Mesozoic-Cenozoic Mafic Magmatism in Western Shandong Province and Its Implication for the Chemical Evolution of the Mantle
-
摘要: 镁铁质火成岩作为分布最为广泛的典型幔源岩石, 已成为探索地幔化学性状及示踪岩石圈深部过程的主要研究对象.通过对典型样品元素-同位素组成的系统测定, 并结合前人已有资料, 综合研究了鲁西中生代和新生代镁铁质岩石的地质与地球化学特征.研究结果表明, 中生代镁铁质火成岩总体具有富轻稀土和大离子亲石元素、贫高场强元素、ISr值变化范围大(0.70396~0.71247)、εNd (t) 值显著偏低(-9.20~-21.21) 的地球化学特征, 但该区南部和北部的中生代镁铁质岩石在元素-同位素组成上仍存在一定差别, 主要表现在南部较之北部镁铁质岩石具有更高的稀土总量(ΣREE为325.52×10-6~555.75×10-6)和轻、重稀土比值(LREE/HREE=17.75~25.97), 以及更高的LILE/HFSE比值(如La/Nb=6.37~13.85, Th/Nb=0.52~1.53).南部镁铁质岩石较之北部镁铁质岩石也更富放射成因锶, ISr值分别为0.70844~0.71247和0.70396~0.70598.元素-同位素综合示踪指示鲁西中生代地幔总体具有因岩石圈大规模拆沉作用形成的EMⅠ型富集地幔特征, 但其南部叠加了因深俯冲而进入地幔的扬子陆壳的影响, 因而表现出EMⅠ和EMⅡ组分混合的富集地幔特征.新生代玄武岩具有类似于大洋玄武岩的地球化学特征, 其源区应为亏损的软流圈地幔, 但在部分熔融形成岩浆之前遭受了近期的交代作用.自中生代至新生代, 华北克拉通地幔具有由富集向亏损演变的趋势, 这一化学性状的演变最可能是中生代以来岩石圈大规模拆沉作用, 导致软流圈地幔上涌并对原有岩石圈地幔再改造所致.Abstract: Mafic igneous rock, a widely distributed and typical mantle-derived rock, has become a major research source for revealing possible mechanisms for the chemical evolution of the mantle. Combined geological and geochemical studies have been carried out on the Mesozoic and Cenozoic mafic igneous rocks in western Shandong Province, determining the elemental and isotopic compositions of typical samples. Generally, the Mesozoic mafic igneous rocks have enriched LREE and LILE concentrations, low HFSE abundance, and display highly variable ISr ratios (0.703 96-0.712 47) and distinctly negative εNd (t) values (-9.20 to -21.21). Compared to the north of western Shandong Province, the Mesozoic mafic rocks in the south have higher total REE contents (ΣREE=325.52×10-6-555.75×10-6), higher LREE/HREE ratios (17.75-25.97), and higher LILE/HFSE ratios (e. g., La/Nb=6.37-13.85, Th/Nb=0.52-1.53). They also have more radiogenic Sr isotopic compositions, with ISr values of 0.708 44-0.712 47 and 0.703 96-0.705 98, respectively. Integrated elemental and isotopic tracing suggest that the Mesozoic mantle of western Shandong Province is generally characterized by the EMⅠ component, which was probably formed by large-scale lithospheric delamination, whereas the mantle source in the south part has been superimposed by the influence of the deep subducted Yangtze continental materials, and thus displays the mixed features of EMⅠ and EMⅡ components. The geochemical characteristics of the Cenozoic basalts are similar to those of the oceanic basalts. It is likely that the rocks were derived from a depleted asthenosphere source but underwent metasomatism shortly before partial melting. From the Mesozoic to the Cenozoic, the nature of the mantle beneath the North China craton evolved from an enriched one to a depleted one. This chemical evolution most likely resulted from an asthenosphere upwelling, which was induced by large-scale lithospheric delamination and thus replaced the original lithospheric mantle with a newly created one.
