Neoarchean-Paleoproterozoic Multi-Stage Geological Events and Their Tectonic Implications in the Fuping Complex, North China Craton
-
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.
-
Key words:
- Fuping Complex /
- early Neoarchean to late Paleoproterozoic /
- TTG gneisses /
- A-type granite /
- P-T path /
- cratonization /
- geochemistry
-
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 
下载: 导出CSV
-
[1] Cheng, Y. Q., Yang, C. H., Wan, Y. S., et al., 2004. Early Precambrian Geological Characters and Anatectic Reconstruction of Crust in North Part of Middle Taihang Mountain. Geological Publishing House, Beijing (in Chinese). [2] Condie, K. C., 1998. Episodic Continental Growth and Supercontinents: A Mantle Avalanche Connection?. Earth and Planetary Science Letters, 163(1-4): 97-108. https://doi.org/10.1016/s0012⁃821x(98)00178⁃2 doi: 10.1016/s0012⁃821x(98)00178⁃2 [3] Condie, K. C., O'Neill, C., Aster, R. C., 2009. Evidence and Implications for a Widespread Magmatic Shutdown for 250 My on Earth. Earth and Planetary Science Letters, 282(1-4): 294-298. https://doi.org/10.1016/j.epsl.2009.03.033" target="_blank"> https://doi.org/10.1016/j.epsl.2009.03.033 [4] Diwu, C. R., Liu, X., Sun, Y., 2018. The Composition and Evolution of the Taihua Complex in the Southern North China Craton. Acta Petrologica Sinica, 34(4): 999-1018 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201804011.htm [5] Diwu, C. R., Sun, Y., Zhao, Y., et al., 2014. Early Paleoproterozoic (2.45-2.20 Ga) Magmatic Activity during the Period of Global Magmatic Shutdown: Implications for the Crustal Evolution of the Southern North China Craton. Precambrian Research, 255: 627-640. https://doi.org/10.1016/j.precamres.2014.08.001" target="_blank"> https://doi.org/10.1016/j.precamres.2014.08.001 [6] Dong, S. W., Zhang, Y. Q., Zhang, F. Q., et al., 2015. Late Jurassic–Early Cretaceous Continental Convergence and Intracontinental Orogenesis in East Asia: A Synthesis of the Yanshan Revolution. Journal of Asian Earth Sciences, 114: 750-770. https://doi.org/10.1016/j.jseaes.2015.08.011" target="_blank"> https://doi.org/10.1016/j.jseaes.2015.08.011 [7] Dong, X. J., Xu, Z. Y., Liu, Z. H., et al., 2012. 2.7 Ga Granitic Gneiss in the Northern Foot of Daqingshan Mountain, Central Inner Mongolia, and Its Geological Implications. Earth Science, 37(S1): 20-27 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx2012z1003 [8] Du, L. L., Yang, C. H., Song, H. X., et al., 2018. Petrogenesis and Tectonic Setting of 2.2-2.1 Ga Granites in Wutai Area, North China Craton. Acta Petrologica Sinica, 34(4): 1154-1174 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201804016 [9] Du, L. L., Yang, C. H., Wang, W., et al., 2011. The Reexamination of the Age and Stratigraphic Subdivision of the Hutuo Group in the Wutai Mountains Area, North China Craton: Evidences from Geology and Zircon U⁃Pb Geochronology. Acta Petrologica Sinica, 27(4): 1037-1055 (in Chinese with English abstract). [10] Du, L. L., Yang, C. H., Wyman, D. A., et al., 2015. Petrogenesis and Tectonic Implications of the Iron⁃Rich Tholeiitic Basalts in the Hutuo Group of the Wutai Mountains, Central Trans⁃North China Orogen. Precambrian Research, 271: 225-242. https://doi.org/10.1016/j.precamres.2015.10.008" target="_blank"> https://doi.org/10.1016/j.precamres.2015.10.008 [11] Du, L. L., Yang, C. H., Wyman, D. A., et al., 2016a. Age and Depositional Setting of the Paleoproterozoic Gantaohe Group in Zanhuang Complex: Constraints from Zircon U–Pb Ages and Hf Isotopes of Sandstones and Dacite. Precambrian Research, 286: 59-100. https://doi.org/10.1016/j.precamres.2016.09.027" target="_blank"> https://doi.org/10.1016/j.precamres.2016.09.027 [12] Du, L. L., Yang, C. H., Wyman, D. A., et al., 2016b. 2 090-2 070 Ma A⁃Type Granitoids in Zanhuang Complex: Further Evidence on a Paleoproterozoic Rift⁃Related Tectonic Regime in the Trans⁃North China Orogen. Lithos, 254-255: 18-35. https://doi.org/10.1016/j.lithos.2016.03.007" target="_blank"> https://doi.org/10.1016/j.lithos.2016.03.007 [13] Du, L. L., Yang, C. H., Wyman, D. A., et al., 2017. Zircon U⁃Pb Ages and Lu⁃Hf Isotope Compositions from Clastic Rocks in the Hutuo Group: Further Constraints on Paleoproterozoic Tectonic Evolution of the Trans⁃North China Orogen. Precambrian Research, 303: 291-314. https://doi.org/10.1016/j.precamres.2017.04.007" target="_blank"> https://doi.org/10.1016/j.precamres.2017.04.007 [14] Du, L. L., Zhuang, Y. X., Yang, C. H., et al., 2003. Characters of Zircons in the Mengjiatun Formation in Xintai of Shandong and Their Chronological Significance. Acta Geologica Sinica, 77(3): 359-366 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200303007 [15] Duan, Q. S., Du, L. L., Song, H. X., et al., 2020. Geochronology and Geochemistry of the Metavolcanic Rocks at Lengkou Area, Zhongtiao Mountains: Implications for Magmatic and Tectonic Setting in the Paleoproterozoic Magmatic Quiescence in the North China Craton. Precambrian Research, under review. [16] Faure, M., Trap, P., Lin, W., et al., 2007. Polyorogenic Evolution of the Paleoproterozoic Trans⁃North China Belt. Episodes, 30(2): 96-107. doi: 10.18814/epiiugs/2007/v30i2/004 [17] Geng, Y. S., Shen, Q. H., Ren, L. D., 2010. Late Neoarchean to Early Paleoproterozoic Magmatic Events and Tectonothermal Systems in the North China Craton. Acta Petrologica Sinica, 26(7): 1945-1966 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201007001 [18] Guan, H., Sun, M., Wilde, S. A., et al., 2002. SHRIMP U⁃Pb Zircon Geochronology of the Fuping Complex: Implications for Formation and Assembly of the North China Craton. Precambrian Research, 113(1-2): 1-18. https://doi.org/10.1016/s0301⁃9268(01)00197⁃8 doi: 10.1016/s0301⁃9268(01)00197⁃8 [19] Han, B. F., Xu, Z., Ren, R., et al., 2012. Crustal Growth and Intracrustal Recycling in the Middle Segment of the Trans⁃North China Orogen, North China Craton: A Case Study of the Fuping Complex. Geological Magazine, 149(4): 729–742. https://doi.org/10.1017/s0016756811001014" target="_blank"> https://doi.org/10.1017/s0016756811001014 [20] 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" target="_blank"> https://doi.org/10.2475/03.2008.03 [21] Kröner, A., Wilde, S. A., Li, J. H., et al., 2005. Age and Evolution of a Late Archean to Paleoproterozoic Upper to Lower Crustal Section in the Wutaishan/Hengshan/Fuping Terrain of Northern China. Journal of Asian Earth Sciences, 24(5): 577-595. https://doi.org/10.1016/j.jseaes.2004.01.001" target="_blank"> https://doi.org/10.1016/j.jseaes.2004.01.001 [22] Kusky, T., Li, J. H., Santosh, M., 2007. The Paleoproterozoic North Hebei Orogen: North China Craton's Collisional Suture with the Columbia Supercontinent. Gondwana Research, 12(1-2): 4-28. https://doi.org/10.1016/j.gr.2006.11.012" target="_blank"> https://doi.org/10.1016/j.gr.2006.11.012 [23] Li, J. H., Yang, C. H., Du, L. L., 2004. Genesis and SHRIMP U⁃Pb Geochronology of Zircons from Pegmatites of Anatexis in Pingshan County, Hebei Province. Progress in Natural Science, 14(7): 774-781 (in Chinese). [24] Liu, D. Y., Nutman, A. P., Compston, W., et al., 1992. Remnants of ≥3 800 Ma Crust in the Chinese Part of the Sino⁃Korean Craton. Geology, 20(4): 339-342. https://doi.org/10.1130/0091⁃7613(1992)0200339:romcit>2.3.co;2 doi: 10.1130/0091⁃7613(1992)0200339:romcit>2.3.co;2 [25] Liu, D. Y., Page, R. W., Compston, W., et al., 1984. U⁃Pb Zircon Geochronology of Precambrian Metamorphic Rocks in the Taihangshan⁃Wutaishan Area, North China. Bulletin of the Chinese Academy of Geological Sciences, (8): 55-82 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB198401004.htm [26] Liu, D. Y., Page, R. W., Compston, W., et al., 1985. U⁃Pb Zircon Geochronology of Late Archaean Metamorphic Rocks in the Taihangshan: Wutaishan Area, North China. Precambrian Research, 27(1-3): 85-109. https://doi.org/10.1016/0301⁃9268(85)90007⁃5 doi: 10.1016/0301⁃9268(85)90007⁃5 [27] Liu, D. Y., Wilde, S. A., Wan, Y. S., et al., 2009. Combined U⁃Pb, Hafnium and Oxygen Isotope Analysis of Zircons from Meta⁃Igneous Rocks in the Southern North China Craton Reveal Multiple Events in the Late Mesoarchean⁃Early Neoarchean. Chemical Geology, 261(1-2): 140-154. https://doi.org/10.1016/j.chemgeo.2008.10.041" target="_blank"> https://doi.org/10.1016/j.chemgeo.2008.10.041 [28] Liu, J. H., Liu, F. L., Ding, Z. J., et al., 2013. The Growth, Reworking and Metamorphism of Early Precambrian Crust in the Jiaobei Terrane, the North China Craton: Constraints from U⁃Th⁃Pb and Lu⁃Hf Isotopic Systematics, and REE Concentrations of Zircon from Archean Granitoid Gneisses. Precambrian Research, 224: 287-303. https://doi.org/10.1016/j.precamres.2012.10.003" target="_blank"> https://doi.org/10.1016/j.precamres.2012.10.003 [29] Liu, J. H., Zhang, Q. W. L., Zhang, H. C. G., et al., 2019. Metamorphic Evolution and SHRIMP U⁃Pb Geochronology of Mafic Granulites with Double Symplectites in the Fuping Metamorphic Complex, Middle Palaeoproterozoic Trans⁃North China Orogen. Precambrian Research, 326: 142-154. https://doi.org/10.1016/j.precamres.2017.11.009" target="_blank"> https://doi.org/10.1016/j.precamres.2017.11.009 [30] Liu, S. W., 1996. Study on the P⁃T⁃t Path of Granulites in Fuping Area, Hebei Province. Geological Journal of China Universities, 2(1): 75-84 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX601.007.htm [31] Liu, S. W., Liang, H. H., Hua, Y. G., 1999. Fluid⁃Rock Equilibrium System of Archean Wanzi Rock Series in Taihang Mountains. Acta Scientiarum Naturalium Universitatis Pekinensis, 35(2): 259-264 (in Chinese with English abstract). [32] Liu, S. W., Liang, H. H., Zhao, G. C., et al., 2000. Isotopic Chronology and Geological Events of Precambrian Complex in Taihangshan Region. Science in China (Series D), 30(1): 18-24 (in Chinese). http://d.wanfangdata.com.cn/Periodical_zgkx-ed200004006.aspx [33] Liu, S. W., Pan, Y. M., Li, J. H., et al., 2002. Geological and Isotopic Geochemical Constraints on the Evolution of the Fuping Complex, North China Craton. Precambrian Research, 117(1-2): 41-56. https://doi.org/10.1016/s0301⁃9268(02)00063⁃3 doi: 10.1016/s0301⁃9268(02)00063⁃3 [34] Liu, S. W., Pan, Y. M., Xie, Q. L., et al., 2004. Archean Geodynamics in the Central Zone, North China Craton: Constraints from Geochemistry of Two Contrasting Series of Granitoids in the Fuping and Wutai Complexes. Precambrian Research, 130(1-4): 229-249. https://doi.org/10.1016/j.precamres.2003.12.001" target="_blank"> https://doi.org/10.1016/j.precamres.2003.12.001 [35] Liu, S. W., Pan, Y. M., Xie, Q. L., et al., 2005. Geochemistry of the Paleoproterozonic Nanying Granitic Gneisses in the Fuping Complex: Implications for the Tectonic Evolution of the Central Zone, North China Craton. Journal of Asian Earth Sciences, 24(5): 643-658. https://doi.org/10.1016/j.jseaes.2003.10.010" target="_blank"> https://doi.org/10.1016/j.jseaes.2003.10.010 [36] Lu, S. N., Chen, Z. H., Xiang, Z. Q., 2008. Geochronological Framework of Ancient Intrusions in Taishan Geopark, China. Geological