现代地质 ›› 2022, Vol. 36 ›› Issue (04): 1155-1172.DOI: 10.19657/j.geoscience.1000-8527.2022.04.18
收稿日期:
2021-09-22
修回日期:
2021-10-22
出版日期:
2022-08-10
发布日期:
2022-09-09
通讯作者:
陈岳龙
作者简介:
陈岳龙,男,教授,博士生导师,1962年出生,地球化学专业,主要从事区域地球化学研究。Email: chyl@cugb.edu.cn。基金资助:
YANG Fan(), CHEN Yuelong(
), YU Yang
Received:
2021-09-22
Revised:
2021-10-22
Online:
2022-08-10
Published:
2022-09-09
Contact:
CHEN Yuelong
摘要:
鲁西地区位于华北克拉通东部,是研究区域太古宙演化的重要地区。以鲁西地区西南部出露的正长-二长花岗岩为研究对象,系统开展了岩石学、地球化学、锆石U-Pb年龄与Hf同位素组成研究。结果表明,该正长-二长花岗岩为钙碱性、过铝质。锆石U-Pb年龄揭示正长-二长花岗岩侵位于~2 540~2 530 Ma;锆石Hf同位素组成表明其主体由~2.70 Ga的TTG类岩石熔融形成,但再循环的古老地壳组分也参与了岩浆产生过程。微量元素和同位素组成模拟计算结果表明,正长-二长花岗岩是由97%的新生TTG地壳组分部分熔融和3%的变质表壳岩部分熔融物混合形成。结合区域特征,我们认为正长-二长花岗岩形成于伸展构造环境中,该区新太古代晚期岩浆作用与板片俯冲后回撤作用有关,板片回撤过程所致的软流圈上涌为此类岩石的岩浆产生提供了热源。
中图分类号:
杨帆, 陈岳龙, 于洋. 鲁西地区新太古代晚期正长-二长花岗岩成因及地质意义[J]. 现代地质, 2022, 36(04): 1155-1172.
YANG Fan, CHEN Yuelong, YU Yang. Genesis and Geological Significance of Late Archean Syeno-monzogranite in Western Shandong Province[J]. Geoscience, 2022, 36(04): 1155-1172.
图1 鲁西地区太古宙花岗-绿岩带地质简图(据文献[14,27,29,46])
Fig.1 Simplified geological map of Archean granite-greenstone belt in Western Shandong (according to references [14,27,29,46])
序号 | 样品号 | 岩性 | 采样位置 | 经度 | 纬度 |
---|---|---|---|---|---|
1 | TA1801-1 | 中细粒正长花岗岩 | 花果峪村(平邑—郑家峪剖面) | E117°31.746' | N35°28.811' |
2 | TA1808-1 | 细粒正长花岗岩 | 庞庄—城前镇剖面 | E117°26.631' | N35°21.618' |
3 | TA1808-2 | 弱片麻状似斑状二长花岗岩 | 庞庄—城前镇剖面 | E117°26.631' | N35°21.618' |
4 | TA1809 | 片麻状二长花岗岩 | 庞庄—城前镇剖面 | E117°26.164' | N35°21.319' |
5 | TA1817 | 细粒二长花岗岩 | 东郭镇—店子镇—城前镇 | E117°19.281' | N35°12.237' |
6 | TA1818 | 细粒正长花岗岩 | 东郭镇—店子镇—城前镇 | E117°19.378' | N35°12.745' |
表1 采样位置及样品岩性
Table 1 Sampling locations and lithologies
序号 | 样品号 | 岩性 | 采样位置 | 经度 | 纬度 |
---|---|---|---|---|---|
1 | TA1801-1 | 中细粒正长花岗岩 | 花果峪村(平邑—郑家峪剖面) | E117°31.746' | N35°28.811' |
2 | TA1808-1 | 细粒正长花岗岩 | 庞庄—城前镇剖面 | E117°26.631' | N35°21.618' |
3 | TA1808-2 | 弱片麻状似斑状二长花岗岩 | 庞庄—城前镇剖面 | E117°26.631' | N35°21.618' |
4 | TA1809 | 片麻状二长花岗岩 | 庞庄—城前镇剖面 | E117°26.164' | N35°21.319' |
5 | TA1817 | 细粒二长花岗岩 | 东郭镇—店子镇—城前镇 | E117°19.281' | N35°12.237' |
6 | TA1818 | 细粒正长花岗岩 | 东郭镇—店子镇—城前镇 | E117°19.378' | N35°12.745' |
图3 鲁西地区正长-二长花岗岩野外接触关系、手标本及典型显微照片 a.中细粒正长花岗岩(TA1801-1)侵入强片麻状TTG岩石野外照片;b.中细粒正长花岗岩(TA1801-1)野外照片;c.细粒正长花岗岩(TA1808-1)侵入弱片麻状似斑状二长花岗岩(TA1808-2)野外照片;d、e、f.分别是中细粒正长花岗岩、弱片麻状似斑状二长花岗岩、片麻状黑云母二长花岗岩正交偏光照片;Kfs.钾长石;Mi.微斜长石;Pl.斜长石;Qz.石英;Bt.黑云母。
Fig.3 Field contact relationship, hand specimens and typical micrographs of syeno-monzogranites in Western Shandong
样品号 | SiO2 | TiO2 | Al2O3 | TFe2O3 | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | K2O/Na2O | |||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
TA1801-1 | 72.16 | 0.34 | 14.3 | 1.42 | 0.01 | 0.19 | 0.55 | 2.60 | 7.67 | 0.02 | 0.60 | 102.81 | 2.95 | |||
TA1808-1 | 75.92 | 0.07 | 12.96 | 0.72 | <0.01 | 0.14 | 0.85 | 3.08 | 5.41 | 0.02 | 0.43 | 101.36 | 1.76 | |||
TA1808-2 | 74.47 | 0.08 | 13.78 | 0.89 | <0.01 | 0.20 | 1.02 | 3.68 | 4.64 | 0.02 | 0.61 | 100.65 | 1.26 | |||
TA1809 | 76.64 | 0.06 | 13.04 | 0.73 | 0.01 | 0.12 | 0.61 | 3.80 | 4.61 | 0.01 | 0.50 | 101.34 | 1.21 | |||
TA1817 | 73.00 | 0.16 | 14.26 | 1.45 | 0.01 | 0.29 | 1.08 | 3.87 | 4.56 | 0.05 | 0.86 | 100.77 | 1.18 | |||
TA1818 | 74.44 | 0.10 | 13.57 | 1.11 | 0.01 | 0.16 | 0.61 | 3.60 | 5.32 | 0.03 | 0.71 | 101.14 | 1.48 | |||
样品号 | A/CNK | A/NK | Mg# | Li | Be | Sc | Ti | V | Cr | Mn | Co | Ni | Cu | |||
TA1801-1 | 1.09 | 1.13 | 21 | 6.25 | 1.00 | 3.36 | 2 113.57 | 13.16 | 6.44 | 113.48 | 1.27 | 4 | 4.66 | |||
TA1808-1 | 1.11 | 1.18 | 28 | 2.73 | 1.58 | 0.98 | 522.45 | 11.75 | 4.38 | 31.01 | 1.13 | 3 | 17.8 | |||
TA1808-2 | 1.15 | 1.24 | 31 | 2.96 | 0.84 | 0.89 | 534.65 | 7.50 | 2.67 | 52.76 | 1.10 | 2 | 1.93 | |||
