Petrogenesis and Tectonic Setting of Intermediate-Felsic Volcanics in Ta'erqi Area, Central Great Xing'an Range
-
摘要: 为探讨大兴安岭中段塔尔气地区中酸性火山岩成因及构造背景，深化大兴安岭中生代火山岩带的对比研究，对该地区满克头鄂博组、白音高老组火山岩开展了锆石U-Pb定年、岩石地球化学及Hf同位素分析.满克头鄂博组年龄为154±2 Ma和154±3 Ma，白音高老组年龄为132±2 Ma.样品富碱质，贫镁和钙，为弱过铝质.富K、Rb、Zr、Hf，贫Eu、Ba、Sr、P、Ti等元素，具有中等到较强的Eu负异常.锆石饱和温度平均值分别为915℃和841℃，表现出A型流纹岩的特点.样品εHf（t）值分别介于+6.9~+8.4和+6.7~+7.9，tDM2分别介于624~670 Ma和611~682 Ma，指示岩浆来源于新元古代亏损地幔增生年轻地壳物质.本地区满克头鄂博组形成于蒙古-鄂霍茨克洋闭合后伸展早期阶段，白音高老组则形成于蒙古-鄂霍茨克洋闭合后岩石圈伸展及拆沉作用，同时受到太平洋板块俯冲引发的弧后伸展作用叠加的影响.Abstract: In order to study the petrogenesis and tectonic setting of intermediate-felsic volcanics in Ta'erqi area, central Great Xing'an Range and promote the comparative study of Mesozoic volcanics in this region, in this paper it presents a synthesis study of zircon U-Pb chronology, geochemistry and Hf isotopes of volcanics from Manketouebo and Baiyingaolao formations. Zircon U-Pb dating yielded weighted mean ages of 154±2 Ma and 154±3 Ma of Manketouebo Formation and 132±2 Ma of Baiyingaolao Formation.The samples are weak peraluminous with high alkali, low Mg and Ca contents, while existing the enrichment of Rb, K, Zr, Hf and depletion of Eu, Sr, Ba, P, Ti with moderate to strong negative Eu anomalies. The average zirconium saturation temperature are 915 ℃ and 841 ℃, respectively, showing the characteristics of A-type rhyolite. The εHf(t) values range from +6.9 to +8.4 and +6.7 to +7.9, while the tDM2 values range from 624 Ma to 670 Ma and 611 Ma to 682 Ma, indicating that the magma originated from the the partial melting of Neoproterozoic young crust accreted from the depleted mantle. Manketouebo Formation in Ta'erqi area formed in the early stage of extensional tectonic setting after the closure of Mongolia-Okhotsk ocean, while Baiyingaolao Formation was caused by the lithosphere extension and delamination after the closure of the Mongolia-Okhotsk Ocean and the back-arc extension induced by the subduction of the paleo-Pacific plate to Eurasia.