Publishing House, Beijing (in Chinese). [37] Lu, Z. L., Song, H. X., Du, L. L., et al., 2014. Delineation of the Ca. 2.7 Ga TTG Gneisses in the Fuping Complex, North China Craton and Its Geological Significance. Acta Petrologica Sinica, 30(10): 2872-2884 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201410007 [38] Ma, M. Z., Xu, Z. Y., Zhang, L. C., et al., 2013. SHRIMP Dating and Hf Isotope Analysis of Zircons from the Early Precambrian Basement in the Xi Ulanbulang Area, Wuchuan, Inner Mongolia. Acta Petrologica Sinica, 29(2): 501-516 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201302011 [39] Martin, H., Smithies, R. H., Rapp, R., et al., 2005. An Overview of Adakite, Tonalite–Trondhjemite–Granodiorite (TTG), and Sanukitoid: Relationships and some Implications for Crustal Evolution. Lithos, 79(1-2): 1-24. https://doi.org/10.1016/j.lithos.2004.04.048" target="_blank"> https://doi.org/10.1016/j.lithos.2004.04.048 [40] Meng, J., Peng, T., Liu, J. H., et al., 2017. Metamorphic Evolution and SIMS Zircon U⁃Pb Geochronology of Mafic Granulite and Amphibolite Enclaves of the Pingyang Trondhjemitic Pluton, Fuping Terrane, North China. Precambrian Research, 303: 75-90. https://doi.org/10.1016/j.precamres.2017.02.014" target="_blank"> https://doi.org/10.1016/j.precamres.2017.02.014 [41] Mo, X. X., Zhao, Z. D., DePaolo, D. J., et al., 2006. Three Types of Collisional and Post⁃Collisional Magmatism in the Lhasa Block, Tibet and Implications for India Intra⁃Continental Subduction and Mineralization: Evidence from Sr⁃Nd Isotopes. Acta Petrologica Sinica, 22(4): 795-803 (in Chinese with English abstract). http://www.oalib.com/paper/1472307 [42] Nutman, A. P., Wan, Y. S., Du, L. L., et al., 2011. Multistage Late Neoarchaean Crustal Evolution of the North China Craton, Eastern Hebei. Precambrian Research, 189(1-2): 43-65. https://doi.org/10.1016/j.precamres.2011.04.005" target="_blank"> https://doi.org/10.1016/j.precamres.2011.04.005 [43] Peng, P., Guo, J. H., Zhai, M. G., et al., 2012. Genesis of the Hengling Magmatic Belt in the North China Craton: Implications for Paleoproterozoic Tectonics. Lithos, 148: 27-44. https://doi.org/10.1016/j.lithos.2012.05.021" target="_blank"> https://doi.org/10.1016/j.lithos.2012.05.021 [44] Peng, P., Wang, X. P., Windley, B. F., et al., 2014. Spatial Distribution of ~1 950-1 800 Ma Metamorphic Events in the North China Craton: Implications for Tectonic Subdivision of the Craton. Lithos, 202-203: 250-266. https://doi.org/10.1016/j.lithos.2014.05.033" target="_blank"> https://doi.org/10.1016/j.lithos.2014.05.033 [45] Peng, P., Yang, S. Y., Su, X. D., et al., 2017. Petrogenesis of the 2 090 Ma Zanhuang Ring and Sill Complexes in North China: A Bimodal Magmatism Related to Intra⁃continental Process. Precambrian Research, 303: 153-170. https://doi.org/10.1016/j.precamres.2017.03.015" target="_blank"> https://doi.org/10.1016/j.precamres.2017.03.015 [46] Qian, J. H., Yin, C. Q., Zhang, J., et al., 2018. High⁃Pressure Granulites in the Fuping Complex of the Central North China Craton: Metamorphic P⁃T⁃t Evolution and Tectonic Implications. Journal of Asian Earth Sciences, 154: 255-270. https://doi.org/10.1016/j.jseaes.2017.12.027" target="_blank"> https://doi.org/10.1016/j.jseaes.2017.12.027 [47] Ren, L. D., Geng, Y. S., Du, L. L., et al., 2013. SHRIMP Data on Zircons from the Wanzi Series: Constraints on the Rock Formation Time and Implications of Migmatization at 2.1-2.0 Ga in the Fuping Complex, North China Craton. Journal of Asian Earth Sciences, 72: 203-215. https://doi.org/10.1016/j.jseaes.2012.12.041" target="_blank"> https://doi.org/10.1016/j.jseaes.2012.12.041 [48] Shen, B. F., Li, J. J., Lin, Y. X., et