TA1809 | 1.11 | 1.16 | 25 | 4.93 | 1.87 | 1.31 | 452.95 | 6.20 | 1.23 | 85.33 | 0.75 | 1 | 4.95 | |||
TA1817 | 1.16 | 1.26 | 28 | 22.96 | 1.77 | 1.95 | 974.31 | 11.09 | 2.72 | 113.67 | 1.48 | 2 | 5.05 | |||
TA1818 | 1.11 | 1.16 | 22 | 7.04 | 1.90 | 1.65 | 669.47 | 9.02 | 0.50 | 122.68 | 1.08 | 1 | 3.7 | |||
样品号 | Zn | Ga | As | Se | Rb | Sr | Y | Zr | Nb | Mo | Sn | Cs | Ba | |||
TA1801-1 | 15.60 | 15.94 | 1.60 | 0.73 | 229 | 142 | 14.5 | 354 | 19.3 | 0.82 | 2.39 | 3.39 | 578 | |||
TA1808-1 | 6.95 | 13.06 | 0.43 | 0.13 | 175 | 276 | 3.53 | 78.6 | 7.12 | 4.9 | 0.53 | 2.44 | 386 | |||
TA1808-2 | 10.85 | 12.03 | 0.41 | 0.08 | 146 | 304 | 2.79 | 70.8 | 2.25 | 0.17 | 0.26 | 2.44 | 1 179 | |||
TA1809 | 11.86 | 14.90 | 0 | 0.12 | 156 | 102 | 3.93 | 58.3 | 5.99 | 0.07 | 0.59 | 2.70 | 266 | |||
TA1817 | 26.54 | 15.50 | 1.16 | 0.31 | 196 | 206 | 4.95 | 133 | 6.77 | 0.09 | 1.00 | 2.87 | 839 | |||
TA1818 | 21.47 | 14.95 | 1.03 | 0.3 | 282 | 135 | 7.57 | 123 | 10.5 | 0.22 | 1.30 | 5.11 | 712 | |||
样品号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | |||
TA1801-1 | 26.50 | 83.1 | 7.44 | 26.8 | 4.99 | 0.71 | 3.39 | 0.54 | 3.11 | 0.62 | 1.82 | 0.31 | 2.07 | |||
TA1808-1 | 5.05 | 15.6 | 1.17 | 4.36 | 0.8 | 0.20 | 0.65 | 0.09 | 0.56 | 0.11 | 0.36 | 0.06 | 0.44 | |||
TA1808-2 | 13.60 | 15.5 | 2.08 | 6.85 | 0.95 | 0.41 | 0.62 | 0.08 | 0.43 | 0.09 | 0.28 | 0.05 | 0.35 | |||
TA1809 | 4.18 | 14.0 | 1.02 | 3.87 | 0.69 | 0.17 | 0.61 | 0.09 | 0.52 | 0.11 | 0.35 | 0.06 | 0.48 | |||
TA1817 | 27.30 | 31.7 | 4.94 | 15.5 | 2.3 | 0.50 | 1.48 | 0.2 | 0.96 | 0.18 | 0.52 | 0.08 | 0.52 | |||
TA1818 | 20.10 | 41.5 | 3.70 | 12.5 | 2.08 | 0.42 | 1.65 | 0.24 | 1.28 | 0.25 | 0.70 | 0.11 | 0.74 | |||
样品号 | Lu | Hf | Ta | Pb | Th | U | REE | (La/Yb)N | (La/Sm)N | (Gd/Yb)N | δEu | |||||
TA1801-1 | 0.27 | 8.84 | 2.1 | 19.6 | 10.9 | 3.28 | 161.69 | 9.18 | 3.43 | 1.35 | 0.53 | |||||
TA1808-1 | 0.07 | 3.21 | 0.71 | 18.8 | 22.5 | 6.00 | 29.54 | 8.23 | 4.08 | 1.22 | 0.85 | |||||
TA1808-2 | 0.06 | 1.80 | 0.24 | 15.3 | 17.7 | 1.99 | 41.33 | 27.9 | 9.24 | 1.47 | 1.63 | |||||
TA1809 | 0.08 | 2.69 | 0.64 | 20.6 | 18.7 | 3.54 | 26.24 | 6.25 | 3.91 | 1.05 | 0.80 | |||||
TA1817 | 0.08 | 3.38 | 0.63 | 16.0 | 15.3 | 1.60 | 86.16 | 37.66 | 7.66 | 2.35 | 0.83 | |||||
TA1818 | 0.11 | 3.51 | 1.48 | 13.3 | 19.6 | 2.62 | 85.41 | 19.48 | 6.24 | 1.84 | 0.69 |
表2 鲁西地区正长-二长花岗岩主量元素(wB/%)、微量元素(wB/(μg/g))组成
Table 2 Composition of major elements(%)and trace elements (μg/g) of syeno-monzogranites in Western Shandong
样品号 | SiO2 | TiO2 | Al2O3 | TFe2O3 | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | K2O/Na2O | |||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
TA1801-1 | 72.16 | 0.34 | 14.3 | 1.42 | 0.01 | 0.19 | 0.55 | 2.60 | 7.67 | 0.02 | 0.60 | 102.81 | 2.95 | |||
TA1808-1 | 75.92 | 0.07 | 12.96 | 0.72 | <0.01 | 0.14 | 0.85 | 3.08 | 5.41 | 0.02 | 0.43 | 101.36 | 1.76 | |||
TA1808-2 | 74.47 | 0.08 | 13.78 | 0.89 | <0.01 | 0.20 | 1.02 | 3.68 | 4.64 | 0.02 | 0.61 | 100.65 | 1.26 | |||
TA1809 | 76.64 | 0.06 | 13.04 | 0.73 | 0.01 | 0.12 | 0.61 | 3.80 | 4.61 | 0.01 | 0.50 | 101.34 | 1.21 | |||
TA1817 | 73.00 | 0.16 | 14.26 | 1.45 | 0.01 | 0.29 | 1.08 | 3.87 | 4.56 | 0.05 | 0.86 | 100.77 | 1.18 | |||
TA1818 | 74.44 | 0.10 | 13.57 | 1.11 | 0.01 | 0.16 | 0.61 | 3.60 | 5.32 | 0.03 | 0.71 | 101.14 | 1.48 | |||
样品号 | A/CNK | A/NK | Mg# | Li | Be | Sc | Ti | V | Cr | Mn | Co | Ni | Cu | |||
TA1801-1 | 1.09 | 1.13 | 21 | 6.25 | 1.00 | 3.36 | 2 113.57 | 13.16 | 6.44 | 113.48 | 1.27 | 4 | 4.66 | |||
TA1808-1 | 1.11 | 1.18 | 28 | 2.73 | 1.58 | 0.98 | 522.45 | 11.75 | 4.38 | 31.01 | 1.13 | 3 | 17.8 | |||
TA1808-2 | 1.15 | 1.24 | 31 | 2.96 | 0.84 | 0.89 | 534.65 | 7.50 | 2.67 | 52.76 | 1.10 | 2 | 1.93 | |||
