Petrological and Geochronological Study of Amphibolite from Jiaobei Terrane
-
摘要: 胶北地块位于华北克拉通东部陆块,胶-辽-吉活动带的南端.胶北地区荆山杂岩中存在一组与高压基性麻粒岩密切共生的斜长角闪岩,是构成前寒武纪变质基底的重要组成部分.岩石学矿物学研究表明,斜长角闪岩记录了3个阶段的变质作用:峰期变质矿物组合(M1)为角闪石1+斜长石+榍石,根据NCKFMASHTO体系的成分视剖面图和角闪石压力计估算出温度条件T=660~715 ℃,压力条件P=0.65~0.71 GPa;其后经历了退变质作用(M2),矿物组合为角闪石2+绿帘石+斜长石+绿泥石+钠长石,估算温压条件为537~630 ℃/0.41~0.58 GPa;晚期发生前绿片岩相退变质作用(M3),其矿物组合为钠长石+葡萄石+绿泥石+方解石,其温压条件 < 400 ℃/0.35 GPa.斜长角闪石的CL图像显示其具有较弱的阴极发光效应和弱震荡环带,Th/U比值相对较小(0.06~0.43),锆石形态和内部结构指示锆石形成于深熔作用过程,21个锆石的LA-ICP-MS定年研究的结果表明,斜长角闪岩记录的最老206Pb/238U年龄为2 075±25 Ma,上交点年龄为1 845±23 Ma(MSWD=0.35),该组年龄记录了斜长角闪岩峰期变质作用时代的上限.斜长角闪岩在原岩形成以后,可能曾经历麻粒岩相变质作用,并记录了在胶-辽-吉带~1.85 Ga碰撞闭合过程中的深熔事件,此后经历了角闪岩相变质作用,及其二次退变质作用,终结于前绿片岩相的变质温压条件.Abstract: Jiaobei terrane lies in the southern segment of the Paleoproterozoic Jiao-Liao-Ji belt, eastern block of the North China craton. There is a set of amphibolite closely related to the high-pressure mafic granulite in Jingshan complex of Jiaobei terrane, which is an important component of the Precambrian metamorphic basement. Our petrological and mineralogical study shows that amphibolite records three stages of metamorphism. The peak stage (M1) shows a mineral assemblage Amp1+Pl +Ttn. The temperature calculated by pseudosection modeling and estimated pressure conditions are T=660-715 ℃, P=0.65-0.71 GPa. The mineral assemblage at post-peak stage (M2) is Amp2+Ep+Pl+Chl+Ab, suggesting temperature and pressure conditions 537-630 ℃/0.41-0.58 GPa. The mineral assemblage at retrograde stage (M3) is Ab+Prh+Chl+Cal.Prehnite and calcite veins indicate that the amphibolite underwent a prehnite-pumpellyite facies metamorphism with P-T conditions < 400 ℃/0.35 GPa.LA-ICP-MS U-Pb geochronology combined with cathodoluminescence (CL) imaging of 21 zircons are all characterized by relatively low Th/U ratios (0.06-0.43), low luminescence and weakly oscillatory zoning. The morphological and internal structure features of zircons suggest that their growths were associated with partial melting, and they yielded 206Pb/238U weighted mean ages of 1 845±23 Ma (MSWD=0.35). After formation of the mafic rock, it may have experienced granulite facies metamorphism, and then recorded the anataxis event during collisional convergence of the Jiao-Liao-Ji orogenic belt at~1.85 Ga. The investigated amphibolite recorded amphibolite facies metamorphism, and subsquently two episodes of retrogressive metamorphism during the lift of the belt.
-
Key words:
- amphibolite /
- mineral chemistry /
- geochronology /
- metamorphism /
- Jiaobei terrane
-
图 1 (a) 胶东地区地质构造简图和研究区马连庄-河头店一带地质图及采样位置(b)
a据周喜文等(2004)和Tam et al.(2011)修改;b据李旭平等(2013)
Fig. 1. (a) Geological schematic map of the Jiaodong district; (b) geological map and sample localities in malianzhuang-hetoudian of study area
图 2 胶北地块斜长角闪岩的显微结构照片
a.样品09LY21的峰期(M1)角闪石颗粒较大(Amp1),可见三连点结构,与斜长石(Pl)共生(单偏光图像);b.样品09LY21背散射(BSE)图像;c.样品09LY23峰期后(M2)角闪石边缘发生退变质形成退变角闪石(Amp2),斜长石(Pl)开始退变质为钠长石(Ab)(单偏光图像);d.样品09LY23背散射(BSE)图像;e.样品09LY23中可见晚期(M3)出现葡萄石(Prh)脉体(单偏光图像);f.样品09LY23中斜长石(Pl)边缘浑圆,角闪石(Amp1)港湾状边缘(正交偏光图像);g.样品09LY23中可见晚期(M3)出现方解石(Cal)脉体,斜长石(Pl)完全退变质为钠长石(Ab)端元(正交偏光图像);h.样品09LY23中部分角闪石(Amp2)退变质为绿帘石(Ep),靠近方解石脉的斜长石均为钠长石(Ab)(背散射图像)
Fig. 2. Photomicrographs of amphibolite from Jiaobei terrane
图 3 胶北地块斜长角闪岩中角闪石的Si-Mg/(Mg+Fe2+)成分分类图
Fig. 3. Si-Mg/(Mg+Fe2+) diagram of amphibole from amphibolites in the Jiaobei terrane
图 4 胶北地块斜长角闪岩中角闪石的AlⅣ-Ti (a)和Ti-(Na+K)(b)成分图解
Fig. 4. Amphibole chemistry from amphibolites in the Jiaobei terrane AlⅣ-Ti (a) diagram and Ti-(Na+K) (b) diagram
图 5 胶北地块斜长角闪岩(09LY21)在NCKFMASHTO体系下的P-T视剖面
图中矿物代号:Hb为角闪石;Bi为黑云母;Pl为斜长石;Ab为钠长石;Ep为绿帘石;Ttn为榍石;L为熔体;H为水,全岩成分分析是利用德国鲁尔大学矿物、地质、地球物理研究生化学实验室X-射线荧光光谱仪(Philips PW 1400)分析测定,在NCKFMASHTO体系标准化之后的摩尔百分比为:SiO2=51.85、Al2O3=8.51、CaO=11.28、MgO=11.77、FeO=11.37、K2O=0.59、Na2O=3.31、TiO2=0.72、O=0.51
Fig. 5. P-T pseudosections for the amphibolite sample (09LY21) from Jiaobei terrane in the systems of NCKFMASHTO
图 10 胶北斜长角闪岩与胶-辽-吉带古元古代变质演化P-T-t轨迹图
变质相边界桑隆康和马昌前(2012); Z.沸石相;P-P.葡萄石—绿纤石相;LA.硬柱石-钠长石-绿泥石相;BS.蓝片岩相;GS.绿片岩相;EA.绿帘角闪岩相;A.角闪岩相;G.麻粒岩相; 1.胶北高压泥质麻粒岩(周喜文等,2004);2.胶北高压泥质麻粒岩(王舫等,2010);3.胶北高压泥质麻粒岩(Tam et al., 2012a);4.胶北中压泥质麻粒岩(Tam et al., 2012b);5.胶北高压基性麻粒岩(Tam et al., 2012c);6.胶北高压基性麻粒岩(Liu et al., 2013);7.三家子石榴斜长角闪岩(刘平华等,2017);8.胶北斜长角闪岩(本文)
Fig. 10. P-T-t projection showing the P-T-t paths determined in this study for amphibolite (a and red bold lines), and previous metamorphic P-T-t paths depicted by other researchers from the Jiao-Liao-Ji belt
表 1 胶北地块斜长角闪岩中角闪石化学成分(%)特征
Table 1. Amphibole compositions (%) in the amphibolites from Jiaobei terrane
