Neoarchean-Paleoproterozoic Multi-Stage Geological Events and Their Tectonic Implications in the Fuping Complex, North China Craton
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摘要: 本文收集了阜平杂岩新太古代早期-古元古代晚期基底岩石的岩石地球化学、锆石U-Pb年代学、同位素地球化学和变质作用资料，以期对阜平杂岩早寒武纪演化历史进行初步总结.阜平新太古代早期~2.7 Ga片麻岩原岩为英云闪长岩，具有TTG质片麻岩的地球化学特征；其锆石εHf（t）具有较高的正值（+5.44~+7.50），单阶段模式年龄为2 745~2 824 Ma，表明新太古代早期为阜平杂岩强烈的地壳生长时期.新太古代晚期片麻岩的时代集中于2 543~2 484 Ma，主要岩石类型为英云闪长岩-奥长花岗岩-花岗闪长岩（TTG），同时区域内还存在二长花岗岩.TTG质片麻岩的εNd（t）值为-1.64~+0.96，单阶段模式年龄为2.76~3.04 Ga；锆石εHf（t）值为-1.9~+7.91，单阶段和两阶段模式年龄分别为2 546~2 888 Ma和2 548~3 119 Ma.这些TTG岩石主要为新太古代早期岩石的部分熔融，并有少量中太古代地壳物质参与.近于同期具有岛弧性质的辉长岩和变质作用暗示阜平杂岩新太古代晚期可能经历了俯冲和弧-陆或陆-陆碰撞.古元古代中期（2.1~2.0 Ga）阜平地区花岗质岩浆活动强烈.该阶段花岗岩具有A型花岗岩特征，与同期的火山-沉积岩系形成于华北克拉通古元古代中期伸展的陆内裂谷环境中.阜平杂岩中基性麻粒岩包体记录的变质作用时代为1.89~1.85 Ga，并具有顺时针演化的P-T轨迹，其代表了古元古代晚期裂谷闭合的陆内造山过程，表明华北最终克拉通化.Abstract: In this paper, we summarize the evolutionary history on Fuping Complex from the early Neoarchean to late Paleoproterozoic by comprehensive analyses of data collected on its geochemistry, zircon U-Pb dating, isotopic geochemistry and metamorphism. It is found that the protolith of ca. 2.7 Ga gneisses are tonalite with the geochemical features of TTG, and zircons in these gneisses show positive εHf(t) values of 5.44 to 7.50, with single stage model age (TDM) of 2 745-2 824 Ma, which indicates the intensive crustal growth in early Neoarchean in the Fuping Complex. The late Neoarchean gneisses yield the age of 2 543-2 484 Ma and are mainly composed of tonalite-trondjemite-granodiorite (TTG) besides some monzogranite. TTG gneisses have εNd(t) values ranging from -1.64 to +0.96, with single stage model age (TDM) of 2.76-3.04 Ga, and zircon εHf(t) of -1.9-+7.91, with single stage model age (THf1) and two stage model age (THf2) of 2 546-2 888 Ma and 2 548-3 119 Ma, respectively. Thus, these TTG are derived from partial melting of the early Neoarchean rocks with some addition of Mesoarchean crust. Gabbro coeval with TTG gneisses displays the features of island arc magma and ca. 2.5 Ga metamorphism in Neoarchean supracrustal rocks, suggesting that the Fuping Complex underwent subduction and arc-continent or continent-continent collision in late Neoarchean. 2.1-2.0 Ga granitoids widely occur in the Fuping Complex with the feartures of A-type granite and the simultaneous volcanic-sedimentary rocks formed intra-continental rift environment in middle Paleoproterozoic. Mafic granulite enclaves in the Fuping Complex yield metamorphic age of 1.89-1.85 Ga and show clockwise P-T paths, which represents closure of intra-continent rifts and cratonization of the North China Craton in late Paleoproterozoic.