TA1809 | 1.11 | 1.16 | 25 | 4.93 | 1.87 | 1.31 | 452.95 | 6.20 | 1.23 | 85.33 | 0.75 | 1 | 4.95 | |||
TA1817 | 1.16 | 1.26 | 28 | 22.96 | 1.77 | 1.95 | 974.31 | 11.09 | 2.72 | 113.67 | 1.48 | 2 | 5.05 | |||
TA1818 | 1.11 | 1.16 | 22 | 7.04 | 1.90 | 1.65 | 669.47 | 9.02 | 0.50 | 122.68 | 1.08 | 1 | 3.7 | |||
样品号 | Zn | Ga | As | Se | Rb | Sr | Y | Zr | Nb | Mo | Sn | Cs | Ba | |||
TA1801-1 | 15.60 | 15.94 | 1.60 | 0.73 | 229 | 142 | 14.5 | 354 | 19.3 | 0.82 | 2.39 | 3.39 | 578 | |||
TA1808-1 | 6.95 | 13.06 | 0.43 | 0.13 | 175 | 276 | 3.53 | 78.6 | 7.12 | 4.9 | 0.53 | 2.44 | 386 | |||
TA1808-2 | 10.85 | 12.03 | 0.41 | 0.08 | 146 | 304 | 2.79 | 70.8 | 2.25 | 0.17 | 0.26 | 2.44 | 1 179 | |||
TA1809 | 11.86 | 14.90 | 0 | 0.12 | 156 | 102 | 3.93 | 58.3 | 5.99 | 0.07 | 0.59 | 2.70 | 266 | |||
TA1817 | 26.54 | 15.50 | 1.16 | 0.31 | 196 | 206 | 4.95 | 133 | 6.77 | 0.09 | 1.00 | 2.87 | 839 | |||
TA1818 | 21.47 | 14.95 | 1.03 | 0.3 | 282 | 135 | 7.57 | 123 | 10.5 | 0.22 | 1.30 | 5.11 | 712 | |||
样品号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | |||
TA1801-1 | 26.50 | 83.1 | 7.44 | 26.8 | 4.99 | 0.71 | 3.39 | 0.54 | 3.11 | 0.62 | 1.82 | 0.31 | 2.07 | |||
TA1808-1 | 5.05 | 15.6 | 1.17 | 4.36 | 0.8 | 0.20 | 0.65 | 0.09 | 0.56 | 0.11 | 0.36 | 0.06 | 0.44 | |||
TA1808-2 | 13.60 | 15.5 | 2.08 | 6.85 | 0.95 | 0.41 | 0.62 | 0.08 | 0.43 | 0.09 | 0.28 | 0.05 | 0.35 | |||
TA1809 | 4.18 | 14.0 | 1.02 | 3.87 | 0.69 | 0.17 | 0.61 | 0.09 | 0.52 | 0.11 | 0.35 | 0.06 | 0.48 | |||
TA1817 | 27.30 | 31.7 | 4.94 | 15.5 | 2.3 | 0.50 | 1.48 | 0.2 | 0.96 | 0.18 | 0.52 | 0.08 | 0.52 | |||
TA1818 | 20.10 | 41.5 | 3.70 | 12.5 | 2.08 | 0.42 | 1.65 | 0.24 | 1.28 | 0.25 | 0.70 | 0.11 | 0.74 | |||
样品号 | Lu | Hf | Ta | Pb | Th | U | REE | (La/Yb)N | (La/Sm)N | (Gd/Yb)N | δEu | |||||
TA1801-1 | 0.27 | 8.84 | 2.1 | 19.6 | 10.9 | 3.28 | 161.69 | 9.18 | 3.43 | 1.35 | 0.53 | |||||
TA1808-1 | 0.07 | 3.21 | 0.71 | 18.8 | 22.5 | 6.00 | 29.54 | 8.23 | 4.08 | 1.22 | 0.85 | |||||
TA1808-2 | 0.06 | 1.80 | 0.24 | 15.3 | 17.7 | 1.99 | 41.33 | 27.9 | 9.24 | 1.47 | 1.63 | |||||
TA1809 | 0.08 | 2.69 | 0.64 | 20.6 | 18.7 | 3.54 | 26.24 | 6.25 | 3.91 | 1.05 | 0.80 | |||||
TA1817 | 0.08 | 3.38 | 0.63 | 16.0 | 15.3 | 1.60 | 86.16 | 37.66 | 7.66 | 2.35 | 0.83 | |||||
TA1818 | 0.11 | 3.51 | 1.48 | 13.3 | 19.6 | 2.62 | 85.41 | 19.48 | 6.24 | 1.84 | 0.69 |
图4 鲁西地区正长-二长花岗岩样品地球化学分类图 (a)K2O-Na2O-CaO三元图解(据文献[60]);(b)K2O与SiO2图解(据文献[61]);(c)A/NK(Al2O3/(Na2O+K2O))与A/CNK(Al2O3/(CaO+Na2O+K2O))图解(据文献[62])。
Fig.4 Geochemical classification map of syeno-monzogranites samples in Western Shandong
图5 鲁西地区正长-二长花岗岩样品稀土元素球粒陨石标准化分布型式(a)和微量元素原始地幔标准化蛛网图(b) (球粒陨石和原始地幔标准化值分别据文献[57,63], ~2.70 Ga TTG岩石引自文献[64⇓-66])
Fig.5 Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element spider diagrams (b) for the syeno-monzogranites in Western Shandong
样品分析点号 | wB/(μg/g) | 同位素比值 | 年龄/Ma | |||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | Th/U | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | ||||
TA1808-2-01 | 983 | 1 557 | 0.631 3 | 0.211 5 | 0.005 5 | 1.260 0 | 0.070 0 | 0.043 2 | 0.003 0 | 2 917 | 39 | 828 | 32 | 273 | 19 | |||
TA1808-2-02 | 1 173 | 840 | 1.396 4 | 0.191 5 | 0.004 3 | 1.880 0 | 0.050 0 | 0.071 2 | 0.001 2 | 2 755 | 39 | 1 074 | 19 | 443 | 7 | |||
TA1808-2-03 | 4 770 | 3 420 | 1.394 7 | 0.258 9 | 0.003 4 | 1.235 0 | 0.025 5 | 0.034 6 | 0.000 9 | 3 240 | 21 | 817 | 12 | 219 | 6 | |||
TA1808-2-04 | 461 | 656 | 0.702 7 | 0.173 3 | 0.002 8 | 7.480 0 | 0.130 0 | 0.313 0 | 0.003 6 | 2 590 | 28 | 2 171 | 16 | 1 755 | 18 | |||
TA1808-2-05 | 3 450 | 4 570 | 0.754 9 | 0.224 2 | 0.003 2 | 1.487 0 | 0.027 5 | 0.048 1 | 0.001 2 | 3 011 | 24 | 925 | 11 | 303 | 7 | |||
TA1808-2-06 | 2 060 | 3 110 | 0.662 4 | 0.245 7 | 0.004 1 | 0.935 0 | 0.045 0 | 0.027 6 | 0.001 4 | 3 157 | 26 | 670 | 23 | 176 | 9 | |||