样品编号 09LY21 09LY23 09LY23 Amp1 Amp1 Amp1 Amp1 Amp1 Amp1 Amp1 Amp1 Amp1 Amp1 Amp2 Amp2 Amp2 Amp2 Amp2 SiO2 42.25 42.38 41.95 41.94 42.04 45.74 45.12 43.96 44.65 43.00 46.21 47.67 48.36 46.7 48.67 TiO2 1.61 1.60 1.72 1.59 1.76 1.01 1.01 1.23 1.11 1.21 0.15 0.75 0.22 0.53 0.09 Al2O3 11.16 11.29 11.42 11.46 11.41 8.42 9.07 9.93 10.08 10.28 7.67 7.46 5.72 7.83 5.68 FeO 16.77 16.44 17.25 16.86 17.31 15.68 16.57 15.64 16.49 16.63 18.22 14.57 17.63 14.94 15.89 MnO 0.33 0.34 0.37 0.32 0.36 0.37 0.34 0.31 0.32 0.32 0.34 0.32 0.39 0.36 0.31 MgO 9.78 9.70 9.20 9.73 9.28 11.88 10.47 10.55 10.66 10.29 9.27 12.49 9.89 12.03 11.78 CaO 11.35 11.54 11.35 11.35 11.29 11.19 11.49 11.47 12.1 11.61 11.84 11.76 11.87 11.71 12.08 Na2O 1.7 1.56 1.58 1.65 1.60 1.14 1.35 1.33 1.27 1.34 1.19 1.08 0.91 1.01 0.87 K2O 1.25 1.26 1.26 1.23 1.25 0.70 0.72 0.99 0.90 1.04 0.29 0.52 0.21 0.53 0.19 Sum 96.20 96.11 96.10 96.13 96.30 96.13 96.14 95.41 97.58 95.72 95.18 96.62 95.20 95.64 95.56 Oxygens 23 23 23 23 23 23 23 23 23 23 23 23 23 23 23 Si 6.47 6.48 6.45 6.43 6.45 6.90 6.84 6.71 6.69 6.60 7.11 7.09 7.38 7.04 7.34 AlⅣ 1.53 1.52 1.55 1.57 1.55 1.10 1.16 1.29 1.31 1.40 0.89 0.91 0.62 0.96 0.66 AlⅥ 0.49 0.52 0.52 0.50 0.51 0.39 0.47 0.50 0.47 0.46 0.50 0.39 0.41 0.43 0.35 Ti 0.19 0.18 0.20 0.18 0.20 0.11 0.12 0.14 0.13 0.14 0.02 0.08 0.03 0.06 0.01 Fe3+ 0.29 0.33 0.32 0.29 0.32 0.52 0.50 0.45 0.43 0.37 0.61 0.62 0.76 0.59 0.71 Fe2+ 1.86 1.77 1.89 1.88 1.9 1.45 1.60 1.54 1.63 1.77 1.73 1.19 1.49 1.29 1.29 Mn 0.04 0.04 0.05 0.04 0.05 0.05 0.04 0.04 0.04 0.04 0.04 0.04 0.05 0.05 0.04 Mg 2.23 2.21 2.11 2.23 2.12 2.67 2.37 2.40 2.38 2.35 2.13 2.77 2.25 2.70 2.65 Ca 1.86 1.89 1.87 1.87 1.86 1.81 1.87 1.88 1.94 1.91 1.95 1.87 1.94 1.89 1.95 Na 0.50 0.46 0.47 0.49 0.47 0.33 0.40 0.39 0.37 0.40 0.36 0.31 0.27 0.29 0.25 K 0.24 0.25 0.25 0.24 0.25 0.13 0.14 0.19 0.17 0.20 0.06 0.10 0.04 0.10 0.04 Mg/(Mg+Fe) 0.55 0.56 0.53 0.54 0.53 0.65 0.60 0.61 0.59 0.57 0.55 0.70 0.60 0.68 0.67 2 胶北地块斜长角闪岩中代表性矿物化学成分(%)特征
2. Representative mineral compositions (%) in the amphibolites from Jiaobei terrane
样品 09LY23 09LY21 矿物点数 钠长石 斜长石 绿帘石 绿帘石 绿泥石 葡萄石 斜长石 绿帘石 榍石 5 3 2 2 2 2 3 2 1 SiO2 65.18 64.09 37.36 38.40 25.70 42.92 64.74 37.22 30.87 TiO2 0.03 0.07 0.23 0.19 0.06 0.04 0.02 0.27 36.83 Al2O3 20.79 22.49 27.14 27.24 19.20 28.12 24.09 26.64 1.90 Cr2O3 0.01 0.01 0.01 0.00 0.01 0.00 0.01 0.00 0.02 Fe2O3 0.07 0.12 7.66 8.21 1.17 0.14 0.20 8.29 0.00 FeO 0.00 0.00 0.99 0.07 23.50 0.00 0.00 1.50 0.52 MnO 0.00 0.00 0.24 0.17 0.28 0.01 0.00 0.51 0.05 MgO 0.01 0.01 0.00 0.03 15.47 0.01 0.03 0.06 0.02 CaO 1.31 2.96 23.57 23.72 0.16 18.20 3.94 22.84 29.19 Na2O 11.36 8.91 0.08 0.05 0.27 2.49 8.44 0.11 0.03 K2O 0.09 0.07 0.01 0.00 0.07 0.08 0.12 0.03 0.01 Totals 98.84 98.73 97.29 98.08 85.88 92.01 101.59 97.46 99.44 Oxygens 8.00 8.00 12.50 12.50 14.00 11.00 8.00 12.50 5.00 Si 2.90 2.85 2.95 3.00 2.76 2.99 2.80 2.95 1.01 Al 0.00 0.00 0.01 0.01 0.00 0.00 0.00 0.02 0.07 Ti 1.09 1.18 2.53 2.51 2.43 2.31 1.23 2.49 0.91 Cr 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Fe3+ 0.00 0.00 0.46 0.48 0.09 0.01 0.01 0.50 0.00 Mg 0.00 0.00 0.07 0.01 2.11 0.00 0.00 0.10 0.00 Fe2+ 0.00 0.00 0.02 0.01 0.03 0.00 0.00 0.03 0.01 Mn 0.00 0.00 0.00 0.00 2.48 0.00 0.00 0.01 0.00 Na 0.98 0.77 2.00 1.98 0.02 1.36 0.71 1.94 0.00 Ca 0.06 0.14 0.01 0.01 0.06 0.34 0.18 0.02 1.03 K 0.01 0.00 0.00 0.00 0.01 0.01 0.01 0.00 0.00 Sum 5.04 4.95 8.05 8.00 10.00 7.02 4.94 8.05 3.04 An 5.94 15.44 20.35 Ab 93.55 84.12 78.94 表 3 胶北斜长角闪岩(09LY21、09LY23)温压估算结果
Table 3. P-T estimates for amphibolite(09LY21、09LY23)in Jiaobei terrane
样品号 样品 SiHb Xab KD LnKD AlHbT T(℃) P(GPa) Amp1 6.473 0.79 1.295 0.259 2.015 715.316 0.658 Amp1 6.485 0.79 1.312 0.272 2.037 711.444 0.668 09LY21 Amp1 6.449 0.79 1.263 0.234 2.068 716.084 0.683 Amp1 6.433 0.79 1.242 0.216 2.072 718.967 0.685 Amp1 6.448 0.79 1.262 0.232 2.063 716.692 0.681 Amp1 6.896 0.85 2.36 0.859 1.496 650.188 0.411 Amp1 6.845 0.85 2.216 0.796 1.621 651.864 0.471 09LY23 Amp1 6.713 0.85 1.898 0.641 1.787 665.453 0.55 Amp1 6.69 0.85 1.847 0.614 1.779 670.396 0.546 Amp1 6.597 0.85 1.667 0.511 1.859 682.051 0.584 Amp2 7.043 0.97 3.179 1.157 1.480 607.684 0.403 Amp2 7.087 0.97 3.38 1.218 1.307 609.695 0.321 09LY23 Amp2 7.38 0.97 5.456 1.697 1.029 563.795 0.189 Amp2 7.037 0.97 3.152 1.148 1.391 614.334 0.361 Amp2 7.339 0.97 5.052 1.620 1.010 574.368 0.180 注:温度计算采用Blundy and Holland(1990),压力计算采用Schmidt(1992). 表 4 胶北地块斜长角闪岩锆石(09LY21)LA-ICP-MS U-Pb分析结果
Table 4. LA-ICP-MS zircon U-Pb dating data from amphibolite (09LY21) in Jiaobei terrane