-
图 1 鲁西中、新生代镁铁质岩石分布
1.新生代碱性玄武岩; 2.中生代火山岩; 3.辉长质杂岩体; 4.金伯利岩; 5.碳酸岩; 6.镁铁-超镁铁质煌斑岩; 7.断裂; Ⅰ.华北板块; Ⅱ.扬子板块
Fig. 1. Sketch map showing the distribution of the Mesozoic and Cenozoic mafic igneous rocks in western Shandong Province
图 2 鲁西中、新生代镁铁质岩石地球化学对比
1.新生代玄武岩; 2.方城中生代玄武岩; 3.蒙阴中生代钾玄质火山岩; 4.济南辉长岩; 5.邹平辉长岩; 6.邹平中生代玄武质火山岩.C.新生代玄武岩; MS.鲁西地块南部中生代镁铁质火成岩; MN.鲁西地块北部中生代镁铁质火成岩.图中除本文资料外, 其余资料引自: 新生代玄武岩据金隆裕(1989)、支霞臣(1990)、陈道公(1992)和牛漫兰等(2001); 中生代镁铁质岩石据邱检生等(1997)、Guo et al. (2001)、Zhang et al. (2002)、Guo et al. (2003)和裴福萍等(2004)
Fig. 2. Geochemical comparison diagrams of the Mesozoic and Cenozoic mafic igneous rocks in western Shandong Province
图 3 鲁西中、新生代镁铁质岩石稀土元素球粒陨石标准化配分型式(球粒陨石值据Boynton, 1984)
Fig. 3. Chondrite-normalized REE distribution patterns of the Mesozoic and Cenozoic mafic igneous rocks in western Shandong Province
图 4 鲁西中、新生代镁铁质岩石微量元素相对于原始地幔标准化蛛网图(原始地幔值据Sun and McDonough, 1989)
Fig. 4. Primitive mantle-normalized spidergrams of trace elements for the Mesozoic and Cenozoic mafic igneous rocks in western Shandong Province
图 5 鲁西中、新生代镁铁质岩石La/Nb-Ba/Nb关系(图例及资料来源同图 2)
Fig. 5. La/Nb versus Ba/Nb diagram of the Mesozoic and Cenozoic mafic igneous rocks in western Shandong Province
图 6 鲁西中、新生代镁铁质岩石(87Sr/86Sr) i-εNd (t) 关系
1.新生代玄武岩; 2.邹平玄武质火山岩; 3.邹平辉长岩; 4.济南辉长岩; 5.方城玄武岩; 6.蒙阴钾玄质火山岩; 7.鲁西地块南缘中生代镁铁-超镁铁质煌斑岩; 8.北淮阳富钾火山岩; 9.北大别镁铁-超镁铁岩; 10.胶莱盆地钾玄质火山-侵入岩; DM.亏损地幔; MORB.洋脊玄武岩; OIB.洋岛玄武岩; PM.原始地幔; EMⅠOIB.具EMⅠ型富集地幔特征的洋岛玄武岩; EMⅠ.Ⅰ型富集地幔; EMⅡ.Ⅱ型富集地幔; 其余代号同图 2.除本文资料外, 新生代玄武岩据陈道公(1992)和支霞臣等(1994); 中生代镁铁质岩石据Guo et al. (2001)、Qiu et al. (2002); Zhang et al. (2002)和Guo et al. (2003); 北大别镁铁-超镁铁岩据Jahn et al. (1999); 北淮阳富钾火山岩据邱检生等(2002); 胶莱盆地钾玄质火山-侵入岩据邱检生和王德滋(1999)、Fan et al. (2001)
Fig. 6. (87Sr/86Sr) i versus εNd (t) diagram for the Mesozoic and Cenozoic mafic igneous rocks in western Shandong Province
图 7 鲁西中、新生代镁铁质岩石ISr-Mg#、SiO2关系(a)和La/Nb-Ba/La关系(b)
图 7a除本文资料外, 其余资料引自Guo et al. (2001)、Zhang et al. (2002)和Guo et al. (2003); 图 7b资料来源同图 2
Fig. 7. ISr versus Mg# and SiO2 diagrams (a) and La/Nb versus Ba/La diagram (b) for the Mesozoic and Cenozoic mafic igneous rocks in western Shandong Province
图 8 鲁西不同时代幔源岩石εNd (t) 值频率分布
古生代金伯利岩据路凤香和郑建平(1996);中、新生代岩石同图 6
Fig. 8. Histogram of εNd (t) values for mantle-derived rocks of different ages in western Shandong Province
图 9 鲁西中生代镁铁质火成岩ISr频率分布(资料来源同图 7a)
Fig. 9. Histogram of ISr values for the Mesozoic mafic igneous rocks in the north and south parts of western Shandong Province
表 1 鲁西中、新生代镁铁质火成岩代表性样品主量和微量元素含量及Sr-Nd同位素组成
Table 1. Major, trace element contents and Sr-Nd isotopic compositions of the typical mafic igneous rocks in western Shandong Province
表 2 鲁西中、新生代镁铁质火成岩不相容元素比值及与各主要地球化学储库的对比
Table 2. Incompatible element ratios of the Mesozoic and Cenozoic mafic igneous rocks in western Shandong Province and comparison with those of the other geochemical reservoirs
表 3 华北地块东部中生代镁铁质岩石εNd (t) 值
Table 3. εNd (t) values of the Mesozoic mafic igneous rocks in east part of the North China block
-
[1] Boynton, W.V., 1984. Geochemistry of the rare earth elements: Meteorite studies. In: Henderson, P., ed., Rare earth elements geochemistry. Elservier, Amsterdam, 63-144. [2] Bureau of Geology and Mineral Resources of Shandong Province, 1991. Regional geology of Shandong Province. Geological Publishing House, Beijing, 1-572(in Chinese with English abstract). [3] Chen, B., Zhai, M., 2003. Geochemistry of Late Mesozoic lamprophyre dykes from the Taihang mountains, north China, and implications for the sub-continental lithospheric mantle. Geol. Mag. , 