al., 2005. Sm⁃Nd Isotope Age of the Lower Fuping Group Complex and Its Geological Significance. Acta Geologica Sinica, 79(6): 784-789 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200506014.htm [49] Shen, Q. H., Geng, Y. S., Song, B., et al., 2005. New Information from the Surface Outcrops and Deep Crust of Archean Rocks of the North China and Yangtze Blocks, and Qinling⁃Dabie Orogenic Belt. Acta Geologica Sinica, 79(5): 616-627 (in Chinese with English abstract). [50] Shi, W., Zhang, Y. Q., Dong, S. W., et al., 2012. Intra⁃Continental Dabashan Orocline, Southwestern Qinling, Central China. Journal of Asian Earth Sciences, 46: 20-38. https://doi.org/10.1016/j.jseaes.2011.10.005" target="_blank"> https://doi.org/10.1016/j.jseaes.2011.10.005 [51] Song, B., Nutman, A. P., Liu, D. Y., et al., 1996. 3 800 to 2 500 Ma Crustal Evolution in the Anshan Area of Liaoning Province, Northeastern China. Precambrian Research, 78(1-3): 79-94. https://doi.org/10.1016/0301⁃9268(95)00070⁃4 doi: 10.1016/0301⁃9268(95)00070⁃4 [52] Song, H. X., Yang, C. H., Du, L. L., et al., 2018. Delineation of the ~2.7 Ga TTG Gneisses in Zanhuang Complex, Hebei Province, and Its Geological Significance. Acta Petrologica Sinica, 34(6): 1599-1611 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201806004.htm [53] Tang, L., Santosh, M., Teng, X. M., 2015. Paleoproterozoic (Ca. 2.1-2.0 Ga) Arc Magmatism in the Fuping Complex: Implications for the Tectonic Evolution of the Trans⁃North China Orogen. Precambrian Research, 268: 16-32. https://doi.org/10.1016/j.precamres.2015.07.001" target="_blank"> https://doi.org/10.1016/j.precamres.2015.07.001 [54] Tang, L., Santosh, M., Tsunogae, T., et al., 2016. Late Neoarchean Arc Magmatism and Crustal Growth Associated with Microblock Amalgamation in the North China Craton: Evidence from the Fuping Complex. Lithos, 248-251: 324-338. https://doi.org/10.1016/j.lithos.2016.01.022" target="_blank"> https://doi.org/10.1016/j.lithos.2016.01.022 [55] Trap, P., Faure, M., Lin, W., et al., 2012. Paleoproterozoic Tectonic Evolution of the Trans⁃North China Orogen: Toward a Comprehensive Model. Precambrian Research, 222-223: 191-211. https://doi.org/10.1016/j.precamres.2011.09.008" target="_blank"> https://doi.org/10.1016/j.precamres.2011.09.008 [56] Wan, Y. S., Dong, C. Y., Liu, D. Y., et al., 2012. Zircon Ages and Geochemistry of Late Neoarchean Syenogranites in the North China Craton: A Review. Precambrian Research, 222-223: 265-289. https://doi.org/10.1016/j.precamres.2011.05.001" target="_blank"> https://doi.org/10.1016/j.precamres.2011.05.001 [57] Wan, Y. S., Dong, C. Y., Wang, W., et al., 2010. Archean Basement and a Paleoproterozoic Collision Orogen in the Huoqiu Area at the Southeastern Margin of North China Craton: Evidence from Sensitive High Resolution Ion Micro⁃Probe U⁃Pb Zircon Geochronology. Acta Geologica Sinica (English Edition), 84(1): 91-104. https://doi.org/10.1111/j.1755⁃6724.2010.00173.x doi: 10.1111/j.1755⁃6724.2010.00173.x [58] Wan, Y. S., Liu, D. Y., Wang, S. J., et al., 2011. ∼2.7 Ga Juvenile Crust Formation in the North China Craton (Taishan⁃Xintai Area, Western Shandong Province): Further Evidence of an Understated Event from U⁃Pb Dating and Hf Isotopic Composition of Zircon. Precambrian Research, 186(1-4): 169-180. https://doi.org/10.1016/j.precamres.2011.01.015" target="_blank"> https://doi.org/10.1016/j.precamres.2011.01.015 [59] Wan, Y. S., Zhang, Y. H., Williams, I. S., et al., 2013. Extreme Zircon O Isotopic Compositions from 3.8 to 2.5 Ga Magmatic Rocks from the Anshan Area, North China Craton. Chemical Geology, 352: 