测点号 Th (10-6) U (10-6) Th/U 206Pb/238U ±(%) 207Pb/235U ±(%) 207Pb/206Pb ±(%) 206Pb/238U σ 207Pb/235U σ 207Pb/206Pb σ 1 2 492 3 464 0.72 0.379 7 1.4 6.706 2 1.5 0.128 0 3.0 2 075 25 2 073 13 2 071 52 2 153 854 0.18 0.304 0 1.5 4.833 3 2.1 0.115 3 3.3 1 711 23 1 791 18 1 884 59 3 1 934 4 477 0.43 0.346 6 1.4 5.597 3 1.4 0.117 1 3.0 1 918 23 1 916 12 1 912 53 4 70 463 0.15 0.331 0 1.4 5.277 0 1.6 0.115 6 3.1 1 843 23 1 865 14 1 889 54 5 257 990 0.26 0.311 3 2.5 4.592 3 4.6 0.106 9 5.2 1 747 38 1 748 39 1 748 93 8 119 692 0.17 0.332 2 1.4 5.183 2 1.4 0.113 1 3.0 1 849 22 1 850 12 1 850 53 9 645 2 483 0.26 0.277 4 1.3 4.371 5 1.3 0.114 3 2.9 1 578 19 1 707 11 1 869 52 10 87 521 0.17 0.333 8 1.4 5.221 1 1.4 0.113 4 3.0 1 857 22 1 856 12 1 855 53 13 160 1 019 0.16 0.332 2 1.3 5.179 5 1.3 0.113 1 2.9 1 849 21 1 849 11 1 849 52 14 72 531 0.13 0.322 6 1.3 5.006 0 1.4 0.112 5 3.0 1 802 21 1 820 12 1 841 53 15 72 630 0.11 0.327 2 1.4 5.031 1 1.5 0.111 5 3.0 1 825 22 1 825 13 1 824 53 16 73 583 0.13 0.326 6 1.3 5.020 6 1.4 0.111 5 3.0 1 822 21 1 823 12 1 824 53 17 76 495 0.15 0.324 3 1.4 4.990 9 1.4 0.111 6 3.0 1 811 21 1 818 12 1 826 53 18 80 578 0.14 0.337 8 1.6 5.379 2 2.2 0.115 5 3.4 1 876 26 1 882 19 1 887 60 22 309 1 098 0.28 0.327 4 1.3 5.031 8 1.3 0.111 5 2.9 1 826 21 1 825 11 1 823 52 25 94 698 0.13 0.330 5 1.3 5.141 1 1.3 0.112 8 2.9 1 841 21 1 843 11 1 845 52 26 284 1 163 0.24 0.331 2 1.3 5.138 2 1.3 0.112 5 2.9 1 844 21 1 842 11 1 840 52 27 502 8 560 0.06 0.329 3 1.3 5.094 5 1.3 0.112 2 2.9 1 835 21 1 835 11 1 836 51 28 1 162 6 966 0.17 0.328 5 1.3 5.083 2 1.3 0.112 2 2.9 1 831 21 1 833 11 1 836 51 29 139 808 0.17 0.326 2 1.3 5.006 0 1.3 0.111 3 2.9 1 820 21 1 820 11 1 821 52 30 96 671 0.14 0.321 3 1.3 4.860 9 1.4 0.109 7 2.9 1 796 21 1 796 12 1 795 52 表 5 胶北地块斜长角闪岩锆石(09LY21)LA-ICP-MS稀土元素和微量元素测试结果(10-6)
Table 5. LA-ICP-MS zircon REE and mean trace-element data from amphibolite (09LY21) in Jiaobei terrane
测点号 Y Nb La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Hf Ta ∑REE Lu/Hf Eu/Eu* Ce/Ce* (La/Yb)N (La/Sm)N (Gd/Yb)N 1 896.26 6.89 5.930 37.33 4.360 30.30 11.36 42.820 26.73 4.99 50.27 20.36 108.95 28.76 347.04 75.96 10 240.90 4.680 795 0.007 4 7.23 1.72 0.012 26 0.337 0 0.063 7 2 803.52 4.04 2.100 22.20 1.421 10.44 5.08 12.180 16.64 4.98 59.37 24.03 114.76 26.00 268.41 53.84 9 139.18 1.544 621 0.005 9 3.68 3.05 0.005 61 0.266 9 0.051 3 3 1 039.40 6.69 8.460 39.92 4.340 25.03 9.59 75.62 20.61 5.00 56.85 24.55 140.50 39.23 494.88 103.04 11 184.80 3.330 1 048 0.009 2 16.00 1.60 0.012 26 0.569 5 0.034 5 4 476.81 1.94 0.056 8.82 0.065 0.36 1.07 1.070 6.08 2.92 36.69 15.46 76.73 17.37 188.11 36.54 9 612.42 1.088 391 0.003 8 1.01 31.31 0.000 21 0.033 8 0.026 7 5 486.96 2.53 1.553 14.53 0.900 5.92 2.58 13.24 8.76 2.82 34.75 14.55 73.01 17.80 196.21 38.31 9 994.19 1.589 425 0.003 8 7.67 2.96 0.005 68 0.388 6 0.036 9 8 1 205.55 2.87 0.040 12.69 0.053 0.80 2.23 0.618 15.36 6.97 91.29 38.66 192.59 43.32 452.66 90.09 8 542.40 1.125 947 0.010 5 0.24 57.07 0.000 06 0.011 6 0.028 1 9 2 183.22 11.68 7.720 76.47 6.380 38.20 16.63 14.48 47.52 14.82 173.80 67.13 302.14 65.15 648.09 123.50 9 513.55 5.390 1 602 0.013 0 1.47 2.51 0.008 54 0.299 7 0.060 7 10 683.12 3.48 2.090 17.56 0.976 5.03 2.17 2.130 10.18 3.89 52.50 21.66 106.15 24.44 253.41 49.40 8 815.19 1.630 552 0.005 6 1.15 3.01 0.005 92 0.621 8 0.033 2 13 1 255.94 3.58 0.130 14.94 0.199 2.41 2.93 1.140 17.53 7.38 95.88 39.32 192.06 43.54 451.31 89.52 8 854.67 1.364 958 0.010 1 0.38 18.47 0.000 21 0.028 6 0.032 1 14 663.97 2.20 0 9.05 0.034 0.44 1.46 0.444 10.01 4.06 52.00 21.20 102.27 23.77 250.83 50.39 8 959.63 0.951 526 0.005 6 0.26 82.64 0 0 0.033 0 15 631.57 1.95 0.031 8.90 0.033 0.68 1.48 0.570 11.35 4.09 50.69 20.13 97.41 22.25 239.10 46.83 9 011.79 1.260 504 0.005 2 0.30 60.83 0.000 09 0.013 5 0.039 3 16 571.47 1.74 0 9.27 0.023 0.56 1.70 0.424 9.89 4.06 46.29 18.50 87.24 19.56 208.52 41.24 8 707.77 0.988 447 0.004 7 0.25 125.13 0 0 0.039 2 17 716.62 1.99 0 9.31 0.025 0.42 1.83 0.456 12.49 4.57 56.26 23.15 111.07 25.80 267.63 54.41 8 347.96 1.126 567 0.006 5 0.22 115.61 0 0 0.038 6 18 729.30 2.10 0.341 9.88 0.044 0.65 1.90 0.469 12.13 4.50 57.07 23.23 112.34 25.77 273.43 54.50 9 074.33 1.006 576 0.006 0 0.23 16.98 0.000 89 0.115 9 0.036 7 22 778.78 3.33 1.053 14.29 0.033 0.39 1.72 0.253 11.33 4.52 59.06 23.96 116.42 27.04 281.43 56.10 10 141.30 2.480 598 0.005 5 0.13 9.75 0.002 68 0.395 2 0.033 3 25 905.36 3.23 0.656 11.49 0.258 1.54 1.79 0.539 12.00 5.21 68.45 29.07 143.97 33.40 343.88 69.16 10 769.70 2.040 721 0.006 4 0.27 6.85 0.001 37 0.236 6 0.028 9 26 1 554.97 6.35 0.329 24.19 0.307 2.95 4.19 1.150 24.08 9.51 122.14 50.44 238.31 52.63 526.29 102.32 8 983.52 2.060 1 159 0.011 4 0.27 17.11 0.000 45 0.050 7 0.037 9 27 720.19 3.47 0.925 6.88 0.564 4.33 3.81 2.300 15.21 5.02 56.08 20.56 92.63 20.42 205.60 37.53 7 314.13 1.870 472 0.005 1 0.80 2.28 0.003 23 0.156 7 0.061 2 28 3 104.76 29.68 3.620 54.77 2.800 20.72 14.67 20.660 58.31 20.05 244.33 94.93 449.34 102.61 1075.63 196.70 11 053.50 15.240 2 359 0.017 8 1.88 4.00 0.002 41 0.159 3 0.044 8 29 1 265.33 4.50 0.037 14.55 0.051 0.77 2.36 0.736 16.72 7.20 95.13 40.16 196.53 44.70 464.46 91.96 8 938.02 1.577 975 0.010 3 0.26 68.62 0.000 06 0.010 1 0.029 8 30 1 007.91 2.98 0.131 10.91 0.068 0.87 2.11 0.610 13.79 5.81 77.21 32.29 158.11 36.06 376.80 72.03 8 838.76 1.369 787 0.008 1 0.26 28.11 0.000 25 0.040 1 0.030 3 -