TA1808-2-07 | 3 190 | 3 770 | 0.846 2 | 0.201 5 | 0.003 6 | 1.420 0 | 0.050 0 | 0.051 1 | 0.002 5 | 2 839 | 28 | 897 | 21 | 321 | 15 | |||
TA1808-2-08 | 244 | 283 | 0.862 2 | 0.169 5 | 0.002 6 | 8.310 0 | 0.130 0 | 0.355 5 | 0.003 7 | 2 553 | 26 | 2 265 | 15 | 1 961 | 17 | |||
TA1808-2-09 | 704 | 1 184 | 0.594 6 | 0.180 0 | 0.004 0 | 1.420 0 | 0.050 0 | 0.057 2 | 0.002 0 | 2 653 | 38 | 897 | 21 | 359 | 12 | |||
TA1808-2-10 | 3 460 | 1 700 | 2.035 3 | 0.240 0 | 0.003 2 | 1.671 0 | 0.046 0 | 0.050 5 | 0.001 5 | 3 120 | 24 | 998 | 18 | 318 | 9 | |||
TA1808-2-11 | 6 180 | 6 800 | 0.908 8 | 0.219 8 | 0.003 5 | 1.170 0 | 0.065 0 | 0.038 6 | 0.002 6 | 2 979 | 31 | 787 | 31 | 244 | 16 | |||
TA1808-2-12 | 1 221 | 1 460 | 0.836 3 | 0.218 6 | 0.003 7 | 1.519 0 | 0.045 0 | 0.050 4 | 0.001 8 | 2 970 | 31 | 938 | 19 | 317 | 11 | |||
TA1808-2-13 | 228 | 228 | 1.000 0 | 0.205 2 | 0.006 0 | 3.400 0 | 0.125 0 | 0.120 2 | 0.003 9 | 2 868 | 48 | 1 504 | 31 | 732 | 22 | |||
TA1808-2-14 | 3 030 | 2 720 | 1.114 0 | 0.202 8 | 0.002 9 | 1.560 0 | 0.050 0 | 0.055 8 | 0.001 9 | 2 849 | 22 | 954 | 20 | 350 | 12 | |||
TA1808-2-15 | 345 | 799 | 0.431 8 | 0.168 5 | 0.003 2 | 2.590 0 | 0.055 0 | 0.111 5 | 0.002 1 | 2 543 | 31 | 1 298 | 16 | 681 | 12 | |||
TA1808-2-16 | 760 | 864 | 0.879 6 | 0.172 3 | 0.002 7 | 2.770 0 | 0.060 0 | 0.116 6 | 0.002 3 | 2 580 | 29 | 1 347 | 16 | 711 | 13 | |||
TA1808-2-17 | 308 | 486 | 0.633 7 | 0.173 0 | 0.002 7 | 5.740 0 | 0.095 0 | 0.240 6 | 0.004 8 | 2 587 | 26 | 1 937 | 15 | 1 390 | 25 | |||
TA1808-2-18 | 4 400 | 2 810 | 1.565 8 | 0.208 7 | 0.003 5 | 2.250 0 | 0.060 0 | 0.078 2 | 0.001 5 | 2 895 | 28 | 1 197 | 19 | 485 | 9 | |||
TA1808-2-19 | 6 090 | 2 410 | 2.527 0 | 0.195 0 | 0.002 9 | 1.960 0 | 0.060 0 | 0.072 9 | 0.002 5 | 2 785 | 24 | 1 102 | 20 | 454 | 15 | |||
TA1808-2-20 | 262 0 | 290 0 | 0.903 4 | 0.218 8 | 0.002 4 | 1.810 0 | 0.050 0 | 0.060 0 | 0.001 9 | 2 972 | 19 | 1 049 | 20 | 376 | 12 | |||
TA1817-01 | 787 | 661 | 1.190 6 | 0.173 2 | 0.001 4 | 5.040 0 | 0.150 0 | 0.211 0 | 0.006 0 | 2 589 | 14 | 1 826 | 28 | 1 234 | 33 | |||
TA1817-02 | 162 | 254 | 0.637 8 | 0.198 1 | 0.006 0 | 6.310 0 | 0.220 0 | 0.231 0 | 0.011 0 | 2 811 | 43 | 2 020 | 31 | 1 340 | 55 | |||
TA1817-03 | 860 | 1 020 | 0.843 1 | 0.232 4 | 0.002 6 | 5.410 0 | 0.150 0 | 0.168 8 | 0.003 8 | 3 069 | 20 | 1 886 | 21 | 1 005 | 21 | |||
TA1817-04 | 417 | 574 | 0.726 5 | 0.173 7 | 0.001 7 | 6.540 0 | 0.150 0 | 0.273 0 | 0.006 5 | 2 594 | 16 | 2 051 | 21 | 1 556 | 33 | |||
TA1817-05 | 990 | 970 | 1.020 6 | 0.191 3 | 0.005 0 | 5.250 0 | 0.335 0 | 0.199 0 | 0.011 5 | 2 754 | 42 | 1 861 | 46 | 1 170 | 55 | |||
TA1817-06 | 287 | 484 | 0.593 0 | 0.191 0 | 0.003 6 | 7.320 0 | 0.150 0 | 0.278 0 | 0.007 5 | 2 751 | 28 | 2 151 | 19 | 1 581 | 39 | |||
TA1817-07 | 1 100 | 1 039 | 1.058 7 | 0.176 6 | 0.001 7 | 3.370 0 | 0.110 0 | 0.138 4 | 0.004 8 | 2 621 | 18 | 1 497 | 26 | 836 | 27 | |||
TA1817-08 | 313 | 402 | 0.778 6 | 0.181 2 | 0.002 8 | 7.320 0 | 0.230 0 | 0.293 0 | 0.008 5 | 2 664 | 25 | 2 151 | 24 | 1 657 | 40 | |||
TA1817-09 | 167 | 306 | 0.545 8 | 0.171 1 | 0.001 8 | 8.800 0 | 0.215 0 | 0.373 0 | 0.009 0 | 2 569 | 18 | 2 317 | 22 | 2 044 | 41 | |||
TA1817-10 | 340 | 1 050 | 0.323 8 | 0.185 8 | 0.003 4 | 2.990 0 | 0.060 0 | 0.116 7 | 0.001 8 | 2 706 | 27 | 1 405 | 17 | 712 | 11 | |||
TA1817-11 | 1 320 | 1 110 | 1.189 2 | 0.178 0 | 0.003 0 | 4.600 0 | 0.080 0 | 0.187 4 | 0.002 3 | 2 635 | 28 | 1 749 | 15 | 1 107 | 13 | |||
TA1817-12 | 230 | 303 | 0.759 1 | 0.172 3 | 0.002 2 | 8.480 0 | 0.290 0 | 0.357 0 | 0.013 0 | 2 580 | 20 | 2 284 | 37 | 1 968 | 65 | |||
TA1817-13 | 640 | 352 | 1.818 2 | 0.171 0 | 0.003 9 | 8.040 0 | 0.375 0 | 0.341 0 | 0.018 0 | 2 567 | 32 | 2 236 | 50 | 1 891 | 90 | |||
