164.00 | 77.30 | 10.50 | 7.80 | 4.40 | 12.00 | 58.00 | 8.80 | 7 329.00 | 36.60 | 170.00 |
样品编号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er |
PM26-23 | 7.20 | 17.80 | 2.90 | 14.80 | 4.30 | 1.20 | 4.59 | 0.92 | 5.91 | 1.15 | 3.29 |
PM26-35 | 3.90 | 9.60 | 1.60 | 8.20 | 2.60 | 0.92 | 2.83 | 0.62 | 4.07 | 0.82 | 2.39 |
PM26-58 | 4.80 | 11.40 | 1.90 | 9.70 | 2.90 | 1.08 | 3.20 | 0.68 | 4.37 | 0.89 | 2.55 |
PM26-76 | 3.60 | 9.50 | 1.60 | 8.30 | 2.60 | 1.04 | 2.88 | 0.63 | 4.12 | 0.85 | 2.46 |
PM26-82 | 3.40 | 9.40 | 1.60 | 8.20 | 2.50 | 0.95 | 2.75 | 0.61 | 3.98 | 0.81 | 2.31 |
PM26-110 | 4.10 | 10.70 | 1.70 | 9.00 | 2.80 | 0.94 | 2.99 | 0.66 | 4.31 | 0.88 | 2.56 |
样品编号 | Tm | Yb | Lu | Y | ∑REE | ∑Ce/∑Y | δEu | δCe | (La/Yb)N | (Ce/Yb)N | |
PM26-23 | 0.49 | 3.02 | 0.42 | 27.60 | 95.59 | 2.44 | 0.83 | 0.91 | 1.39 | 1.33 | |
PM26-35 | 0.36 | 2.36 | 0.34 | 19.90 | 60.51 | 1.94 | 1.04 | 0.90 | 0.96 | 0.92 | |
PM26-58 | 0.37 | 2.28 | 0.34 | 20.90 | 67.36 | 2.16 | 1.09 | 0.88 | 1.22 | 1.13 | |
PM26-76 | 0.36 | 2.24 | 0.32 | 20.20 | 60.70 | 1.92 | 1.17 | 0.92 | 0.93 | 0.96 | |
PM26-82 | 0.35 | 2.15 | 0.31 | 18.90 | 58.22 | 1.96 | 1.11 | 0.94 | 0.92 | 0.98 | |
PM26-110 | 0.38 | 2.41 | 0.36 | 20.70 | 64.49 | 2.01 | 1.00 | 0.95 | 0.99 | 1.00 |
Table 2 REE and trace element contents (10-6) and parameters of the Jixian meta-basalts
样品编号 | Sr | Rb | Ba | Th | Ta | Nb | Zr | Hf | Ti | Sc | Cr |
---|---|---|---|---|---|---|---|---|---|---|---|
PM26-23 | 86.30 | 6.00 | 10.50 | 8.00 | 4.00 | 8.20 | 108.00 | 7.50 | 9 968.00 | 33.60 | 254.00 |
PM26-35 | 230.00 | 9.00 | 22.80 | 10.10 | 5.00 | 14.00 | 51.00 | 8.10 | 6 394.00 | 35.00 | 184.00 |
PM26-58 | 133.00 | 16.60 | 25.10 | 7.80 | 4.30 | 10.10 | 59.00 | 2.80 | 6 498.00 | 40.40 | 214.00 |
PM26-76 | 125.00 | 45.90 | 28.00 | 9.90 | 5.30 | 9.90 | 48.00 | 5.60 | 7 067.00 | 37.20 | 131.00 |
PM26-82 | 226.00 | 72.30 | 8.30 | 8.40 | 3.80 | 8.60 | 56.10 | 9.70 | 7 493.00 | 31.40 | 130.00 |
PM26-110 | 164.00 | 77.30 | 10.50 | 7.80 | 4.40 | 12.00 | 58.00 | 8.80 | 7 329.00 | 36.60 | 170.00 |
样品编号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er |
PM26-23 | 7.20 | 17.80 | 2.90 | 14.80 | 4.30 | 1.20 | 4.59 | 0.92 | 5.91 | 1.15 | 3.29 |
PM26-35 | 3.90 | 9.60 | 1.60 | 8.20 | 2.60 | 0.92 | 2.83 | 0.62 | 4.07 | 0.82 | 2.39 |
PM26-58 | 4.80 | 11.40 | 1.90 | 9.70 | 2.90 | 1.08 | 3.20 | 0.68 | 4.37 | 0.89 | 2.55 |
PM26-76 | 3.60 | 9.50 | 1.60 | 8.30 | 2.60 | 1.04 | 2.88 | 0.63 | 4.12 | 0.85 | 2.46 |