140(1): 87-93. doi: 10.1017/S0016756802007124 [4] Chen, B., Jahn, B., Zhai, M.G., 2003. Sr-Nd isotopic character of Mesozoic magmatism in the Taihang-Yanshan orogen, North China craton, and implications for Archean lithospheric thinning. Journal of the Geological Society, 160: 963-970. doi: 10.1144/0016-764902-129 [5] Chen, D.G., 1992. The geochemistry of Cenozoic basalt at the middle-south segment of Tanlu fault zone. In: Liu, R.X., ed., The age and geochemistry of Cenozoic volcanic rock in China. Seismological Press, Beijing, 1-43 (in Chinese). [6] Deng, J.F., Zhao, H.L., Mo, X.X., et al., 1996. Continental roots-plume tectonics of China—Key to the continental dynamics. Geological Publishing House, Beijing, 1-110 (in Chinese with English abstract). [7] Fan, W.M., Zhang, H.F., Baker, J., et al., 2000. On-craton and off-craton Cenozoic spinel peridotites in eastern China: Similarity and difference. J. Petrology, 41: 933-950. doi: 10.1093/petrology/41.7.933 [8] Fan, W.M., Guo, F., Wang, Y.J., et al., 2001. Post-orogenic bimodal volcanism along the Sulu orogenic belt in eastern China. Phys. Chem. Earth(A), 26: 733-746. doi: 10.1016/S1464-1895(01)00123-5 [9] Fan, W.M., Guo, F., 2005. Late Mesozoic mafic magmatism from the eastern part of North China block and its adjacent regions: Magma genesis and geodynamic implications for lithospheric thinning. Geotectonic et Metallogenia, 29(1): 44-55(in Chinese with English abstract). [10] Gao, S., Zhang, B.R., Jin, Z.M., et al., 1998. How mafic is the lower continental crust? Earth Planet. Sci. Lett. , 106: 101-117. [11] Gao, S., Kern, H., Jin, Z.M., et al., 2003. Poisson's ratio of eclogite: Implications for lower crustal delamination of orogens. Science in China(Series D), 46(9): 909-918. doi: 10.1360/02yd0417 [12] Gao, S., Rudnick, R.L., Carlson, R.W., et al., 2004. Recycling lower continental crust in the North China craton. Nature, 432: 892-897. doi: 10.1038/nature03162 [13] Glazaer, A.F., Farmer, G. L., 1992. Production of isotopic variability in continental basalt by cryptic crustal contamination. Science, 255: 72-74. doi: 10.1126/science.255.5040.72 [14] Guo, F., Fan, W.M., Wang, Y.J., et al., 2001. Late Mesozoic mafic intrusive complexes in North China block: Constraints on the nature of subcontinental lithospheric mantle. Phys. Chem. Earth(A), 26: 759-771. doi: 10.1016/S1464-1895(01)00125-9 [15] Guo, F., Fan, W.M., Wang, Y.J., et al., 2003. Geochemistry of Late Mesozoic mafic magmatism in west Shandong Province, eastern China: Characterizing the lost lithospheric mantle beneath the North China block. Geochem. J. , 37: 63-77. doi: 10.2343/geochemj.37.63 [16] Henderson, P., 1982. Inorganic geochemistry. Pergamon, Oxford, 1-353. [17] Hong, D.W., Wang, T., Tong, Y., et al., 2003. Mesozoic granitoids from North China block and Qinling-DabieSulu orogenic belt and their deep dynamic process. Earth Science Frontiers, 10(3): 231-256(in Chinese with English abstract). [18] Jahn, B.M., Wu, F.Y., Lo, C.H., et al., 1999. Crust-mantle interaction induced by deep subduction of the continental crust: Geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie complex, central China. Chem. Geol. , 157(1-2): 119-146. doi: 10.1016/S0009-2541(98)00197-1 [19] Jin, L.Y., 1985. K-Ar ages of Cenozoic volcanic rocks in the middle segment of the Tancheng-Lujiang fault zone and stages of related volcanic activity. Geological Review, 31(4): 309-315(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP198504003.htm [20] Jin, L.Y., 