-
Key words:
- central Great Xing'an Range /
- zircon U-Pb dating /
- Hf isotope /
- A-type rhyolites /
- lithosphere extension /
- deposits
-
图 1 工作区构造位置图(a)及工作区区域地质简图(b)
a图中，I.兴蒙造山带; I-1.额尔古纳地块; I-2.兴安地块; I-3.松辽地块; I-4.佳木斯地块; II.华北地块.①新林-喜桂图断裂; ②二连-贺根山断裂; ③西拉沐伦断裂; ④牡丹江断裂
Fig. 1. Tectonic location of study area (a) and simplified geological map of study area (b)
图 2 塔尔气地区满克头鄂博组(J3mk)地质剖面
1.浅灰色流纹质晶屑岩屑凝灰岩；2.紫红色流纹质晶屑岩屑凝灰熔岩；3.浅紫色流纹岩；4.紫灰色流纹质晶屑岩屑角砾凝灰熔岩；5.灰色英安质晶屑凝灰熔岩；6.灰色英安质晶屑熔岩
Fig. 2. Geological section map of Manketouebo Formation (J3mk) in Ta'erqi area
图 3 满克头鄂博组岩石手标本及显微照片
a.浅紫色流纹岩；b.紫红色流纹质晶屑凝灰熔岩；c.紫灰色流纹质晶屑凝灰岩，d.斑状结构；e.晶屑凝灰熔岩结构；f.晶屑凝灰结构；Bt.黑云母；Pl.斜长石；Q.石英；Sa.透长石
Fig. 3. Hand specimen photographs and micro photographs of Manketouebo Formation rock samples
图 4 塔尔气地区白音高老组(J3b)地质剖面
1.灰白色流纹质岩屑晶屑凝灰岩；2灰色流纹质岩屑晶屑角砾凝灰岩；3.灰白色流纹岩；4.浅灰色流纹质晶屑岩屑角砾凝灰熔岩；5.浅灰色流纹质晶屑熔岩；6.灰白色流纹质晶屑凝灰熔岩；7.紫红色流纹质岩屑晶屑角砾凝灰熔岩；8.灰白色流纹岩；9.灰白色流纹质晶屑凝灰岩；10.灰白色球粒流纹岩；11.灰白色流纹岩
Fig. 4. Geological section map of Baiyingaolao Formation (J3b) in Ta'erqi area
图 5 白音高老组岩石手标本及显微照片
a.灰白色流纹岩；b.灰色流纹质岩屑晶屑角砾凝灰岩；c.紫红色流纹质晶屑岩屑角砾凝灰熔岩；d.流纹构造；e.晶屑凝灰结构；f.流纹质岩屑；Bt.黑云母；Pl.斜长石；Q.石英；Sa.透长石
Fig. 5. Hand specimen photographs and micro photographs of Baiyingaolao Formation rock samples
图 6 满克头鄂博组流纹岩锆石阴极发光图像
Fig. 6. CL images of the zircons of rhyolite of Manketouebo Formation
图 7 满克头鄂博组流纹岩锆石U-Pb年龄
a.J3mk-1；b.J3mk-6
Fig. 7. Zircon U-Pb ages of rhyolite of Manketouebo Formation
图 8 白音高老组锆石阴极发光图像(a)及U-Pb谐和曲线图(b)
Fig. 8. CL images of the zircons (a) and zircon U-Pb ages of rhyolite of Baiyingaolao Formation (b)
图 9 样品主量元素图解
a.火山岩TAS图解(据Le Bas and LeMaitre，1986)；b.K2O-SiO2图解(据Peccerillo and Taylor, 1976)；c.Na2O-K2O图解(据Rollinson，1993)；d.A/CNK-A/NK图解(据Maniar and Piccoli, 1989)
Fig. 9. Diagrams of major elements
图 10 满克头鄂博组火山岩稀土元素球粒陨石标准化配分曲线图(a)及微量元素原始地幔标准化蛛网(b)
阴影部分数据张超(2014)
Fig. 10. Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element spider diagram (b) for the samples of Manketouebo Formation
图 16 蒙古-鄂霍茨克洋俯冲-闭合构造演化
SIB.西伯利亚板块；KAZ.哈萨克斯坦板块；Tar.塔里木板块；NCB.华北板块；XMOB.兴蒙造山带；MOS.蒙古-鄂霍茨克构造带；据Ren et al.(2018)修改
Fig. 16. Mesozoic tectonic evolution of Mongolia-Okhotsk ocean
图 17 蒙古-鄂霍茨克构造域与古太平洋构造域晚中生代演化模式(据许文良等，2019修改)
Fig. 17. Mesozoic tectonic evolution of Mongolia-Okhotsk and paleo-Pacific ocean (modified after Xu et al., 2019)
-
[1] Amelin, Y., Lee, D.C., Halliday, A.N., 2000.Early-Middle Archaean Crustal Evolution Deduced from Lu-Hf and U-Pb Isotopic Studies of Single Zircon Grains.Geochimica et Cosmochimica Acta, 64(24):4205-4225. https://doi.org/10.1016/s0016-7037(00)00493-2 [2] Ballouard, C., Poujol, M., Boulvais, P., et al., 2016.Nb-Ta Fractionation in Peraluminous Granites:A Marker of the Magmatic-Hydrothermal Transition.Geology, 44(3):231-234. https://doi.org/10.1130/g37475.1 [3] Blichert-Toft, J., Albarède, F., 1997.The Lu-Hf Isotope Geochemistry of Chondrites and the Evolution of the Mantle-Crust System.Earth and Planetary Science Letters, 148(1-2):243-258. https://doi.org/10.1016/s0012-821x(97)00040-x [4] Büchl, A., Münke, C., Mezger, K., et al., 2002.High-Precision Nb/Ta and Zr/Hf Ratios in Global MORB.Geochimica et Cosmochimica Acta, 66(15):108. http://www.researchgate.net/publication/285158476_High_precision_NbTa_and_ZrHf_ratios_in_global_MORB [5] Dostal, J., Chatterjee, A.K., 2000.Contrasting Behaviour of Nb/Ta and Zr/Hf Ratios in a Peraluminous Granitic Pluton (Nova Scotia, Canada).Chemical Geology, 163(1-4):207-218. https://doi.org/10.1016/s0009-2541(99)00113-8 [6] Frost, B.R., Barnes, C.G., Collins, W.J., et al., 2001.A Geochemical Classification for Granitic Rocks.Journal of Petrology, 42(11):2033-2048. https://doi.org/10.1093/petrology/42.11.2033 [7] Gao, L.F., He, Z.H., Sui, Z.M., et al., 2018.Chronology and Geochemistry of Volcanic Rocks from Manketouebo Formation in the Suolun Area, Central Da Hinggan Mountains and Their Tectonic Implications.Geological Bulletin of China, 37(5):881-894(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201805011.htm [8] Gao, S., Liu, X.M., Yuan, H.L., et al., 2002.Determination of Forty Two Major and Trace Elements in USGS and NIST SRM Glasses by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research, 26(2):181-196. https://doi.org/10.1111/j.1751-908x.2002.tb00886.x [9] Guo, Z.X., Yang, Y.T., Zyabrev, S., et al., 2017.Tectonostratigraphic Evolution of the Mohe-Upper Amur Basin Reflects the Final Closure of the Mongol-Okhotsk Ocean in the Latest Jurassic-Earliest Cretaceous.Journal of Asian Earth Sciences, 145:494-511. https://doi.org/10.1016/j.jseaes.2017.06.020 [10] Hu, Z.C., Liu, Y.S., Gao, S., et al., 2012.Improved In Situ Hf Isotope Ratio Analysis of Zircon Using Newly Designed X Skimmer Cone and Jet Sample Cone in Combination with the Addition of Nitrogen by Laser Ablation Multiple Collector ICP-MS.Journal of Analytical Atomic Spectrometry, 27(9):1391-1399. https://doi.org/10.1039/c2ja30078h [11] Le Bas, M.J., Le Maitre, R.W., Streckeisen, A., 1986.A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram.Journal of Petrology, 27(3):745-750. https://doi.org/10.1093/petrology/27.3.745 [12] Li, J., Lü, X.B., Chen, C., et al., 2016.Geochronological and Geochemical Characteristics of the Rhyolites in Taerqi of Middle Da Hinggan Mountains and Their Geological Significance.Geological Bulletin of China, 35(6):906-918(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201606008.htm [13] Li, S.Z., Suo, Y.H., Li, X.Y., et al., 2019.Mesozoic Tectono-Magmatic Response in the East Asian Ocean-Continent Connection Zone to Subduction of the Paleo-Pacific Plate.Earth-Science Reviews, 192:91-137. https://doi.org/10.1016/j.earscirev.2019.03.003 [14] Li, Y., Xu, W.L., Wang, F., et al., 2017.Triassic Volcanism along the Eastern Margin of the Xing'an Massif, NE China:Constraints on the Spatial-Temporal Extent of the Mongol-Okhotsk Tectonic Regime.Gondwana Research, 48:205-223. https://doi.org/10.1016/j.gr.2017.05.002 [15] Li, Y., Xu, W.L., Zhu, R.X., et al., 2020.Late