108-124. https://doi.org/10.1016/j.chemgeo.2013.06.009" target="_blank"> https://doi.org/10.1016/j.chemgeo.2013.06.009 [60] Wang, J. L., Song, H. X., Duan, Q. S., et al., 2020. Zircon U⁃Pb⁃Hf Isotopic Characteristics of Leptite in the Fuping Group, Hebei Province, and Its Geological Significance. Acta Petrologica et Mineralogica, 39(3): 267-282 (in Chinese with English abstract). [61] Wang, J. L., Yang, C. H., Wyman, D. A., et al., 2020. Petrogenesis and Tectonic Implications of the 2.1-2.0 Ga Granitoids in Fuping Complex, North China Craton: Constraints from Petrology, Geochemistry and Zircon U⁃Pb⁃Hf Isotopes. Precambrian Research, 339: 105611. https://doi.org/10.1016/j.precamres.2020.105611" target="_blank"> https://doi.org/10.1016/j.precamres.2020.105611 [62] Wang, K. Y., Li, J. L., Liu, R. Q., 1991. Origin of the Fuping Gneisses. Scientia Geologica Sinica, (3): 254-267 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000368889 [63] Wang, K. Y., Hao, J., Zhou, S. P., et al., 1997. Constraints on the Wutaishan Orogen from SHRIMP Single Zircon Ages. Chinese Science Bulletin, 42(12): 1295-1298 (in Chinese). doi: 10.1360/csb1997-42-12-1295 [64] Wu, C. H., Li, H. M., Zhong, C. T., et al., 2000. TIMS U⁃Pb Single Zircon Ages for the Orthogneiss and the Paragneiss of Fuping Complex: Implications for Existence of the Paleoproterozoic Supracrustal Rocks in the Central Basement of North China Craton. Progress in Precambrian Research, 23(3): 129-139 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ200003000.htm [65] Wu, J. S., Geng, Y. S., Shen, Q. H., et al., 1998. Archean Geological Features and Modification Evolution of the China⁃Korean Paleocontinent. Geological Publishing House, Beijing (in Chinese). [66] Wu, J. S., Geng, Y. S., Xu, H. F., et al., 1989. Metamorphic Geology of the Fuping Group. Bulletin of the Institute of Geology Chinese Academy of Geological Sciences, (19): 1-213 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dldlx-e200102007 [67] Xia, X. P., Sun, M., Zhao, G. C., et al., 2006. U⁃Pb Age and Hf Isotope Study of Detrital Zircons from the Wanzi Supracrustals: Constraints on the Tectonic Setting and Evolution of the Fuping Complex, Trans⁃North China Orogen. Acta Geologica Sinica (English Edition), 80(6): 844-863. https://doi.org/10.1111/j.1755⁃6724.2006.tb00307.x doi: 10.1111/j.1755⁃6724.2006.tb00307.x [68] Xiao, L. L., Liu, F. L., Zhang, J., 2019. Response to the Early Neoarchean Tectono⁃Thermal Events in the North China Craton: Evidence of ca. 2.7 Ga TTG Gneisses from the Zuoquan Metamorphic Complex. Acta Petrologica Sinica, 35(2): 325-348 (in Chinese with English abstract). doi: 10.18654/1000-0569/2019.02.04 [69] Xie, H. Q., Liu, D. Y., Yin, X. Y., et al., 2012. Formation Age and Tectonic Environment of the Gantaohe Group, North China Craton: Geology, Geochemistry, SHRIMP Zircon Geochronology and Hf⁃Nd Isotopic Systematics. Chinese Science Bulletin, 57(36): 4735-4745. https://doi.org/10.1007/s11434⁃012⁃5482⁃7 doi: 10.1007/s11434⁃012⁃5482⁃7 [70] Xie, S. W., Xie, H. Q., Wang, S. J., et al., 2014. Ca. 2.9Ga Granitoid Magmatism in Eastern Shandong, North China Craton: Zircon Dating, Hf⁃in⁃Zircon Isotopic Analysis and Whole⁃Rock Geochemistry. Precambrian Research, 255: 538-562. https://doi.org/10.1016/j.precamres.2014.09.006" target="_blank"> https://doi.org/10.1016/j.precamres.2014.09.006 [71] Xu, W., Liu, F. L., 2019. Geochronological and Geochemical Insights into the Tectonic Evolution of the Paleoproterozoic Jiao⁃Liao⁃Ji Belt, Sino⁃Korean Craton. Earth⁃Science Reviews, 193: 162-198. https://doi.org/10.1016/j.earscirev.2019.04.019" target="_blank"> https://doi.org/10.1016/j.earscirev.2019.04.019 [72] Yang, C. H., Du, L. L., Geng, Y. S., et al., 