[1] Blundy, J.D., Holland, T.J.B., 1990.Calcic Amphibole Equilibria and a New Amphibole-Plagioclase Geothermometer.Contributions to Mineralogy and Petrology, 104(2):208-224. https://doi.org/10.1007/bf00306444 [2] Cai, J., Liu, P.H., Ji, L., et al., 2017.Zircon Geochronology of the Paleoproterozoic High-Grade Supercrustal Rocks from the Huai'an Terrane, Northwestern Hebei.Acta Petrologica Sinica, 33(9):2811-2826 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20170911 [3] Cao, Z.Q., Zhai, W.J., Jiang, X.F., et al., 2016.About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance.Earth Science, 41(4):570-585 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201604002.htm [4] Chen, N., Liao, F., Wang, L., et al., 2013.Late Paleoproterozoic Multiple Metamorphic Events in the Quanji Massif:Links with Tarim and North China Cratons and Implications for Assembly of the Columbia Supercontinent.Precambrian Research, 228:102-116. https://doi.org/10.1016/j.precamres.2013.01.03 [5] Cheng, S.H., You, Z.D., 2016.Metamorphic Petrology.Geological Publishing House, Beijing, 53 (in Chinese). [6] Dong, C.Y., Ma, M.Z., Liu, S.J., et al., 2012.Middle Paleoproterozoic Crustal Extensional Regime in the North China Craton:New Evidence from SHRIMP Zircon U-Pb Dating and Whole-Rock Geochemistry of Meta-gabbro in the Anshan-Gongchangling Area.Acta Petrologica Sinica, 28(9):2785-2792 (in Chinese with English abstract). http://www.oalib.com/paper/1474278 [7] Dong, C.Y., Wang, S.J., Liu, D.Y., et al., 2011.Late Palaeoproterozoic Crustal Evolution of the North China Craton and Formation Time of the Jingshan Group:Constraints from SHRIMP U-Pb Zircon Dating of Meta-Intermediate-Basic Intrusive Rocks in Eastern Shandong Province.Acta Petrologica Sinica, 27(6):1699-1706 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20110611 [8] Faure, M., Lin, W., Monié, P., et al., 2004.Palaeoproterozoic Arc Magmatism and Collision in Liaodong Peninsula (North-East China).Terra Nova, 16(2):75-80. https://doi.org/10.1111/j.1365-3121.2004.00533.x [9] Green, E.C.R., White, R.W., Diener, J.F.A., et al., 2016.Activity-Composition Relations for the Calculation of Partial Melting Equilibria in Metabasic Rocks.Journal of Metamorphic Geology, 34(9):845-869. https://doi.org/10.13039/100004807 [10] Hoskin, P.W.O., Schaltegger, U., 2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Reviews in Mineralogy and Geochemistry, 53(1):27-62. https://doi.org/10.2113/0530027 [11] Jahn, B.M., Liu, D., Wan, Y., et al., 2008.Archean Crustal Evolution of the Jiaodong Peninsula, China, as Revealed by Zircon SHRIMP Geochronology, Elemental and Nd-Isotope Geochemistry.American Journal of Science, 308(3):232-269. https://doi.org/10.2475/03.2008.03 [12] Jin, S.Q., 1991.Composition Characteristics of Calc-Amphiboles in Different Regional Metamorphic Facies.Chinese Science Bulletin, 36(11):851-854 (in Chinese). [13] Kong, F.M., Liu, Y., Li, X.P., et al., 2015.Mineralogical and Petrogeochemical Characteristics of Ultramafic Rocks from the Metamorphic Basement of the Jiaobei Terrane.Acta Petrologica Sinica, 31(6):1549-1563 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-YSXB201506005.htm [14] Leake, B.E., Woolley, A.R., Arps, C.E.S., et al., 1997.Nomenclature of Amphiboles Report of the Subcommittee on Amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names.European Journal of Mineralogy, 9(3):623-651. https://doi.org/10.1127/ejm/9/3/0623 [15] Li, S.Z., Zhao, G.C., 2007.SHRIMP U-Pb Zircon Geochronology of the Liaoji Granitoids:Constraints on the Evolution of the Paleoproterozoic Jiao-Liao-Ji Belt in the Eastern Block of the North China Craton.Precambrian Research, 158(1/2):1-16. https://doi.org/10.1016/j.precamres.2007.04.001 [16] Li, S.Z., Zhao, G.C., Sun, M., et al., 2005.Deformation History of the Paleoproterozoic Liaohe Assemblage in the Eastern Block of the North China Craton.Journal of Asian Earth Sciences, 24(5):659-674. https://doi.org/10.1016/j.jseaes.2003.11.008 [17] Li, X.P., Guo, J.H., Zhao, G.C., et al., 2011.Formation of the Paleoproterozoic Calc-Silicate and High-Pressure Mafic Granulite in the Jiaobei Terrane, Eastern Shandong, China.Acta Petrologica Sinica, 27(4):961-968 (in Chinese with English abstract). http://www.oalib.com/paper/1474220 [18] Li, X.P., Liu, Y., Guo, J.H., et al., 2013.Petrogeochemical Characteristics of the Paleoproterozoic High-Pressure Mafic Granulite and Calc-Silicate from the Nanshankou of the Jiaobei Terrane.Acta Petrologica Sinica, 29(7):2340-2352 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201307007.htm [19] Li, X.P., Rahn, M., Bucher, K., 2004.Metamorphic Processes in Rodingites of the Zermatt-Saas Ophiolites.International Geology Review, 46(1):28-51. https://doi.org/10.2747/0020-6814.46.1.28 [20] Li, X.P., Zhang, L., Wei, C., et al., 2007.Petrology of Rodingite Derived from Eclogite in Western Tianshan, China.Journal of Metamorphic Geology, 25(3):363-382. https://doi.org/10.1111/j.1525-1314.2007.00700.x [21] Liati, A., Gebauer, D., 1999.Constraining the Prograde and Retrograde P-T-t Path of Eocene HP Rocks by SHRIMP Dating of Different Zircon Domains:Inferred Rates of Heating, Burial, Cooling and Exhumation for Central Rhodope, Northern Greece.Contributions to Mineralogy and Petrology, 135(4):340-354. https://doi.org/10.1007/s004100050516 [22] Liu, F.L., Liu, P.H., Ding, Z.J., et al., 2012.Genetic Mechanism of Granitic Leucosome within High-Pressure Granulite from the Early Precambrian Metamorphic Basement of Shandong Peninsula, SE North China Craton.Acta Petrologica Sinica, 28(9):2686-2696 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201209003.htm [23] Liu, F.L., Liu, P.H., Wang, F., et al., 2014.U-Pb Dating of Zircons from Granitic Leucosomes in Migmatites of the Jiaobei Terrane, Southwestern Jiao-Liao-Ji Belt, North China Craton:Constraints on the Timing and Nature of Partial Melting.Precambrian Research, 245:80-99. https://doi.org/10.1016/j.precamres.2014.01.001 [24] Liu, F.L., Liu, P.H., Wang, F., et al., 2015.Progresses and Overviews of Voluminous Meta-Sedimentary Series within the Paleoproterozoic Jiao-Liao-Ji Orogenic/Mobile Belt, North China Craton.Acta Petrologica Sinica, 31(10):2816-2846 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-YSXB201510002.htm [25] Liu, F.L., Robinson, P.T., Gerdes, A., et al., 2010.Zircon U-Pb Ages, REE Concentrations and Hf Isotope Compositions of Granitic Leucosome and Pegmatite from the North Sulu UHP Terrane in China:Constraints on the Timing and Nature of Partial Melting.Lithos, 117(1/2/3/4):247-268. https://doi.org/10.1016/j.lithos.2010.03.002 [26] Liu, J.H., Liu, F.L., Ding, Z.J., et al., 2014.U-Pb Dating and Hf Isotope Study of Early Archean Zircons from the Jiaobei Terrane, North China Craton:Evidence for Growth and Recycling of Ancient Continental Crust.Acta Petrologica Sinica, 30(10):2941-2950 (in Chinese with English abstract). [27] Liu, J.H., Liu, F.L., Ding, Z.J, et al., 2015.Early Precambrian Major Magmatic Events, and Growth and Evolution of Continental Crust in the Jiaobei Terrane, North China Craton.Acta Petrologica Sinica, 31(10):2942-2958 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-YSXB201510006.htm [28] Liu, J.H., Liu, F.L., Liu, P.H., et al., 2011.Polyphase Magmatic and Metamorphic Events from Early Precambrian Metamorphic Basement in Jiaobei Area:Evidences from the Zircon U-Pb Dating of TTG and Granitic Gneisses.Acta Petrologica Sinica, 27(4):943-960 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201104008.htm [29] Liu, P.H., Cai, J., Zou, L., 2017.Metamorphic P-T-t Path and Its Geological Implication of the Sanjiazi Garnet Amphibolites from the Northern Liaodong Penisula, Jiao-Liao-Ji Belt:Constraints on Phase Equilibria and Zircon U-Pb Dating.Acta Petrologica Sinica, 33(9):2649-2674 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-YSXB201709001.htm [30] Liu, P.H., Liu, F.L., Liu, C.H., et al., 2013.Petrogenesis, P-T-t Path, and Tectonic Significance of High-Pressure Mafic Granulites from the Jiaobei Terrane, North China Craton.Precambrian Research, 233:237-258. https://doi.org/10.13039/501100001809 [31] Liu, P.H., Liu, F.L., Wang, F., et al., 2010.Genetic Mineralogy and Metamorphic Evolution of Mafic High-Pressure (HP) Granulites from the Shandong Peninsula, China.Acta Petrologica Sinica, 26(7):2039-2056 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20100707 [32] Liu, P.H., Liu, F.L., Wang, F., et al., 2012.Geochemical Characteristics and Genesis of the High-Pressure Mafic Granulite in the Jiaobei High-Grade Metamorphic Basement, Eastern Shandong, China.Acta