Formation Age, Characteristics and Geological Significance of Boketu Miarolitic Granite in Inner Mongolia
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摘要: 晶洞花岗岩成因类型和大地构造背景等方面的研究,目前颇具争议.先前的研究认为晶洞碱长、正长花岗岩属于A型花岗岩,形成于伸展环境,近年来的研究发现其成因类型具多样性.报道了博克图晶洞花岗岩的岩石学、岩石地球化学、年代学等方面的特征.SHRIMP锆石U-Pb定年结果为140.8±2.2 Ma,指示其属于早白垩世的产物.且其具有高SiO2,高ALK(Na2O+K2O)(7.99%~8.43%),K2O/Na2O=1.0~1.1,以及低的FeOT(1.15%~1.30%).微量元素富Th、U、Cs、Rb,贫Ba、Sr、P、Ti,10 000*Ga/Al、总稀土含量以及Zr+Nb+Y+Ce值均低于A型花岗岩最低平均值,由此指示其应属于Ⅰ型花岗岩,Hf同位素特征显示其成分为新生地壳来源.动力学机制上,博克图晶洞花岗岩主要受制于早白垩世时期蒙古-鄂霍次克洋闭合作用.在东北地区岩石圈由增厚到减薄转换事件中,早期的新生地壳在地幔物质的底侵作用下发生低程度的部分熔融作用.
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关键词:
- 晶洞花岗岩 /
- Ⅰ型花岗岩 /
- SHRIMP U-Pb年龄 /
- 部分熔融 /
- 岩石学
Abstract: Genetic types and tectonic backgrounds of miarolitic granite are still controversial. Previous studies have suggested that miarolitic alkali feldspar granites and miarolitic syenite granites belong to A-type granite formed in extensional environment. However, recent studies have found the diversity of the genetic types. In this paper, the petrology, geochemistry and geochronology of Boketu miarolite pluton are present. The zircon SHRIMP U-Pb dating results yield an age of 140.8±2.2 Ma, belonging to the Early Cretaceous. The pluton is characterized by high SiO2 content, and full high alkali content (7.99%-8.43%), with high K2O/Na2O (1.0-1.1); low total Fe content (1.15%-1.30%). On the primitive mantle-normalized spider diagrams, the granite is characterized by positive Th, U, Cs, Rb anomalies and negative Ba, Sr, P, Ti anomalies. 10 000*Ga/Al ratio, the total rare earth content and Zr+Nb+Y+Ce values are lower than the minimum value of the A-type granites. It is indicated that it should belong to Ⅰ-type granite. Hf isotope compositions show the source of juvenile crust. It is mainly restricted by the closure of the Mongolian-Okhotsk ocean, during which the lithosphere transformation from thickening to thinning took place. The granites are formed by the low-degree partial melting of juvenile crust in the underplating of the mantle.-
Key words:
- miarolitic granite /
- Ⅰ-type granite /
- SHRIMP U-Pb dating /
- partial melting /
- petrology
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图 1 东北地区构造简图
①蒙古-鄂霍次克缝合带;②德尔布干断裂;③贺根山断裂;④西拉沐沦断裂;⑤嫩江-八里罕断裂;⑥牡丹江断裂;⑦佳木斯-伊通断裂;⑧敦化-密山断裂;⑨锡霍特-阿林中央带断裂;红色五角星为博克图晶洞花岗岩岩体位置.据张兴洲等(2006)修改
Fig. 1. Tectonic map of NE China
图 8 博克图花岗岩的微量元素蛛网图(a)和稀土元素配分图(b)
Fig. 8. Primitive mantle-normalized spider diagram(a) and chondrite-normalized REE pattern(b) of Boketu miarolitic granite
图 9 10 000×Ga/Al-(Zr+Nb+Y+Ce)图解
Fig. 9. 10 000×Ga/Al-(Zr+Nb+Y+Ce) diagram of Boketu miarolitic granite
图 10 高分异的Ⅰ型花岗岩、A型花岗岩判别图解
Fig. 10. High differentiation (high fractional) Ⅰ-type granite and A-type granite discrimination diagrams
图 11 岩体SiO2-P2O5图解(a)和Y-Rb图解(b)
Fig. 11. SiO2-P2O5 diagram (a) and Y-Rb diagram (b) of Boketu miarolitic granite
图 13 岩石样品Nb-Y判别图解(a)、Rb-(Yb+Ta)判别图解(b)、Ta-Yb判别图解(c)和A/CNK-A/NK图解(d)