Jurassic to Early Early Cretaceous Tectonic Nature on the NE Asian Continental Margin:Constraints from Mesozoic Accretionary Complexes.Earth-Science Reviews, 200:103042. https://doi.org/10.1016/j.earscirev.2019.103042 [16] Li, Z.X., Li, X.H., 2007.Formation of the 1 300 km-Wide Intracontinental Orogen and Postorogenic Magmatic Province in Mesozoic South China:A Flat-Slab Subduction Model.Geology, 35(2):179-182. https://doi.org/10.1130/g23193a.1 [17] Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS.Chinese Science Bulletin, 55(15):1535-1546. https://doi.org/10.1007/s11434-010-3052-4 [18] Maniar, P.D., Piccoli, P.M., 1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin, 101(5):635-643. doi: 10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2 [19] Mao, J.W., Wang, Z.L., 2000.A Preliminary Study on Time Limits and Geodynamic Setting of Large-Scale Metallogeny in East China.Mineral Deposits, 19(4):289-296(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ200004000.htm [20] Peccerillo, A., Taylor, S.R., 1976.Geochemistry of Eocene Calc-Akaline Volcanic Rocks from the Kastamonu Area, Northern Turkey.Contributions to Mineralogy and Petrology, 58(1):63-81. https://doi.org/10.1007/bf00384745 [21] Qin, T., Zheng, C.Q., Cui, T.R., et al., 2014.Volcanic Rocks of the Baiyingaolao Formation in the Southwest of Zhalantun, Inner Mongolia:Geochemistry, Geochronology and Tectonic Implications.Geology and Resources, 23(2):146-153(in Chinese with English abstract). http://search.cnki.net/down/default.aspx?filename=GJSD201402012&dbcode=CJFD&year=2014&dflag=pdfdown [22] Ren, Q., Zhang, S.H., Wu, Y.Q., et al., 2018.New Late Jurassic to Early Cretaceous Paleomagnetic Results from North China and Southern Mongolia and Their Implications for the Evolution of the Mongol-Okhotsk Suture.Journal of Geophysical Research:Solid Earth, 123(12):10370-10398. https://doi.org/10.1029/2018jb016703 [23] Rollinson, H.R., 1993.Using Geochemical Data.John Wiley and Sons Inc., New York. [24] Shao, J.A., Liu, F.T., Chen, H., et al., 2001.Relationship between Mesozoic Magmatism and Subduction in Da Hinggan-Yanshan Area.Acta Geologica Sinica, 75(1):56-63(in Chinese with English abstract). http://www.cqvip.com/qk/86253X/200101/1001445410.html [25] She, H.Q., Li, J.W., Xiang, A.P., et al., 2012.U-Pb Ages of the Zircons from Primary Rocks in Middle-Northern Daxinganling and Its Implications to Geotectonic Evolution.Acta Petrologica Sinica, 28(2):571-594(in Chinese with English abstract). http://www.oalib.com/paper/1475427 [26] Söderlund, U., Patchett, P.J., Vervoort, J.D., et al., 2004.The 176Lu Decay Constant Determined by Lu-Hf and U-Pb Isotope Systematics of Precambrian Mafic Intrusions.Earth and Planetary Science Letters, 219(3-4):311-324. https://doi.org/10.1016/s0012-821x(04)00012-3 [27] Sun, M.D., 2016.Cretaceous Magmatism in NE China and Adjacent Areas and Its Relationship with the Paleo-Pacific Plate Subduction.Bulletin of Mineralogy, Petrology