Petrologica Sinica, 28(9):2705-2720 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20120904 [33] Liu, P.H., Liu, F.L., Wang, F., et al., 2013.Petrological and Geochronological Preliminary Study of the Xiliu~2.1 Ga Meta-Gabbro from the Jiaobei Terrane, the Southern Segment of the Jiao-Liao-Ji Belt in the North China Craton.Acta Petrologica Sinica, 29(7):2371-2390 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201307009.htm [34] Liu, P.H., Liu, F.L., Wang, F., et al., 2014.Preliminary Study of Petrology and U-Pb Zircon Dating of the Nanshankou Garnet-Bearing Pyroxenolites from the Jiaobei Terrane, the Southeastern Segment of the Jiao-Liao-Ji Belt in the North China Craton.Acta Petrologica Sinica, 30(10):2951-2972 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201410012.htm [35] Liu, P.H., Liu, F.L., Wang, F., et al., 2015.P-T-t Paths of the Multiple Metamorphic Events of the Jiaobei Terrane in the Southeastern Segment of the Jiao-Liao-Ji Belt(JLJB), in the North China Craton:Implication for Formation and Evolution of the JLJB.Acta Petrologica Sinica, 31(10):2889-2941 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201510005.htm [36] Liu, S.J., Jahn, B.M., Wan, Y.S., et al., 2015.Neoarchean to Paleoproterozoic High-Pressure Mafic Granulite from the Jiaodong Terrain, North China Craton:Petrology, Zircon Age Determination and Geological Implications.Gondwana Research, 28(2):493-508. https://doi.org/10.13039/501100001809 [37] Liu, W.J., Zhai, M.G., Li, Y.G., 1998.Metamorphism of the High-Pressure Basic Granulites in Laixi, Eastern Shandong, China.Acta Petrologica Sinica, 14(4):449-459 (in Chinese with English abstract). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_ysxb98199804005 [38] Luo, Y., Sun, M., Zhao, G.C., et al., 2004.LA-ICP-MS U-Pb Zircon Ages of the Liaohe Group in the Eastern Block of the North China Craton:Constraints on the Evolution of the Jiao-Liao-Ji Belt.Precambrian Research, 134(3/4):349-371. https://doi.org/10.1016/j.precamres.2004.07.002 [39] Luo, Y., Sun, M., Zhao, G.C., et al., 2008.A Comparison of U-Pb and Hf Isotopic Compositions of Detrital Zircons from the North and South Liaohe Groups:Constraints on the Evolution of the Jiao-Liao-Ji Belt, North China Craton.Precambrian Research, 163(3/4):279-306. https://doi.org/10.1016/j.precamres.2008.01.002 [40] Meng, E., Liu, F.L., Liu, P.H., et al., 2014.Petrogenesis and Tectonic Significance of Paleoproterozoic Meta-Mafic Rocks from Central Liaodong Peninsula, Northeast China:Evidence from Zircon U-Pb Dating and In Situ Lu-Hf Isotopes, and Whole-Rock Geochemistry.Precambrian Research, 247:92-109. https://doi.org/10.1016/j.precamres.2014.03.017 [41] Powell, R., Holland, T., Worley, B., 1998.Calculating Phase Diagrams Involving Solid Solutions via Non-Linear Equations, with Examples Using THERMOCALC.Journal of Metamorphic Geology, 16(4):577-588. https://doi.org/10.1111/j.1525-1314.1998.00157.x [42] Powell, R., White, R.W., Green, E.C.R., et al., 2014.On Parameterizing Thermodynamic Descriptions of Minerals for Petrological Calculations.Journal of Metamorphic Geology, 32(3):245-260. https://doi.org/10.1111/jmg.12070 [43] Sang, L.K., Ma, C.Q., 2012.Petrology (2nd Edition).Geological Publishing House, Beijing, 478 (in Chinese). [44] Schmidt, M.W., 1992.Amphibole Composition in Tonalite as a Function of Pressure:An Experimental Calibration of the Al-in-Hornblende Barometer.Contributions to Mineralogy and Petrology, 110(2/3):304-310. https://doi.org/10.1007/bf00310745 [45] Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society, London, Special Publications, 42(1):313-345. https://doi.org/10.1144/gsl.sp.1989.042.01.19 [46] Tam, P.Y., Zhao, G.C., Liu, F.L., et al., 2011.Timing of Metamorphism in the Paleoproterozoic Jiao-Liao-Ji Belt:New SHRIMP U-Pb Zircon Dating of Granulites, Gneisses and Marbles of the Jiaobei Massif in the North China Craton.Gondwana Research, 19(1):150-162. https://doi.org/10.1016/j.gr.2010.05.007 [47] Tam, P.Y., Zhao, G.C., Sun, M., et al., 2012a.Metamorphic P-T Path and Tectonic Implications of Medium-Pressure Pelitic Granulites from the Jiaobei Massif in the Jiao-Liao-Ji Belt, North China Craton.Precambrian Research, 220-221:177-191. https://doi.org/10.1016/j.precamres.2012.08.008 [48] Tam, P.Y., Zhao, G.C., Sun, M., et al., 2012b.Petrology and Metamorphic P-T Path of High-Pressure Mafic Granulites from the Jiaobei Massif in the Jiao-Liao-Ji Belt, North China Craton.Lithos, 155:94-109. https://doi.org/10.1016/j.lithos.2012.08.018 [49] Tam, P.Y., Zhao, G.C., Zhou, X.W., et al., 2012c.Metamorphic P-T Path and Implications of High-Pressure