PM26-82 | 3.40 | 9.40 | 1.60 | 8.20 | 2.50 | 0.95 | 2.75 | 0.61 | 3.98 | 0.81 | 2.31 |
PM26-110 | 4.10 | 10.70 | 1.70 | 9.00 | 2.80 | 0.94 | 2.99 | 0.66 | 4.31 | 0.88 | 2.56 |
样品编号 | Tm | Yb | Lu | Y | ∑REE | ∑Ce/∑Y | δEu | δCe | (La/Yb)N | (Ce/Yb)N | |
PM26-23 | 0.49 | 3.02 | 0.42 | 27.60 | 95.59 | 2.44 | 0.83 | 0.91 | 1.39 | 1.33 | |
PM26-35 | 0.36 | 2.36 | 0.34 | 19.90 | 60.51 | 1.94 | 1.04 | 0.90 | 0.96 | 0.92 | |
PM26-58 | 0.37 | 2.28 | 0.34 | 20.90 | 67.36 | 2.16 | 1.09 | 0.88 | 1.22 | 1.13 | |
PM26-76 | 0.36 | 2.24 | 0.32 | 20.20 | 60.70 | 1.92 | 1.17 | 0.92 | 0.93 | 0.96 | |
PM26-82 | 0.35 | 2.15 | 0.31 | 18.90 | 58.22 | 1.96 | 1.11 | 0.94 | 0.92 | 0.98 | |
PM26-110 | 0.38 | 2.41 | 0.36 | 20.70 | 64.49 | 2.01 | 1.00 | 0.95 | 0.99 | 1.00 |
Fig.4 Chondrite-normalized REE patterns and N-MORB normalized multi-element spider diagram of the Jixian meta-basalts (base map after SUN et al.[27] and PEARCE et al.[30])
样号 | 岩性 | w(Sm)/10-6 | w(Nd)/10-6 | 147Sm/144Nd | 143Nd/144Nd±1σ | TDM±1σ/Ma |
---|---|---|---|---|---|---|
1 | 变玄武岩 | 8.951 | 40.170 | 0.134 8 | 0.512 317±0.000 004 | 1 606±8 |
2 | 变玄武岩 | 8.111 | 37.130 | 0.132 2 | 0.512 318±0.000 004 | 1 554±7 |
3 | 变玄武岩 | 2.343 | 7.601 | 0.186 5 | 0.512 800±0.000 003 | 1 956±17 |
4 | 变玄武岩 | 2.356 | 7.460 | 0.191 1 | 0.512 826±0.000 004 | 2 177±27 |
5 | 变玄武岩 | 2.887 | 9.254 | 0.188 7 | 0.512 832±0.000 010 | 1 933±60 |
6 | 变玄武岩 | 3.207 | 10.390 | 0.186 8 | 0.512 826±0.000 004 | 1 831±22 |
7 | 变玄武岩 | 2.633 | 8.461 | 0.188 3 | 0.512 815±0.000 005 | 2 004±30 |
8 | 变玄武岩 | 2.489 | 7.922 | 0.190 1 | 0.512 827±0.000 004 | 2 079±26 |
Table 3 Sm-Nd contents and isotopic compositions of the Baiguoshu Formation meta-basalts
样号 | 岩性 | w(Sm)/10-6 | w(Nd)/10-6 | 147Sm/144Nd | 143Nd/144Nd±1σ | TDM±1σ/Ma |
---|---|---|---|---|---|---|
1 | 变玄武岩 | 8.951 | 40.170 | 0.134 8 | 0.512 317±0.000 004 | 1 606±8 |
2 | 变玄武岩 | 8.111 | 37.130 | 0.132 2 | 0.512 318±0.000 004 | 1 554±7 |
3 | 变玄武岩 | 2.343 | 7.601 | 0.186 5 | 0.512 800±0.000 003 | 1 956±17 |
4 | 变玄武岩 | 2.356 | 7.460 | 0.191 1 | 0.512 826±0.000 004 | 2 177±27 |
5 | 变玄武岩 | 2.887 | 9.254 | 0.188 7 | 0.512 832±0.000 010 | 1 933±60 |
6 | 变玄武岩 | 3.207 | 10.390 | 0.186 8 | 0.512 826±0.000 004 | 1 831±22 |
7 | 变玄武岩 | 2.633 | 8.461 | 0.188 3 | 0.512 815±0.000 005 | 2 004±30 |
8 | 变玄武岩 | 2.489 | 7.922 | 0.190 1 | 0.512 827±0.000 004 | 2 079±26 |
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