TA1817-14 | 6 400 | 1 700 | 3.764 7 | 0.201 1 | 0.003 1 | 3.410 0 | 0.385 0 | 0.123 0 | 0.015 5 | 2 835 | 22 | 1 507 | 60 | 748 | 75 | |||
TA1817-15 | 512 | 776 | 0.659 8 | 0.158 5 | 0.001 2 | 5.130 0 | 0.105 0 | 0.234 7 | 0.004 4 | 2 440 | 13 | 1 841 | 18 | 1 359 | 24 | |||
TA1817-16 | 215 | 278 | 0.773 4 | 0.172 6 | 0.002 6 | 8.780 0 | 0.285 0 | 0.369 0 | 0.012 5 | 2 583 | 24 | 2 315 | 33 | 2 025 | 60 | |||
TA1817-17 | 301 | 359 | 0.838 4 | 0.166 7 | 0.001 7 | 8.410 0 | 0.245 0 | 0.366 0 | 0.010 5 | 2 524 | 18 | 2 276 | 33 | 2 011 | 50 | |||
TA1817-18 | 153 | 131 | 1.167 9 | 0.171 9 | 0.002 9 | 11.260 0 | 0.245 0 | 0.475 0 | 0.005 5 | 2 576 | 27 | 2 545 | 20 | 2 505 | 24 | |||
TA1817-19 | 750 | 580 | 1.293 1 | 0.164 9 | 0.002 0 | 6.410 0 | 0.175 0 | 0.282 0 | 0.008 0 | 2 506 | 20 | 2 034 | 26 | 1 601 | 41 | |||
TA1817-20 | 3 090 | 2 210 | 1.398 2 | 0.163 9 | 0.001 6 | 2.700 0 | 0.050 0 | 0.119 5 | 0.001 9 | 2 496 | 17 | 1 328 | 15 | 728 | 11 |
表3 鲁西地区二长花岗岩U-Pb分析结果
Table 3 U-Pb analysis results of monzogranites in Western Shandong
样品分析点号 | wB/(μg/g) | 同位素比值 | 年龄/Ma | |||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | Th/U | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | ||||
TA1808-2-01 | 983 | 1 557 | 0.631 3 | 0.211 5 | 0.005 5 | 1.260 0 | 0.070 0 | 0.043 2 | 0.003 0 | 2 917 | 39 | 828 | 32 | 273 | 19 | |||
TA1808-2-02 | 1 173 | 840 | 1.396 4 | 0.191 5 | 0.004 3 | 1.880 0 | 0.050 0 | 0.071 2 | 0.001 2 | 2 755 | 39 | 1 074 | 19 | 443 | 7 | |||
TA1808-2-03 | 4 770 | 3 420 | 1.394 7 | 0.258 9 | 0.003 4 | 1.235 0 | 0.025 5 | 0.034 6 | 0.000 9 | 3 240 | 21 | 817 | 12 | 219 | 6 | |||
TA1808-2-04 | 461 | 656 | 0.702 7 | 0.173 3 | 0.002 8 | 7.480 0 | 0.130 0 | 0.313 0 | 0.003 6 | 2 590 | 28 | 2 171 | 16 | 1 755 | 18 | |||
TA1808-2-05 | 3 450 | 4 570 | 0.754 9 | 0.224 2 | 0.003 2 | 1.487 0 | 0.027 5 | 0.048 1 | 0.001 2 | 3 011 | 24 | 925 | 11 | 303 | 7 | |||
TA1808-2-06 | 2 060 | 3 110 | 0.662 4 | 0.245 7 | 0.004 1 | 0.935 0 | 0.045 0 | 0.027 6 | 0.001 4 | 3 157 | 26 | 670 | 23 | 176 | 9 | |||
TA1808-2-07 | 3 190 | 3 770 | 0.846 2 | 0.201 5 | 0.003 6 | 1.420 0 | 0.050 0 | 0.051 1 | 0.002 5 | 2 839 | 28 | 897 | 21 | 321 | 15 | |||
TA1808-2-08 | 244 | 283 | 0.862 2 | 0.169 5 | 0.002 6 | 8.310 0 | 0.130 0 | 0.355 5 | 0.003 7 | 2 553 | 26 | 2 265 | 15 | 1 961 | 17 | |||
TA1808-2-09 | 704 | 1 184 | 0.594 6 | 0.180 0 | 0.004 0 | 1.420 0 | 0.050 0 | 0.057 2 | 0.002 0 | 2 653 | 38 | 897 | 21 | 359 | 12 | |||
TA1808-2-10 | 3 460 | 1 700 | 2.035 3 | 0.240 0 | 0.003 2 | 1.671 0 | 0.046 0 | 0.050 5 | 0.001 5 | 3 120 | 24 | 998 | 18 | 318 | 9 | |||
TA1808-2-11 | 6 180 | 6 800 | 0.908 8 | 0.219 8 | 0.003 5 | 1.170 0 | 0.065 0 | 0.038 6 | 0.002 6 | 2 979 | 31 | 787 | 31 | 244 | 16 | |||
TA1808-2-12 | 1 221 | 1 460 | 0.836 3 | 0.218 6 | 0.003 7 | 1.519 0 | 0.045 0 | 0.050 4 | 0.001 8 | 2 970 | 31 | 938 | 19 | 317 | 11 | |||
TA1808-2-13 | 228 | 228 | 1.000 0 | 0.205 2 | 0.006 0 | 3.400 0 | 0.125 0 | 0.120 2 | 0.003 9 | 2 868 | 48 | 1 504 | 31 | 732 | 22 | |||
TA1808-2-14 | 3 030 | 2 720 | 1.114 0 | 0.202 8 | 0.002 9 | 1.560 0 | 0.050 0 | 0.055 8 | 0.001 9 | 2 849 | 22 | 954 | 20 | 350 | 12 | |||
TA1808-2-15 | 345 | 799 | 0.431 8 | 0.168 5 | 0.003 2 | 2.590 0 | 0.055 0 | 0.111 5 | 0.002 1 | 2 543 | 31 | 1 298 | 16 | 681 | 12 | |||
TA1808-2-16 | 760 | 864 | 0.879 6 | 0.172 3 | 0.002 7 | 2.770 0 | 0.060 0 | 0.116 6 | 0.002 3 | 2 580 | 29 | 1 347 | 16 | 711 | 13 | |||
TA1808-2-17 | 308 | 486 | 0.633 7 | 0.173 0 | 0.002 7 | 5.740 0 | 0.095 0 | 0.240 6 | 0.004 8 | 2 587 | 26 | 1 937 | 15 | 1 390 | 25 | |||
TA1808-2-18 | 4 400 | 2 810 | 1.565 8 | 0.208 7 | 0.003 5 | 2.250 0 | 0.060 0 | 0.078 2 | 0.001 5 | 2 895 | 28 | 1 197 | 19 | 485 | 9 | |||