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Key words:
- Fuping Complex /
- early Neoarchean to late Paleoproterozoic /
- TTG gneisses /
- A-type granite /
- P-T path /
- cratonization /
- geochemistry
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图 1 阜平杂岩地质简图(左上角插图引自Zhao et al., 2005)
Fig. 1. Geological sketch map of the Fuping Complex (figure on upper left after Zhao et al., 2005)
图 2 阜平杂岩新太古代-古元古代岩石中锆石U⁃Pb年龄统计直方图
Fig. 2. Histogram of zircon U⁃Pb ages from late Archean to Paleoproterozoic rocks in the Fuping Complex
图 3 阜平杂岩新太古代片麻岩野外露头照片
a.新太古代早期(2.7 Ga)条带状英云闪长质片麻岩；b.新太古代晚期(2.5 Ga)条带状英云闪长质片麻岩；c.新太古代早期(2.7 Ga)细粒角闪黑云斜长片麻岩(麻河清岩组)；d.新太古代早期(2.7 Ga)细粒黑云斜长片麻岩(阜平岩群)
Fig. 3. Outcrop photos of Neoarchean gneisses in the Fuping Complex
图 4 阜平杂岩新太古代晚期和古元古代中期花岗质岩石野外照片
a.条带状黑云斜长片麻岩(英云闪长质)；b.变形较弱的石英闪长质片麻岩；c.南营花岗质片麻岩中伟晶岩脉穿插；d.岗南片麻岩中磁铁矿特征暗色矿物；e.岗南片麻岩中局部角闪石聚集；f.古元古代中期花岗岩穿切条带状片麻岩后两者又经历变形；g.白羊岭花岗岩中伟晶岩穿切；h.白羊岭花岗岩中条带状片麻岩包体
Fig. 4. Outcrop photos of late Neoarchean and middle Paleoproterozoic grantiods in the Fuping Complex
图 5 阜平杂岩新太古代-古元古代岩石锆石207Pb/206Pb年龄与εHf(t)关系
Fig. 5. Zircon 207Pb/206Pb ages vs. εHf(t) plots of late Archean to Paleoproterozoic rocks in the Fuping Complex
图 6 阜平杂岩新太古代和古元古代花岗质片麻岩207Pb/206Pb年龄与εNd(t)关系(图中数据引自Liu et al. (2002))
Fig. 6. `207Pb/206Pb ages vs. εNd(t) plots of late Archean and Paleoproterozoic granitic gneisses in the Fuping Complex (data from Liu et al. (2002))
表 1 阜平杂岩新太古代-古元古代锆石U⁃Pb年龄统计
Table 1. Statistics on zircon U⁃Pb ages from Neoarchean to Paleoproterozoic in the Fuping Complex
样品号 岩性 测试方法 成岩年龄 变质年龄 文献来源 F117-1 黑云斜长片麻岩(英云闪长质) LA-MC-ICPMS锆石U⁃Pb 2 674±20 Ma 路增龙等, 2014 FP50 角闪斜长片麻岩(英云闪长质) SHRIMP锆石U⁃Pb 2 708±8 Ma Guan et al., 2002 08CWW05 TTG质片麻岩 LA-MC-ICPMS锆石U⁃Pb 2 753±35 Ma Han et al., 2012 08CWW04 TTG质片麻岩 LA-MC-ICPMS锆石U⁃Pb 2 535±14 Ma Han et al., 2012 FP54 黑云斜长片麻岩(奥长花岗质) SHRIMP锆石U⁃Pb 2 513±12 Ma Guan et al., 2002 FP08 黑云斜长片麻岩(花岗闪长质) SHRIMP锆石U⁃Pb 2.5 Ga 1 817±26 Ma Guan et al., 2002 FG1 英云闪长质片麻岩 SHRIMP锆石U⁃Pb 2 523±14 Ma 1 802±43 Ma Zhao et al., 2002 FP217 奥长花岗质片麻岩 SHRIMP锆石U⁃Pb 2 499±6 Ma 1 875±43 Ma Zhao et al., 2002 FP216 花岗闪长质片麻岩 SHRIMP锆石U⁃Pb 2 486±8 Ma 1 825±12 Ma Zhao et al., 2002 FP236 龙泉关眼球状二长花岗片麻岩 SHRIMP锆石U⁃Pb 2 510±22 Ma Zhao et al., 2002 FP224 糜棱岩化花岗伟晶岩脉 SHRIMP锆石U⁃Pb 2 507±11 Ma Zhao et al., 2002 WL9 龙泉关眼球状花岗闪长质片麻岩 