图a、b、c据Pearce et al.(1984);图d据Maniar and Piccoli(1989).WPG.班内花岗岩,VAG.火山弧花岗岩,ORG.洋中脊花岗岩,syn-COLG.同碰撞花岗岩,IAGIAG.岛弧花岗岩类;CAG.大陆弧花岗岩类;CCG.大陆碰撞花岗岩类;POG.后造山花岗岩类;RRG.与裂谷有关的花岗岩类;OP.大洋斜长花岗岩;CEUG.与大陆的造陆抬升有关的花岗岩类
Fig. 13. Nb-Y diagram (a), Rb-(Yb+Ta) diagram (b), Ta-Yb diagram (c) and A/CNK-A/NK diagram(d) of granite samples
表 1 博克图晶洞花岗岩SHRIMP锆石U-Pb年龄
Table 1. The SHRIMP zircon U-Pb ages of Boketu miarolitic granite
点号 含量(10-6) Th/U 同位素比值 年龄(Ma) U Th 206Pb 206Pb/238U ±% 207Pb*/235U ±% 207Pb/206Pb ±% 206Pb/238U 207Pb/235U 207Pb/206Pb BKT3-1 263 138 5.23 0.54 0.022 60 2.7 0.161 0 6.0 0.051 6 5.4 144.1±3.9 147.4±3.9 -947±950 BKT3-2 250 144 4.77 0.60 0.022 21 2.5 0.137 3 6.5 0.046 6 5.7 141.6±3.5 141.3±3.9 28±140 BKT3-3 148 96 2.67 0.67 0.020 32 4.1 0.119 0 10 0.055 8 7.0 129.7±5.3 131.4±5.6 -1 020±1 900 BKT3-4 699 446 12.9 0.66 0.021 40 2.2 0.152 3 4.6 0.051 5 4.1 136.5±3.0 137.4±3.3 -5±210 BKT3-5 590 404 11.5 0.71 0.022 77 2.3 0.152 6 4.9 0.053 7 3.9 145.1±3.4 144.3±3.8 359±88 BKT3-6 620 386 11.5 0.64 0.021 27 2.4 0.199 6 3.5 0.052 5 3.6 135.7±3.2 140.3±3.5 -462±680 BKT3-7 115 79 2.20 0.71 0.021 30 3.7 0.149 0 12 0.065 4 8.1 135.9±5.0 139.6±5.4 -1 450±1 800 BKT3-8 545 323 10.3 0.61 0.021 91 2.1 0.145 8 4.7 0.050 4 4.0 139.7±2.9 139.4±3.3 212±93 BKT3-9 646 655 12.1 1.05 0.021 78 2.0 0.145 3 4.3 0.050 6 3.6 138.9±2.8 138.5±3.4 225±83 BKT3-10 422 330 8.57 0.81 0.023 66 2.2 0.195 3 4.5 0.053 9 4.3 150.8±3.3 151.8±3.8 368±97 BKT3-11 554 337 10.60 0.63 0.021 97 2.4 0.174 2 4.4 0.054 3 3.9 140.1±3.3 142.6±3.7 -234±240 BKT3-12 345 168 6.62 0.50 0.022 33 2.3 0.146 4 6.0 0.054 5 4.8 142.3±3.3 141.2±3.6 390±110 BKT3-13 804 475 15.70 0.61 0.022 61 2.2 0.162 9 3.8 0.050 4 3.3 144.1±3.1 145.4±3.4 -52±190 表 2 Hf同位素分析结果
Table 2. Hf isotopic analysis results of Boketu miarolitic granite
样品 176Yb/177Hf 2σ 176Lu/177Hf 2σ 176Hf/177Hf 2σ εHf(0) εHf(t) f(Lu/Hf) TDM1(Ma) TDM2(Ma) BKT3-1 0.047 76 0.000 98 0.001 35 0.000 018 0.282 88 0.000 028 3.8 6.87 -0.96 534.09 1 013.46 BKT3-2 0.047 73 0.000 35 0.001 39 0.000 003 0.282 85 0.000 025 2.8 5.76 -0.96 575.28 1 110.83 BKT3-3 0.044 42 0.000 34 0.001 28 0.000 004 0.282 81 0.000 021 1.3 4.09 -0.96 632.68 1 254.96 BKT3-4 0.055 90 0.000 07 0.001 59 0.000 006 0.282 73 0.000 028 -1.6 1.27 -0.95 755.74 1 513.20 BKT3-5 0.071 01 0.001 78 0.001 96 0.000 042 0.282 75 0.000 031 -0.9 2.08 -0.94 734.64 1 444.60 BKT3-6 0.062 65 0.000 59 0.001 96 0.000 008 0.282 82 0.000 022 1.7 4.51 -0.94 629.08 1 220.43 BKT3-7 0.055 08 0.000 29 0.001 64 0.000 019 0.282 82 0.000 024 1.6 4.49 -0.95 627.18 1 223.48 BKT3-8 0.041 42 0.000 42 0.001 25 0.000 019 0.282 83 0.000 021 2.0 4.92 -0.96 605.04 1 184.99 BKT3-9 0.047 54 0.000 38 0.001 40 0.000 001 0.282 80 0.000 026 1.0 3.95 -0.96 645.13 1 271.74 BKT3-10 0.055 34 0.000 71 0.001 60 0.000 015 0.282 83 0.000 024 2.0 5.15 -0.95 608.4 1 170.60 注:TDM1为单阶段模式年龄;TDM2为两阶段模式年龄;f(Lu/Hf)为分馏因子,Hf同位素数据具体处理参考 Wu et al.(2006) . -
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