TA1808-2-19 | 6 090 | 2 410 | 2.527 0 | 0.195 0 | 0.002 9 | 1.960 0 | 0.060 0 | 0.072 9 | 0.002 5 | 2 785 | 24 | 1 102 | 20 | 454 | 15 | |||
TA1808-2-20 | 262 0 | 290 0 | 0.903 4 | 0.218 8 | 0.002 4 | 1.810 0 | 0.050 0 | 0.060 0 | 0.001 9 | 2 972 | 19 | 1 049 | 20 | 376 | 12 | |||
TA1817-01 | 787 | 661 | 1.190 6 | 0.173 2 | 0.001 4 | 5.040 0 | 0.150 0 | 0.211 0 | 0.006 0 | 2 589 | 14 | 1 826 | 28 | 1 234 | 33 | |||
TA1817-02 | 162 | 254 | 0.637 8 | 0.198 1 | 0.006 0 | 6.310 0 | 0.220 0 | 0.231 0 | 0.011 0 | 2 811 | 43 | 2 020 | 31 | 1 340 | 55 | |||
TA1817-03 | 860 | 1 020 | 0.843 1 | 0.232 4 | 0.002 6 | 5.410 0 | 0.150 0 | 0.168 8 | 0.003 8 | 3 069 | 20 | 1 886 | 21 | 1 005 | 21 | |||
TA1817-04 | 417 | 574 | 0.726 5 | 0.173 7 | 0.001 7 | 6.540 0 | 0.150 0 | 0.273 0 | 0.006 5 | 2 594 | 16 | 2 051 | 21 | 1 556 | 33 | |||
TA1817-05 | 990 | 970 | 1.020 6 | 0.191 3 | 0.005 0 | 5.250 0 | 0.335 0 | 0.199 0 | 0.011 5 | 2 754 | 42 | 1 861 | 46 | 1 170 | 55 | |||
TA1817-06 | 287 | 484 | 0.593 0 | 0.191 0 | 0.003 6 | 7.320 0 | 0.150 0 | 0.278 0 | 0.007 5 | 2 751 | 28 | 2 151 | 19 | 1 581 | 39 | |||
TA1817-07 | 1 100 | 1 039 | 1.058 7 | 0.176 6 | 0.001 7 | 3.370 0 | 0.110 0 | 0.138 4 | 0.004 8 | 2 621 | 18 | 1 497 | 26 | 836 | 27 | |||
TA1817-08 | 313 | 402 | 0.778 6 | 0.181 2 | 0.002 8 | 7.320 0 | 0.230 0 | 0.293 0 | 0.008 5 | 2 664 | 25 | 2 151 | 24 | 1 657 | 40 | |||
TA1817-09 | 167 | 306 | 0.545 8 | 0.171 1 | 0.001 8 | 8.800 0 | 0.215 0 | 0.373 0 | 0.009 0 | 2 569 | 18 | 2 317 | 22 | 2 044 | 41 | |||
TA1817-10 | 340 | 1 050 | 0.323 8 | 0.185 8 | 0.003 4 | 2.990 0 | 0.060 0 | 0.116 7 | 0.001 8 | 2 706 | 27 | 1 405 | 17 | 712 | 11 | |||
TA1817-11 | 1 320 | 1 110 | 1.189 2 | 0.178 0 | 0.003 0 | 4.600 0 | 0.080 0 | 0.187 4 | 0.002 3 | 2 635 | 28 | 1 749 | 15 | 1 107 | 13 | |||
TA1817-12 | 230 | 303 | 0.759 1 | 0.172 3 | 0.002 2 | 8.480 0 | 0.290 0 | 0.357 0 | 0.013 0 | 2 580 | 20 | 2 284 | 37 | 1 968 | 65 | |||
TA1817-13 | 640 | 352 | 1.818 2 | 0.171 0 | 0.003 9 | 8.040 0 | 0.375 0 | 0.341 0 | 0.018 0 | 2 567 | 32 | 2 236 | 50 | 1 891 | 90 | |||
TA1817-14 | 6 400 | 1 700 | 3.764 7 | 0.201 1 | 0.003 1 | 3.410 0 | 0.385 0 | 0.123 0 | 0.015 5 | 2 835 | 22 | 1 507 | 60 | 748 | 75 | |||
TA1817-15 | 512 | 776 | 0.659 8 | 0.158 5 | 0.001 2 | 5.130 0 | 0.105 0 | 0.234 7 | 0.004 4 | 2 440 | 13 | 1 841 | 18 | 1 359 | 24 | |||
TA1817-16 | 215 | 278 | 0.773 4 | 0.172 6 | 0.002 6 | 8.780 0 | 0.285 0 | 0.369 0 | 0.012 5 | 2 583 | 24 | 2 315 | 33 | 2 025 | 60 | |||
TA1817-17 | 301 | 359 | 0.838 4 | 0.166 7 | 0.001 7 | 8.410 0 | 0.245 0 | 0.366 0 | 0.010 5 | 2 524 | 18 | 2 276 | 33 | 2 011 | 50 | |||
TA1817-18 | 153 | 131 | 1.167 9 | 0.171 9 | 0.002 9 | 11.260 0 | 0.245 0 | 0.475 0 | 0.005 5 | 2 576 | 27 | 2 545 | 20 | 2 505 | 24 | |||
TA1817-19 | 750 | 580 | 1.293 1 | 0.164 9 | 0.002 0 | 6.410 0 | 0.175 0 | 0.282 0 | 0.008 0 | 2 506 | 20 | 2 034 | 26 | 1 601 | 41 | |||
TA1817-20 | 3 090 | 2 210 | 1.398 2 | 0.163 9 | 0.001 6 | 2.700 0 | 0.050 0 | 0.119 5 | 0.001 9 | 2 496 | 17 | 1 328 | 15 | 728 | 11 |
图6 鲁西地区二长花岗岩样品LA-ICP-MS锆石U-Pb谐和图 (a)二长花岗岩(TA1808-2);(b)二长花岗岩(TA1817);插图显示了所分析样品中代表性锆石的阴极发光图像,图中已标明圈点、相应的U-Pb年龄和εHf(t)值。
Fig.6 LA-ICP-MS zircon U-Pb concordance diagram of monzogranites samples in Western Shandong
样品分析点号 | 176Yb/177Hf | 2σ | 176Lu/177Hf | 2σ | 176Hf/177Hf | 2σ | εHf(t) | 2σ | TDM1/Ma | TDM2/Ma | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|---|---|
TA1808-2-2 | 0.036 7 | 0.000 7 | 0.001 311 | 0.000 012 | 0.281 273 | 0.000 021 | 1.92 | 1.65 | 2 781 | 2 900 | -0.96 |
TA1808-2-4 | 0.026 7 | 0.000 5 | 0.001 031 | 0.000 010 | 0.281 240 | 0.000 023 | 1.23 | 1.69 | 2 807 | 2 943 | -0.97 |
TA1808-2-8 | 0.021 4 | 0.000 1 | 0.000 678 | 0.000 002 | 0.281 252 | 0.000 019 | 2.27 | 1.64 | 2 764 | 2 878 | -0.98 |