2017. Paleoproterozoic Metamafic Dyke Swarms in the Eastern Hebei Massif, the Eastern North China Craton: ~2.1 Ga Extension and ~1.8 Ga Metamorphism. Acta Petrologica Sinica, 33(9): 2827-2849 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201709012.htm [73] Yang, C. H., Du, L. L., Ren, L. D., et al., 2013. Delineation of the Ca. 2.7 Ga TTG Gneisses in the Zanhuang Complex, North China Craton and Its Geological Implications. Journal of Asian Earth Sciences, 72: 178-189. https://doi.org/10.1016/j.jseaes.2012.09.031" target="_blank"> https://doi.org/10.1016/j.jseaes.2012.09.031 [74] Yang, C. H., Du, L. L., Song, H. X., et al., 2018. Stratigraphic Division and Correlation of the Pleoproterozoic Strata in the North China Craton: A Review. Acta Petrologica Sinica, 34(4): 1019-1057 (in Chinese with English abstract). http://www.researchgate.net/publication/330637994_Stratigraphic_division_and_correlation_of_the_Pleoproterozoic_strata_in_the_North_China_Craton_A_review [75] Yang, C. H., Du, L. L., Wan, Y. S., et al., 2004. SHRIMP Zircon U⁃Pb Chronology of Tonalitic Gneiss in Banqiaogou Area, Pingshan County, Hebei Province. Geological Journal of China Universities, 10(4): 514-522 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_geological-journal-china-universities_thesis/0201253567620.html [76] Yang, L. H., Hou, G. T., Liu, S. W., et al., 2019. 2.09 Ga Mafic Dykes from Western Shandong, Eastern Block of North China Craton, and Their Tectonic Implications.Precambrian Research, 325: 39-54. https://doi.org/10.1016/j.precamres.2019.02.007" target="_blank"> https://doi.org/10.1016/j.precamres.2019.02.007 [77] Zhai, M. G., Santosh, M., 2011. The Early Precambrian Odyssey of the North China Craton: A Synoptic Overview. Gondwana Research, 20(1): 6-25. https://doi.org/10.1016/j.gr.2011.02.005" target="_blank"> https://doi.org/10.1016/j.gr.2011.02.005 [78] Zhang, X. P., Wan, Y. S., Yang, C. H., 2003. Geology and Petrography of the Pingyang Gneissic Trondhjemite, Fuping, Hebei. Chinese Geology, 30(1): 61-71 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200301007 [79] Zhao, G. C., Wilde, S. A., Cawood, P. A., et al., 2002. SHRIMP U⁃Pb Zircon Ages of the Fuping Complex: Implications for Late Archean to Paleoproterozoic Accretion and Assembly of the North China Craton. American Journal of Science, 302(3): 191-226. https://https://doi.org/10.2475/ajs.302.3.191" target="_blank"> https://https://doi.org/10.2475/ajs.302.3.191 [80] Zhao, G. C., Sun, M., Wilde, S. A., et al., 2005. Late Archean to Paleoproterozoic Evolution of the North China Craton: Key Issues Revisited. Precambrian Research, 136(2): 177-202. https://doi.org/10.1016/j.precamres.2004.10.002" target="_blank"> https://doi.org/10.1016/j.precamres.2004.10.002 [81] 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" target="_blank"> https://doi.org/10.1016/j.gr.2012.08.016 [82] Zhu, X. Y., Zhai, M. G., Chen, F. K., et al., 2013. ∼2.7 Ga Crustal Growth in the North China Craton: Evidence from Zircon U⁃Pb Ages and Hf Isotopes of the Sushui Complex in the Zhongtiao Terrane. Journal of Geology, 121(3): 239-254. https://doi.org/10.1086/669977" target="_blank"> https://doi.org/10.1086/669977 [83] 程裕淇, 杨崇辉, 万渝生, 等, 2004.太行山中北段早前寒武纪地质和深熔作用对地壳岩石的改造.北京:地质出版社. [84] 第五春荣, 刘祥, 孙勇, 2018.华北克拉通南缘太华杂岩组成及演化.岩石学报, 34(4): 999-1018. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201804009 [85] 董晓杰, 徐仲元, 刘正宏, 等, 2012.内蒙古大青山北麓2.7 Ga花岗质片麻岩的发现及其地质意义.地球科学, 37(S1): 20-27. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx2012z1003 [86] 杜利林, 杨崇辉, 宋会侠, 等, 2018.华北克拉通五台地区2.2~2.1 Ga花岗岩的成因与构造背景.岩石学报, 34(4): 1154-1174. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201804018.htm [87] 杜利林, 杨崇辉, 王伟, 等, 2011.