and Geochemistry, 35(6):1090-1097, 1071(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KYDH201606005.htm [28] Suo, Y.H., Li, S.Z., Cao, X.Z., et al., 2017.Mesozoic-Cenozoic Inversion Tectonics of East China and Its Implications for the Subduction Process of the Oceanic Plate.Earth Science Frontiers, 24(4):249-267(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201704031.htm [29] Tang, J., Xu, W.L., Wang, F., et al., 2018.Subduction History of the Paleo-Pacific Slab beneath Eurasian Continent:Mesozoic-Paleogene Magmatic Records in Northeast Asia.Science China Earth Sciences, 61(5):527-559. https://doi.org/10.1007/s11430-017-9174-1 [30] Wang, F., Xu, W.L., Xing, K.C., et al., 2019.Final Closure of the Paleo-Asian Ocean and Onset of Subduction of Paleo-Pacific Ocean:Constraints from Early Mesozoic Magmatism in Central Southern Jilin Province, NE China.Journal of Geophysical Research:Solid Earth, 124(3):2601-2622. https://doi.org/10.1029/2018jb016709 [31] Wang, F., Xu, W.L., Xu, Y.G., et al., 2015.Late Triassic Bimodal Igneous Rocks in Eastern Heilongjiang Province, NE China:Implications for the Initiation of Subduction of the Paleo-Pacific Plate beneath Eurasia.Journal of Asian Earth Sciences, 97:406-423. https://doi.org/10.1016/j.jseaes.2014.05.025 [32] Wang, J.F., Li, Y.J., Li, H.Y., et al., 2019.Post-Orogeny of the Hegenshan Suture Zone:Zircon U-Pb Age and Geochemical Constraints from Volcanic Rocks of the Manketouebo Formation.Geological Bulletin of China, 38(9):1443-1454(in Chinese with English abstract). [33] Wang, X., Chen, Y.J., Li, Y., et al., 2015.Geochemical Characteristics and Geological Implication of Volcanic Rocks in Early Cretaceous Baiyingaolao Formation from Taerqi Area, Middle-North Part of Da Hinggan Mountains.Global Geology, 34(1):25-33(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SJDZ201501005.htm [34] Watson, E.B., Harrison, T.M., 1983.Zircon Saturation Revisited:Temperature and Composition Effects in a Variety of Crustal Magma Types.Earth and Planetary Science Letters, 64(2):295-304. https://doi.org/10.1016/0012-821x(83)90211-x [35] Watson, E.B., Harrison, T.M., 2005.Zircon Thermometer Reveals Minimum Melting Conditions on Earliest Earth.Science, 308(5723):841-844. https://doi.org/10.1126/science.1110873 [36] Whalen, J.B., Currie, K.L., Chappell, B.W., 1987.A-Type Granites:Geochemical Characteristics, Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology, 95(4):407-419. https://doi.org/10.1007/bf00402202 [37] Wu, F.Y., Li, X.H., Zheng, Y.F., et al., 2007a.Lu-Hf Isotopic Systematics and Their Applications in Petrology.Acta Petrologica Sinica, 23(2):185-220(in Chinese with English abstract). http://www.researchgate.net/publication/279910636_Lu-Hf_isotopic_systematics_and_thier_applications_in_petrology [38] Wu, F.Y., Li, X.H., Yang, J.H., et al., 2007b.Discussions on the Petrogenesis of Granites.Acta Petrologica Sinica, 23(6):1217-1238(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB200706000.htm [39] Wu, F.Y., Liu, X.C., Ji, W.Q., et al., 2017.Highly Fractionated Granites:Recognition and Research.Science China:Earth Sciences, 47(7):745-765 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JDXG201707001.htm [40] Xu, B., Zhao, P., Bao, Q.Z., et al., 2014.Preliminary Study on the Pre-Mesozoic Tectonic Unit Division of the Xing-Meng Orogenic Belt (XMOB).Acta Petrologica Sinica, 30(7):1841-1857(in Chinese with English abstract). http://adsabs.harvard.edu/abs/2014EGUGA..16.2314X [41] Xu, W.L., Sun, C.Y., Tang, J., et al., 2019.Basement Nature and Tectonic Evolution of the Xing'an-Mongolian Orogenic Belt.Earth Science, 44(5):1620-1646(in Chinese with English abstract). http://www.researchgate.net/publication/337905371_Basement_nature_and_tectonic_evolution_of_the_Xing'an-Mongolian_Orogenic_Belt_in_Chinese [42] Xu, W.L., Wang, F., Pei, F.P., et al., 2013.Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations.Acta Petrologica Sinica, 29(2):339-353(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical_ysxb98201302001.aspx [43] Yang, X.P., Jiang, B., Yang, Y.J., 2019.Spatial-Temporal Distribution Characteristics of Early Cretaceous Volcanic Rocks in Great Xing'an Range Area.Earth Science, 44(10):3237-3251(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201910006.htm [44] Zhang, C., 2014.Petrogenesis and Tectonic Setting of Volcanic Rocks Manketouebo Formation from Ta'erqi Area, Central Great Xing'an Range (Dissertation).Jilin University, Changchun, 55(in Chinese with English abstract). [45] Zhang, C., Li, N., Chen, Y.J., et al., 2013.Zircon U-Pb Ages and Hf Isotopic Compositions of the Intrusive Rocks in the Xing'an Mo-Cu Deposit, Inner Mongolia.Acta Petrologica Sinica, 29(1):217-230(in Chinese with English abstract). http://www.oalib.com/paper/1476795 [46] Zhang, J.H., 2009.Geochronology and Geochemistry of the Mesozoic Volcanic Rocks in the Great Xing'an Range, Northeastern China (Dissertation).China University of Geosciences, Wuhan, 76(in Chinese with English abstract). [47] Zhang, L.T., Li, S.C., Zhao, Q.Y., et al., 2015.Formation Age and Geochemical Characteristics of Volcanic Rocks from Baiyingaolao Formation of Middle Da Hinggan Mountains.World Geology, 34(1):44-54(in Chinese with English abstract). http://epub.cnki.net/grid2008/docdown/docdownload.aspx?filename=SJDZ201501007&dbcode=CJFD&year=2015&dflag=pdfdown [48] Zhang, Q., Ran, H., Li, C.D., 2012.A-Type Granite:What is the Essence? Acta Petrologica et Mineralogica, 31(4):621-626(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201204015.htm [49] Zhang, Q., Wang, Y., Li, C.D., et al., 2006.Granite Classification on the Basis of Sr and Yb Contents and Its Implications.Acta Petrologica Sinica, 22(9):2249-2269(in Chinese with English abstract). http://www.oalib.com/paper/1473353 [50] Zhou, J.B., Cao, J.L., Wilde, S.A., et al., 2014.Paleo-Pacific Subduction-Accretion:Evidence from Geochemical and U-Pb Zircon Dating of the Nadanhada Accretionary Complex, NE China.Tectonics, 33(12):2444-2466. https://doi.org/10.1002/2014tc003637 [51] 高龙飞, 和钟铧, 隋振民, 等, 2018.