SHRIMP锆石U⁃Pb 2 540±18 Ma 王凯怡等, 1997 WN11 龙泉关眼球状花岗闪长质片麻岩 SHRIMP锆石U⁃Pb 2 541±4 Ma 王凯怡等, 1997 WL12 龙泉关眼球状花岗闪长质片麻岩 SHRIMP锆石U⁃Pb 2 543±7 Ma 王凯怡等, 1997 F0045-6 英云闪长质片麻岩 SHRIMP锆石U⁃Pb 2 537±10 Ma 1 802±43 Ma 杨崇辉等, 2004 F01-84-3 糜棱岩化花岗闪长质片麻岩 SHRIMP锆石U⁃Pb 2 526±15 Ma 程裕淇等, 2004 F004 长英质麻粒岩 SHRIMP锆石U⁃Pb 2 538±14 Ma, 1 829±32 Ma 程裕淇等, 2004 F103 英云闪长质片麻岩 TIMS锆石U⁃Pb 2 484±37 Ma 吴昌华等, 2000 FP7 TTG片麻岩 LA-ICPMS锆石U⁃Pb 2 513±13 Ma Tang et al., 2016 FP-29-1 含辉石角闪石岩 LA-ICPMS锆石U⁃Pb 2 514±15 Ma Tang et al., 2016 HB412 平阳奥长花岗质片麻岩 SIMS锆石U⁃Pb 2 513±6 Ma Meng et al., 2017 HB416 平阳奥长花岗质片麻岩 SIMS锆石U⁃Pb 2 525±15 Ma 1 856±9 Ma Meng et al., 2017 HB422 平阳奥长花岗质片麻岩 SIMS锆石U⁃Pb 2 523±5 Ma Meng et al., 2017 F02-2 浅粒岩 LA-MC-ICPMS锆石U⁃Pb 2 531±15 Ma, 1 943±16 Ma 王建龙等, 2020 FP30 岗南片麻状花岗岩 SHRIMP锆石U⁃Pb 2 045±64 Ma Guan et al., 2002 F188-2 南营花岗质片麻岩 SHRIMP锆石U⁃Pb 2 077±13 Ma 1 826±12 Ma Zhao et al., 2002 F204 南营花岗质片麻岩 SHRIMP锆石U⁃Pb 2 024±21 Ma 1 850±9.6 Ma Zhao et al., 2002 FP-1-1 片麻状花岗岩 LA-ICPMS锆石U⁃Pb 2 055±21 Ma 1 891±44 Ma Tang et al., 2015 FP3 片麻状正长花岗岩 LA-ICPMS锆石U⁃Pb 2 077±16 Ma Tang et al., 2015 F17-1 南营花岗质片麻岩 SHRIMP锆石U⁃Pb 2 075±13 Ma Wang et al., 2020 F20-1 南营花岗质片麻岩 SHRIMP锆石U⁃Pb 2 079±9 Ma Wang et al., 2020 F22-1 南营花岗质片麻岩 SHRIMP锆石U⁃Pb 2 073±10 Ma Wang et al., 2020 F05-2 岗南片麻状花岗岩 SHRIMP锆石U⁃Pb 2 081±8 Ma Wang et al., 2020 F08-1 岗南片麻状花岗岩 SHRIMP锆石U⁃Pb 2 082±14 Ma Wang et al., 2020 F39-1 岗南片麻状花岗岩 SHRIMP锆石U⁃Pb 2 063±7 Ma Wang et al., 2020 F10-1 白羊岭花岗岩 SHRIMP锆石U⁃Pb 2 077±6 Ma Wang et al., 2020 F32-1 白羊岭花岗岩 SHRIMP锆石U⁃Pb 2 070±19 Ma 1 823±24 Ma Wang et al., 2020 F33-1 白羊岭花岗岩 SHRIMP锆石U⁃Pb 2 069±12 Ma Wang et al., 2020 F14-1 上庄花岗岩 SHRIMP锆石U⁃Pb 2 072±12 Ma Wang et al., 2020 F38-1 上庄花岗岩 SHRIMP锆石U⁃Pb 2 070±12 Ma 1 867±24 Ma Wang et al., 2020 F005 变质基性岩脉 SHRIMP锆石U⁃Pb 1 819.4±8.2 Ma 程裕淇等, 2004 F9913 变质基性岩脉 SHRIMP锆石U⁃Pb 1 823±11 Ma 程裕淇等, 2004 FG2 花岗伟晶岩脉 SHRIMP锆石U⁃Pb 1 790±8 Ma 王凯怡等, 1997 I9711-1B 花岗伟晶岩脉 TIMS锆石U⁃Pb 1 799±7 Ma 刘树文等, 2000 F01101-1 钠质伟晶岩脉 SHRIMP锆石U⁃Pb 1 872±19 Ma 李基宏等, 2004 F01101-2 钾质伟晶岩脉 SHRIMP锆石U⁃Pb 1 885±37 Ma 李基宏等, 2004 F1510 镁铁质麻粒岩 SIMS锆石U⁃Pb 1 891±14 Ma, 1 849±6 Ma Qian et al., 2018 HB339 镁铁质麻粒岩 SIMS锆石U⁃Pb 1 885±22 Ma Meng et al., 2017 HB351 镁铁质麻粒岩 SIMS锆石U⁃Pb 1 862±12 Ma Meng et al., 2017 HB402 镁铁质麻粒岩 SIMS锆石U⁃Pb 1 859±38 Ma Meng et al., 2017 
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