五台地区滹沱群时代与地层划分新认识:地质学与锆石年代学证据.岩石学报, 27(4): 1037-1055. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201104015.htm [88] 杜利林, 庄育勋, 杨崇辉, 等, 2003.山东新泰孟家屯岩组锆石特征及其年代学意义.地质学报, 77(3): 359-366. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200303007 [89] 耿元生, 沈其韩, 任留东, 2010.华北克拉通晚太古代末-古元古代初的岩浆事件及构造热体制.岩石学报, 26(7): 1945-1966. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201007001 [90] 李基宏, 杨崇辉, 杜利林, 2004.河北平山深熔伟晶岩锆石成因及SHRIMP U⁃Pb年龄.自然科学进展, 14(7): 774-781. http://www.cnki.com.cn/Article/CJFDTotal-ZKJZ200407010.htm [91] 刘敦一, Page, R. W., Compston, W., 等, 1984.太行山—五台山区前寒武纪变质岩系同位素地质年代学研究.中国地质科学院院报, (8): 55-82. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=HY000002240364 [92] 刘树文, 1996.阜平地区麻粒岩的P⁃T⁃t路径研究.高校地质学报, 2(1): 75-84. http://qikan.cqvip.com/Qikan/Article/Detail?id=2410756 [93] 刘树文, 梁海华, 华永刚, 1999.太行山太古宙湾子岩系的流体与岩石平衡体系.北京大学学报(自然科学版), 35(2): 259-264. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=bjdxxb199902021 [94] 刘树文, 梁海华, 赵国春, 等, 2000.太行山早前寒武纪杂岩的同位素年代学和地质事件.中国科学(D辑), 30(1): 18-24. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd200001003 [95] 陆松年, 陈志宏, 相振群, 2008.泰山世界地质公园:古老侵入岩系年代格架.北京:地质出版社. [96] 路增龙, 宋会侠, 杜利林, 等, 2014.华北克拉通阜平杂岩中~2.7 Ga TTG片麻岩的厘定及其地质意义.岩石学报, 30(10): 2872-2884. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201410007.htm [97] 马铭株, 徐仲元, 张连昌, 等, 2013.内蒙古武川西乌兰不浪地区早前寒武纪变质基底锆石SHRIMP定年及Hf同位素组成.岩石学报, 29(2): 501-516. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201302011 [98] 莫宣学, 赵志丹, DePaolo, D. J., 等, 2006.青藏高原拉萨地块碰撞-后碰撞岩浆作用的三种类型及其对大陆俯冲和成矿作用的启示: Sr⁃Nd同位素证据.岩石学报, 22(4): 795-803. http://www.cnki.com.cn/Article/CJFDTotal-YSXB200604004.htm [99] 沈保丰, 李俊建, 林源贤, 等, 2005.阜平岩群下部Sm⁃Nd同位素年龄及其地质意义.地质学报, 79(6): 784-789. http://www.cnki.com.cn/Article/CJFDTotal-DZXE200506014.htm [100] 沈其韩, 耿元生, 宋彪, 等, 2005.华北和扬子陆块及秦岭—大别造山带地表和深部太古宙基底的新信息.地质学报, 79(5): 616-627. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200505006 [101] 宋会侠, 杨崇辉, 杜利林, 等, 2018.河北赞皇杂岩中2.7 Ga TTG片麻岩的厘定及其地质意义.岩石学报, 34(6): 1599-1611. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201806004 [102] 王建龙, 宋会侠, 段庆松, 等, 2020.河北阜平杂岩中阜平岩群浅粒岩锆石U⁃Pb⁃Hf同位素特征及其地质意义.岩石矿物学杂志, 39(3): 267-282. https://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=CJFD&filename=YSKW202003002 [103] 王凯怡, 李继亮, 刘如琦, 1991.阜平片麻岩之成因.地质科学, (3): 254-267. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000368889 [104] 王凯怡, 郝杰, 周少平, 等, 1997.单颗粒锆石离子探针质谱定年结果对五台造山事件的制约.科学通报, 42(12): 1295-1298. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb199712017 [105] 吴昌华, 李惠民, 钟长汀, 等, 2000.阜平片麻岩和湾子片麻岩的单颗粒锆石U⁃Pb年龄——阜平杂岩并非一统太古宙基底的年代学证据.前寒武纪研究进展, 23(3): 129-139. https://www.ixueshu.com/document/4ee3fc474ee622783907b3d9175217ad318947a18e7f9386.html [106] 伍家善, 耿元生, 沈其韩, 等, 1998.中朝古大陆太古宙地质特征及构造演化.北京:地质出版社. [107] 伍家善, 耿元生, 徐惠芬, 等, 1989.阜平群变质地质.中国地质科学院地质研究所所刊, (19): 1-213. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ198900002001.htm [108] 肖玲玲, 刘福来, 张健, 2019.华北克拉通新太古代早期构造热事件的响应:来自左权地区Ca. 2.7 Ga TTG片麻岩的证据.岩石学报, 35(2): 325-348. https://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=CJFD&filename=YSXB201902004 [109] 杨崇辉, 杜利林, 耿元生, 等, 2017.冀东古元古代基性岩墙群的年龄及地球化学: ~2.1 Ga伸展及~1.8 Ga变质.岩石学报, 33(9): 2827-2849. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201709012.htm [110] 杨崇辉, 杜利林, 宋会侠, 等, 2018.华北克拉通古元古代地层划分与对比.岩石学报, 34(4): 1019-1057. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201804010 [111] 杨崇辉, 杜利林, 万渝生, 等, 2004.河北平山英云闪长质片麻岩锆石SHRIMP年代学.高校地质学报, 10(4): 514-521. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb200404004 [112] 张西平, 万渝生, 杨崇辉, 2003.河北阜平平阳片麻状奥长花岗岩的地质和岩相学特征.中国地质, 30(1): 61-72. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200301007 -
点击查看大图
图(6) / 表(1)
计量
- 文章访问数: 869
- HTML全文浏览量: 219
- PDF下载量: 105
- 被引次数: 0