TA1808-2-9 | 0.139 5 | 0.003 2 | 0.004 189 | 0.000 138 | 0.281 231 | 0.000 024 | -4.56 | 1.60 | 3 071 | 3 298 | -0.87 |
TA1808-2-10 | 0.049 4 | 0.000 6 | 0.001 737 | 0.000 012 | 0.281 239 | 0.000 019 | -0.03 | 1.59 | 2 860 | 3 020 | -0.95 |
TA1808-2-13 | 0.040 2 | 0.001 5 | 0.001 565 | 0.000 043 | 0.281 233 | 0.000 025 | 0.06 | 1.71 | 2 856 | 3 015 | -0.95 |
TA1808-2-14 | 0.034 6 | 0.000 5 | 0.001 073 | 0.000 020 | 0.281 257 | 0.000 021 | 1.77 | 1.65 | 2 786 | 2 910 | -0.97 |
TA1808-2-16 | 0.085 1 | 0.001 4 | 0.002 665 | 0.000 023 | 0.281 312 | 0.000 020 | 0.96 | 1.58 | 2 829 | 2 962 | -0.92 |
TA1808-2-17 | 0.037 2 | 0.000 7 | 0.001 351 | 0.000 009 | 0.281 275 | 0.000 017 | 1.92 | 1.58 | 2 782 | 2 901 | -0.96 |
TA1808-2-19 | 0.046 8 | 0.000 6 | 0.001 900 | 0.000 023 | 0.281 318 | 0.000 020 | 2.50 | 1.61 | 2 763 | 2 867 | -0.94 |
TA1817-1 | 0.030 2 | 0.000 7 | 0.000 942 | 0.000 007 | 0.281 197 | 0.000 018 | 0.15 | 1.33 | 2 857 | 3 032 | -0.97 |
TA1817-4 | 0.028 6 | 0.000 2 | 0.000 908 | 0.000 008 | 0.281 320 | 0.000 017 | 4.58 | 1.32 | 2 688 | 2 762 | -0.97 |
TA1817-5 | 0.048 6 | 0.001 7 | 0.001 515 | 0.000 049 | 0.281 320 | 0.000 022 | 3.53 | 1.39 | 2 732 | 2 827 | -0.95 |
TA1817-7 | 0.043 3 | 0.000 8 | 0.001 398 | 0.000 025 | 0.281 343 | 0.000 018 | 4.55 | 1.32 | 2 692 | 2 766 | -0.96 |
TA1817-9 | 0.033 7 | 0.000 4 | 0.001 162 | 0.000 004 | 0.281 270 | 0.000 021 | 2.36 | 1.37 | 2 775 | 2 898 | -0.96 |
TA1817-11 | 0.046 5 | 0.001 1 | 0.001 317 | 0.000 020 | 0.281 289 | 0.000 025 | 2.77 | 1.46 | 2 760 | 2 874 | -0.96 |
TA1817-13 | 0.022 4 | 0.000 3 | 0.000 75 | 0.000 003 | 0.281 298 | 0.000 018 | 4.08 | 1.34 | 2 708 | 2 794 | -0.98 |
TA1817-16 | 0.012 0 | 0.000 1 | 0.000 503 | 0.000 002 | 0.281 275 | 0.000 016 | 3.69 | 1.31 | 2 721 | 2 817 | -0.98 |
TA1817-17 | 0.020 5 | 0.000 5 | 0.000 663 | 0.000 009 | 0.281 262 | 0.000 015 | 2.95 | 1.30 | 2 749 | 2 862 | -0.98 |
TA1817-18 | 0.015 7 | 0.000 3 | 0.000 564 | 0.000 003 | 0.281 28 | 0.000 019 | 3.76 | 1.36 | 2 719 | 2 813 | -0.98 |
表4 鲁西地区二长花岗岩锆石Hf同位素数据
Table 4 Hf isotopic data of zircon from monzogranites in Western Shandong
样品分析点号 | 176Yb/177Hf | 2σ | 176Lu/177Hf | 2σ | 176Hf/177Hf | 2σ | εHf(t) | 2σ | TDM1/Ma | TDM2/Ma | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|---|---|
TA1808-2-2 | 0.036 7 | 0.000 7 | 0.001 311 | 0.000 012 | 0.281 273 | 0.000 021 | 1.92 | 1.65 | 2 781 | 2 900 | -0.96 |
TA1808-2-4 | 0.026 7 | 0.000 5 | 0.001 031 | 0.000 010 | 0.281 240 | 0.000 023 | 1.23 | 1.69 | 2 807 | 2 943 | -0.97 |
TA1808-2-8 | 0.021 4 | 0.000 1 | 0.000 678 | 0.000 002 | 0.281 252 | 0.000 019 | 2.27 | 1.64 | 2 764 | 2 878 | -0.98 |
TA1808-2-9 | 0.139 5 | 0.003 2 | 0.004 189 | 0.000 138 | 0.281 231 | 0.000 024 | -4.56 | 1.60 | 3 071 | 3 298 | -0.87 |
TA1808-2-10 | 0.049 4 | 0.000 6 | 0.001 737 | 0.000 012 | 0.281 239 | 0.000 019 | -0.03 | 1.59 | 2 860 | 3 020 | -0.95 |
TA1808-2-13 | 0.040 2 | 0.001 5 | 0.001 565 | 0.000 043 | 0.281 233 | 0.000 025 | 0.06 | 1.71 | 2 856 | 3 015 | -0.95 |
TA1808-2-14 | 0.034 6 | 0.000 5 | 0.001 073 | 0.000 020 | 0.281 257 | 0.000 021 | 1.77 | 1.65 | 2 786 | 2 910 | -0.97 |
TA1808-2-16 | 0.085 1 | 0.001 4 | 0.002 665 | 0.000 023 | 0.281 312 | 0.000 020 | 0.96 | 1.58 | 2 829 | 2 962 | -0.92 |
TA1808-2-17 | 0.037 2 | 0.000 7 | 0.001 351 | 0.000 009 | 0.281 275 | 0.000 017 | 1.92 | 1.58 | 2 782 | 2 901 | -0.96 |
TA1808-2-19 | 0.046 8 | 0.000 6 | 0.001 900 | 0.000 023 | 0.281 318 | 0.000 020 | 2.50 | 1.61 | 2 763 | 2 867 | -0.94 |
TA1817-1 | 0.030 2 | 0.000 7 | 0.000 942 | 0.000 007 | 0.281 197 | 0.000 018 | 0.15 | 1.33 | 2 857 | 3 032 | -0.97 |
TA1817-4 | 0.028 6 | 0.000 2 | 0.000 908 | 0.000 008 | 0.281 320 | 0.000 017 | 4.58 | 1.32 | 2 688 | 2 762 | -0.97 |