Pelitic Granulites from the Jiaobei Massif in the Jiao-Liao-Ji Belt, North China Craton.Gondwana Research, 22(1):104-117. https://doi.org/10.1016/j.gr.2011.09.006 [50] Tang, J., Zheng, Y.F., Wu, Y.B., et al., 2007.Geochronology and Geochemistry of Metamorphic Rocks in the Jiaobei Terrane:Constraints on Its Tectonic Affinity in the Sulu Orogen.Precambrian Research, 152(1/2):48-82. https://doi.org/10.1016/j.precamres.2006.09.001 [51] Wan, Y.S., Song, B., Liu, D.Y., et al., 2006.SHRIMP U-Pb Zircon Geochronology of Palaeoproterozoic Metasedimentary Rocks in the North China Craton:Evidence for a Major Late Palaeoproterozoic Tectonothermal Event.Precambrian Research, 149(3/4):249-271. https://doi.org/10.1016/j.precamres.2006.06.006 [52] Wang, F., Liu, F.L., Liu, P.H., et al., 2010.Metamorphic Evolution of Early Precambrian Khondalite Series in North Shandong Province.Acta Petrologica Sinica, 26(7):2057-2072 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201007009.htm [53] Watson, E.B., Wark, D.A., Thomas, J.B., 2006.Crystallization Thermometers for Zircon and Rutile.Contributions to Mineralogy and Petrology, 151(4):413-433. https://doi.org/10.1007/s00410-006-0068-5 [54] Whitney, D.L., Evans, B.W., 2010.Abbreviations for Names of Rock-Forming Minerals.American Mineralogist, 95(1):185-187. https://doi.org/10.2138/am.2010.3371 [55] Wu, Y.B., Zheng, Y.F., 2004.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age.Chinese Science Bulletin, 49(15):1554-1569. https://doi.org/10.1007/bf03184122 [56] Yang, F.C., Sun, J.G., Song, Y.H., et al., 2016.SHRIMP U-Pb Age, Hf Isotope Composition and Geochemical Characteristics of Neoarchean Granitic Complex in Liaodong Lianshanguan Area, NE China.Earth Science, 41(12):2008-2018 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DQKX201612005.htm [57] Yui, T.F., Maki, K., Usuki, T., et al., 2010.Genesis of Guatemala Jadeitite and Related Fluid Characteristics:Insight from Zircon.Chemical Geology, 270(1/2/3/4):45-55. https://doi.org/10.1016/j.chemgeo.2009.11.004 [58] Zeh, A., Gerdes, A., Barton, J.Jr, et al., 2010.U-Th-Pb and Lu-Hf Systematics of Zircon from TTG's, Leucosomes, Meta-Anorthosites and Quartzites of the Limpopo Belt (South Africa):Constraints for the Formation, Recycling and Metamorphism of Palaeoarchaean Crust.Precambrian Research, 179(1/2/3/4):50-68. https://doi.org/10.1016/j.precamres.2010.02.012 [59] Zhai, M.G., 2009.Two Kinds of Granulites (HT-HP and HT-UHT) in North China Craton:Their Genetic Relation and Geotectonic Implications.Acta Petrologica Sinica, 25(8):1753-1771 (in Chinese with English abstract). http://www.oalib.com/paper/1472671 [60] Zhai, M.G., 2010.Tectonic Evolution and Metallogenesis of North China Craton.Mineral Deposits, 29(1):24-36 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KCDZ201001005.htm [61] Zhao, G.C., Cawood, P.A., Li, S.Z., et al., 2012.Amalgamation of the North China Craton:Key Issues and Discussion.Precambrian Research, 222-223:55-76. https://doi.org/10.1016/j.precamres.2012.09.016 [62] Zhao, G.C., Guo, J.H., 2012.Precambrian Geology of China:Preface.Precambrian Research, 222-223:1-12. https://doi.org/10.1016/j.precamres.2012.09.018 [63] Zhao, G.C., Sun, M., Wilde, S.A., et al., 2005.Late Achaean to Paleoproterozoic Evolution of the North China Craton:Key Issues Revisited.Precambrian Research, 136(2):177-202. doi: 10.1016/j.precamres.2004.10.002 [64] Zhao, G.C., Wilde, S.A., Cawood, P.A., et al., 1998.Thermal Evolution of Archean Basement Rocks from the Eastern Part of the North China Craton and Its Bearing on Tectonic Setting.International Geology Review, 40(8):706-721. https://doi.org/10.1080/00206819809465233 [65] Zhao, G.C., Wilde, S.A., Cawood, P.A., et al., 2001.Archean Blocks and Their Boundaries in the North China Craton:Lithological, Geochemical, Structural and P-T Path Constrains and Tectonic Evolution.Precambrian Research, 107:45-73. doi: 10.1016/S0301-9268(00)00154-6 [66] Zhao, G.C., Zhai, M.G., 2013.Lithotectonic Elements of Precambrian Basement in the North China Craton:Review and Tectonic Implications.Gondwana Research, 23(4):1207-1240. https://doi.org/10.1016/j.gr.2012.08.016 [67] Zhao, L., Li, T.S., Peng, P., et al., 2015.Anatomy of Zircon Growth in High Pressure Granulites:SIMS U-Pb Geochronology and Lu-Hf Isotopes from the Jiaobei Terrane, Eastern North China Craton.Gondwana Research, 28(4):1373-1390. https://doi.org/10.13039/501100001809 [68] Zhou, X., Zhao, G., Wei, C., et al., 2008.EPMA U-Th-Pb Monazite and SHRIMP U-Pb Zircon Geochronology of High-Pressure Pelitic Granulites in the Jiaobei Massif of the North China Craton.American Journal of Science, 308(3):328-350. https://doi.org/10.2475/03.2008.06 [69] Zhou, X.W., Wei, C.J., Geng, Y.S., 2007.Phase Equilibria P-T Path of the High-and Low-Pressure Pelitic Granulites from the Jiaobei Massif.Earth Science Frontiers, 14(1):135-143 (in Chinese with English abstract). http://www.academia.edu/563643/Prograde_Symplectites_in_High-Temperature_Low-Pressure_Metamorphism_Bushveld_Complex_South_Africa_ [70] Zhou, X.W., Wei, C.J., Geng, Y.S., et al., 2004.Discovery and Implications of the High-Pressure Pelitic Granulite from the Jiaobei Massif.Chinese Science Bulletin, 49(18):1424-1430 (in Chinese). doi: 10.1007/BF03184286.pdf [71] 蔡佳, 刘平华, 冀磊, 等, 2017.