大兴安岭中段索伦地区满克头鄂博组火山岩年龄、地球化学特征及其构造环境.地质通报, 37(5):881-894. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201805011.htm [52] 李杰, 吕新彪, 陈超, 等, 2016.大兴安岭中段塔尔气地区流纹岩年龄、地球化学特征及其地质意义.地质通报, 35(6):906-918. doi: 10.3969/j.issn.1671-2552.2016.06.008 [53] 毛景文, 王志良, 2000.中国东部大规模成矿时限及其动力学背景的初步探讨.矿床地质, 19(4):289-296. doi: 10.3969/j.issn.0258-7106.2000.04.001 [54] 秦涛, 郑常青, 崔天日, 等, 2014.内蒙古扎兰屯地区白音高老组火山岩地球化学、年代学及其地质意义.地质与资源, 23(2):146-153. doi: 10.3969/j.issn.1671-1947.2014.02.011 [55] 邵济安, 刘福田, 陈辉, 等, 2001.大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系.地质学报, 75(1):56-63. doi: 10.3321/j.issn:0001-5717.2001.01.006 [56] 佘宏全, 李进文, 向安平, 等, 2012.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系.岩石学报, 28(2):571-594. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201202019.htm [57] 孙明道, 2016.中国东北及邻区白垩纪岩浆活动与古太平洋板块俯冲的关系.矿物岩石地球化学通报, 35(6):1090-1097, 1071. doi: 10.3969/j.issn.1007-2802.2016.06.003 [58] 索艳慧, 李三忠, 曹现志, 等, 2017.中国东部中新生代反转构造及其记录的大洋板块俯冲过程.地学前缘, 24(4):249-267. [59] 王金芳, 李英杰, 李红阳, 等, 2019.内蒙古贺根山缝合带后造山作用:满克头鄂博组火山岩锆石U-Pb年龄和地球化学制约.地质通报, 38(9):1443-1454. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201909004.htm [60] 王雄, 陈跃军, 李勇, 等, 2015.大兴安岭中北段塔尔气地区早白垩世白音高老组火山岩地球化学特征及意义.世界地质, 34(1):25-33. doi: 10.3969/j.issn.1004-5589.2015.01.004 [61] 吴福元, 李献华, 郑永飞, 等, 2007a.Lu-Hf同位素体系及其岩石学应用.岩石学报, 23(2):185-220. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200702002.htm [62] 吴福元, 李献华, 杨进辉, 等, 2007b.花岗岩成因研究的若干问题.岩石学报, 23(6):1217-1238. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200706000.htm [63] 吴福元, 刘小驰, 纪伟强, 等, 2017.高分异花岗岩的识别与研究.中国科学:地球科学, 47(7):745-765. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201707001.htm [64] 徐备, 赵盼, 鲍庆中, 等, 2014.兴蒙造山带前中生代构造单元划分初探.岩石学报, 30(7):1841-1857. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201407001.htm [65] 许文良, 孙晨阳, 唐杰, 等, 2019.兴蒙造山带的基底属性与构造演化过程.地球科学, 44(5):1620-1646. doi: 10.3799/dqkx.2019.036 [66] 许文良, 王枫, 裴福萍, 等, 2013.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约.岩石学报, 29(2):339-353. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201302002.htm [67] 杨晓平, 江斌, 杨雅军, 2019.大兴安岭早白垩世火山岩的时空分布特征.地球科学, 44(10):3237-3251. doi: 10.3799/dqkx.2019.080 [68] 张超, 2014.大兴安岭中段塔尔气地区满克头鄂博组火山岩岩石成因及构造背景(博士学位论文).长春: 吉林大学, 55. [69] 张成, 李诺, 陈衍景, 等, 2013.内蒙古兴阿钼铜矿区侵入岩锆石U-Pb年龄及Hf同位素组成.岩石学报, 29(1):217-230. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201301018.htm [70] 张吉衡, 2009.大兴安岭中生代火山岩年代学及地球化学研究(博士学位论文).武汉: 中国地质大学, 76. [71] 张乐彤, 李世超, 赵庆英, 等, 2015.大兴安岭中段白音高老组火山岩的形成时代及地球化学特征.世界地质, 34(1):44-54. doi: 10.3969/j.issn.1004-5589.2015.01.006 [72] 张旗, 冉皞, 李承东, 2012.A型花岗岩的实质是什么?岩石矿物学杂志, 31(4):621-626. doi: 10.3969/j.issn.1000-6524.2012.04.014 [73] 张旗, 王焰, 李承东, 等, 2006.花岗岩的Sr-Yb分类及其地质意义.岩石学报, 22(9):2249-2269. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200609000.htm -
下载:
点击查看大图
图(17)
计量
- 文章访问数: 702
- HTML全文浏览量: 211
- PDF下载量: 62
- 被引次数: 0