TA1817-5 | 0.048 6 | 0.001 7 | 0.001 515 | 0.000 049 | 0.281 320 | 0.000 022 | 3.53 | 1.39 | 2 732 | 2 827 | -0.95 |
TA1817-7 | 0.043 3 | 0.000 8 | 0.001 398 | 0.000 025 | 0.281 343 | 0.000 018 | 4.55 | 1.32 | 2 692 | 2 766 | -0.96 |
TA1817-9 | 0.033 7 | 0.000 4 | 0.001 162 | 0.000 004 | 0.281 270 | 0.000 021 | 2.36 | 1.37 | 2 775 | 2 898 | -0.96 |
TA1817-11 | 0.046 5 | 0.001 1 | 0.001 317 | 0.000 020 | 0.281 289 | 0.000 025 | 2.77 | 1.46 | 2 760 | 2 874 | -0.96 |
TA1817-13 | 0.022 4 | 0.000 3 | 0.000 75 | 0.000 003 | 0.281 298 | 0.000 018 | 4.08 | 1.34 | 2 708 | 2 794 | -0.98 |
TA1817-16 | 0.012 0 | 0.000 1 | 0.000 503 | 0.000 002 | 0.281 275 | 0.000 016 | 3.69 | 1.31 | 2 721 | 2 817 | -0.98 |
TA1817-17 | 0.020 5 | 0.000 5 | 0.000 663 | 0.000 009 | 0.281 262 | 0.000 015 | 2.95 | 1.30 | 2 749 | 2 862 | -0.98 |
TA1817-18 | 0.015 7 | 0.000 3 | 0.000 564 | 0.000 003 | 0.281 28 | 0.000 019 | 3.76 | 1.36 | 2 719 | 2 813 | -0.98 |
图7 鲁西地区二长花岗岩结晶年龄与εHf(t)值关系图 (~2.70 Ga的TTG岩石数据引自文献[66,71],~2.50 Ga的富钾花岗岩引自文献[40])
Fig.7 Zircon εHf(t) values versus crystallization age plots of monzogranites in Western Shandong(~2.70 Ga TTG gneiss data reported in references [66,71],~2.50 Ga potassic granites data are from the reference [40])
图8 鲁西地区正长-二长花岗岩成因判别图 (a)MgO与SiO2关系图(PMB.玄武岩或角闪岩部分熔融区域;LSA.低硅埃达克岩;HAS.高硅埃达克岩,据文献[78]);(b)3×CaO-Al2O3/(TFeO+MgO)-5×K2O/Na2O关系图(据文献[5]);(c)部分熔融成岩模型的稀土分布型式对比(~2.50~2.61 Ga的二长花岗岩和~2.53 Ga的钾质花岗岩分别引自文献[28,67,71])。
Fig.8 Petrogenetic discrimination diagrams for the syeno-monzogranites in Western Shandong
SiO2/% | TiO2/% | Al2O3/% | TFeO/% | MgO/% | CaO/% | Na2O/% | K2O/% | P2O5/% | ZrO2/% | ||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
17SD33-1(新生) | 70.99 | 0.48 | 14.79 | 3.11 | 0.78 | 2.81 | 4.23 | 1.26 | 0.14 | 0.015 | |||||||
A0435(古老) | 67.47 | 0.57 | 16.07 | 1.94 | 4.26 | 0.26 | 0.37 | 5.82 | 0.16 | 0.06 | |||||||
TA1817(结果) | 73 | 0.16 | 14.26 | 1.45 | 0.29 | 1.08 | 3.87 | 4.56 | 0.05 | 0.01 | |||||||
模拟计算最优结果 | 70.88 | 0.48 | 14.83 | 3.05 | 0.88 | 2.73 | 4.11 | 1.4 | 0.14 | 0.11 | |||||||
La/(μg/g) | Ce/(μg/g) | Nd/(μg/g) | Sm/(μg/g) | Eu/(μg/g) | Gd/(μg/g) | Ho/(μg/g) | Yb/(μg/g) | ||||||||||
17SD33-1(新生) | 14.5 | 32 | 12.4 | 1.93 | 0.79 | 1.72 | 0.16 | 0.4 | |||||||||
A0435(古老) | 166 | 229 | 100 | 17.3 | 0.82 | 15.8 | 3.38 | 7.04 | |||||||||
TA1817(结果) | 27.3 | 31.7 | 15.5 | 2.3 | 0.5 | 1.48 | 0.18 | 0.52 | |||||||||
模拟计算最优结果 | 25.38 | 48.77 | 20.09 | 3.17 | 1.08 | 2.83 | 0.32 | 0.74 |
表5 新生地壳、古老地壳和二长花岗岩数据与模拟计算最优结果
Table 5 Data of juvenile crust, old crust and monzogranite and optimal results of simulation calculation
SiO2/% | TiO2/% | Al2O3/% | TFeO/% | MgO/% | CaO/% | Na2O/% | K2O/% | P2O5/% | ZrO2/% | ||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
17SD33-1(新生) | 70.99 | 0.48 | 14.79 | 3.11 | 0.78 | 2.81 | 4.23 | 1.26 | 0.14 | 0.015 | |||||||
A0435(古老) | 67.47 | 0.57 | 16.07 | 1.94 | 4.26 | 0.26 | 0.37 | 5.82 | 0.16 | 0.06 | |||||||
TA1817(结果) | 73 | 0.16 | 14.26 | 1.45 | 0.29 | 1.08 | 3.87 | 4.56 | 0.05 | 0.01 | |||||||
模拟计算最优结果 | 70.88 | 0.48 | 14.83 | 3.05 | 0.88 | 2.73 | 4.11 | 1.4 | 0.14 | 0.11 | |||||||
La/(μg/g) | Ce/(μg/g) | Nd/(μg/g) | Sm/(μg/g) | Eu/(μg/g) | Gd/(μg/g) | Ho/(μg/g) | Yb/(μg/g) | ||||||||||
17SD33-1(新生) | 14.5 | 32 | 12.4 | 1.93 | 0.79 | 1.72 | 0.16 | 0.4 | |||||||||
A0435(古老) | 166 | 229 | 100 | 17.3 | 0.82 | 15.8 | 3.38 | 7.04 | |||||||||
TA1817(结果) | 27.3 | 31.7 | 15.5 | 2.3 | 0.5 | 1.48 | 0.18 | 0.52 | |||||||||
模拟计算最优结果 | 25.38 | 48.77 | 20.09 | 3.17 | 1.08 | 2.83 | 0.32 | 0.74 |
图9 鲁西地区新太古代晚期构造环境简化模型及正长-二长花岗岩形成机制图
Fig.9 Simplified model of late Neoarchean tectonic environment and formation mechanism diagram of syeno-monzogranites in Western Shandong
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