冀西北怀安地体高级变质表壳岩的锆石年代学研究.岩石学报, 33(9):2811-2826. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20170911&journal_id=ysxb&year_id=2017 [72] 曹正琦, 翟文建, 蒋幸福, 等, 2016.华北克拉通南缘约2.5Ga构造变质事件及意义.地球科学, 41(4):570-585. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dqkx201604002&dbname=CJFD&dbcode=CJFQ [73] 程素华, 游振东, 2016.变质岩岩石学.北京:地质出版社, 53. [74] 董春艳, 马铭株, 刘守偈, 等, 2012.华北克拉通古元古代中期伸展体制新证据:鞍山-弓长岭地区变质辉长岩的锆石SHRIMP U-Pb定年和全岩地球化学.岩石学报, 28(9):2785-2792. http://mall.cnki.net/magazine/Article/YSXB201209010.htm [75] 董春艳, 王世进, 刘敦一, 等, 2011.华北克拉通古元古代晚期地壳演化和荆山群形成时代制约——胶东地区变质中-基性侵入岩锆石SHRIMP U-Pb定年.岩石学报, 27(6):1699-1706. http://mall.cnki.net/magazine/Article/YSXB201106011.htm [76] 靳是琴, 1991.不同区域变质相中钙质角闪石的成分特征.科学通报, 36(11):851-854. http://www.cqvip.com/qk/94252x/199111/552666.html [77] 孔凡梅, 刘云, 李旭平, 等, 2015.胶北地块变质基底超镁铁岩的矿物岩石地球化学特征.岩石学报, 31(6):1549-1563. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20150605&journal_id=ysxb [78] 李旭平, 郭敬辉, 赵国春, 等, 2011.胶北地块早元古代钙硅酸盐岩与高压基性麻粒岩成因及地质意义.岩石学报, 27(4):961-968. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_ysxb98201104005 [79] 李旭平, 刘云, 郭敬辉, 等, 2013.胶北南山口古元古代高压基性麻粒岩和钙硅酸盐岩的岩石地球化学特征探讨.岩石学报, 29(7):2340-2352. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20130706&journal_id=ysxb&year_id=2013 [80] 刘福来, 刘平华, 丁正江, 等, 2012.山东半岛高压麻粒岩中花岗质浅色脉体的成因.岩石学报, 28(9):2686-2696. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20120902 [81] 刘福来, 刘平华, 王舫, 等, 2015.胶-辽-吉古元古代造山/活动带巨量变沉积岩系的研究进展.岩石学报, 31(10):2816-2846. http://mall.cnki.net/magazine/Article/YSXB201510002.htm [82] 刘建辉, 刘福来, 丁正江, 等, 2014.胶北太古宙早期锆石U-Pb定年及Hf同位素研究:华北克拉通古老陆壳增生及再循环的证据.岩石学报, 30(10):2941-2950. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20141011&journal_id=ysxb&year_id=2014 [83] 刘建辉, 刘福来, 丁正江, 等, 2015.胶北地体早前寒武纪重大岩浆事件、陆壳增生及演化.岩石学报, 31(10):2942-2958. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20151006&journal_id=ysxb&year_id=2015 [84] 刘建辉, 刘福来, 刘平华, 等, 2011.胶北早前寒武纪变质基底多期岩浆-变质热事件:来自TTG片麻岩和花岗质片麻岩中锆石U-Pb定年的证据.岩石学报, 27(4):943-960. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201104004 [85] 刘平华, 蔡佳, 邹雷, 2017.辽东半岛北部三家子石榴斜长角闪岩变质演化P-T-t轨迹及其地质意义:来自相平衡模拟与锆石U-Pb定年的约束.岩石学报, 33(9):2649-2674. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201709001&dbname=CJFD&dbcode=CJFQ [86] 刘平华, 刘福来, 王舫, 等, 2010.山东半岛基性高压麻粒岩的成因矿物学及变质演化.岩石学报, 26(7):2039-2056. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201007007 [87] 刘平华, 刘福来, 王舫, 等, 2012.胶北高级变质基底中高压基性麻粒岩的地球化学特征及其成因.岩石学报, 28(9):2705-2720. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20120904 [88] 刘平华, 刘福来, 王舫, 等, 2013.胶北西留古元古代~2.1Ga变辉长岩岩石学与年代学初步研究.岩石学报, 29(7):2371-2390. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20130708&journal_id=ysxb&year_id=2013 [89] 刘平华, 刘福来, 王舫, 等, 2014.胶北南山口含榴辉石岩岩石学与锆石U-Pb定年的初步研究.岩石学报, 30(10):2951-2972. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20141012 [90] 刘平华, 刘福来, 王舫, 等, 2015.胶北地体多期变质事件的P-T-t轨迹及其对胶-辽-吉带形成与演化的制约.岩石学报, 31(10):2889-2941. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201510005&dbname=CJFD&dbcode=CJFQ [91] 刘文军, 翟明国, 李永刚, 1998.胶东莱西地区高压基性麻粒岩的变质作用.岩石学报, 14(4):449-459. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_ysxb98199804005 [92] 桑隆康, 马昌前, 2012.岩石学(第二版).北京:地质出版社, 478. [93] 王舫, 刘福来, 刘平华, 等, 2010.胶北地区早前寒武纪孔兹岩系的变质演化.岩石学报, 26(7):2057-2072. http://industry.wanfangdata.com.cn/yj/Detail/Periodical?id=Periodical_ysxb98201007008 [94] 杨凤超, 孙景贵, 宋运红, 等, 2016.辽东连山关地区新太古代花岗杂岩SHRIMP U-Pb年龄、Hf同位素组成及地质意义.地球科学, 41(12):2008-2018. http://www.earth-science.net/WebPage/Article.aspx?id=3397 [95] 翟明国, 2009.华北克拉通两类早前寒武纪麻粒岩(HT-HP和HT-UHT)及其相关问题.岩石学报, 25(8):1753-1771. http://www.cnki.com.cn/Article/CJFDTotal-YSXB200908005.htm [96] 翟明国, 2010.华北克拉通的形成演化与成矿作用.矿床地质, 29(1):24-36. http://www.doc88.com/p-084374723035.html [97] 周喜文, 魏春景, 耿元生, 2007.胶北地块高压与低压泥质麻粒岩的相平衡关系与P-T演化轨迹.地学前缘, 14(1):135-143. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dxqy200701013&dbname=CJFD&dbcode=CJFQ [98] 周喜文, 魏春景, 耿元生, 等, 2004.胶北栖霞地区泥质高压麻粒岩的发现及其地质意义.科学通报, 49(14):1424-1430. doi: 10.3321/j.issn:0023-074X.2004.14.015