1989. Petrologic and geochemical characteristics of Cenozoic volcanic rocks in the middle segment of the Tancheng-Lujiang fault zone. Acta Petrologica Sinica, 5(4): 45-57(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB198904004.htm [21] Kelemen, P. B., Kingler, R. J., Johnson, K. T. M., 1990. High field strength element depletions in arc basalt due to mantle-magma interaction. Nature, 345: 521-524. doi: 10.1038/345521a0 [22] Lassiter, J.C., Depaolo, D.J., 2000. Plume/lithosphere interaction in the generation of continental and oceanic flood basalts: Chemical and isotopic constraints. In: Mahoney, J., Coffin, M.F., eds., Large igneous provinces: Continental, oceanic, and planetary flood volcanism. American Geophysical Union Monograph, Washington, D. C., 100: 335-355. [23] Li, C.J., 1992. Opinions on stage division of the intrusive rocks in Jinan-Zouping area. Geology of Shandong, 8 (1): 68-79(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SDDI199201006.htm [24] Li, S.G., Zhang, Z.Q., 1990. Nd isotopic compositions and evolution of the upper mantle in the Archean of North China: Constraints on the mantle heterogeneity of the unmetasomatic continental lithosphere. Geochimica, 4: 277-285(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX199004000.htm [25] Livaceari, R. F., Perry, F. V., 1993. Isotopic evidence for preservation of Cordilleran lithospheric mantle during the Sevier Laramide orogeny, west United States. Geology, 21: 719-722. [26] Lu, F. X., Zheng, J. P., 1996. Palaeozoic nature and deep processes of lithospheric mantle beneath North China. In: Chi, J.S., Lu, F.X., eds., Kimberlites and Paleozoic mantle beneath North China platform. Science Press, Beijing, 215-274(in Chinese). [27] McKenzie, D., Bickle, M.J., 1988. The volume and composition of melt generated by extension of the lithosphere. J. Petrol. , 29: 625-679. doi: 10.1093/petrology/29.3.625 [28] Niu, M.L., Zhu, G., Song, C.Z., et al., 2001. Features and evolution of the mantle source area of Cenozoic basalts in the middle-south segment of the Tanlu fault zone. Geoscience, 15(4): 383-390(in Chinese with English abstract). [29] Pei, F.P., Xu, W.L., Wang, Q.H., et al., 2004. Mesozoic basalt and mineral chemistry of the mantle-derived xenocrysts in Feixian, western Shandong, China: Constraints on nature of Mesozoic lithospheric mantle. Geological Journal of China Universities, 10(1): 88-97 (in Chinese with English abstract). doi: 10.1007/BF02873097 [30] Qiu, J. S., Wang, D. Z., 1999. Geochemistry of pyroxenemonzonite at Qibaoshan caldera in Wulian County, Shandong Province and the nature of the magma source. Geological Review, 45(Suppl. ): 612-617(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZLP1999S1087.htm [31] Qiu, J.S., Wang, D.Z., Liu, H., et al., 2002. Post-collisional potash-rich volcanic rocks in the north margin of Dabie orogenic belt: Geochemistry and petrogenesis. Acta Petrologica Sinica, 18(3): 319-330(in Chinese with English abstract). doi: 10.1016/S0037-0738(01)00236-6 [32] Qiu, J.S., Wang, D.Z., Zeng, J.H., et al., 1997. Study on trace element and Nd-Sr isotopic geochemistry of the Mesozoic potash-rich volcanic rocks and lamprophyres in western Shandong Province. Geological Journal of China Universities, 3(4): 384-395(in Chinese with English abstract). [33] Qiu, J.S., Xu, X.S., Lo, Q.H., 2002. Potash-rich volcanic rocks and lamprophyres in western Shandong Province: 40Ar-39Ar dating and source tracing. Chinese Science Bulletin, 47(2): 91-99. doi: 10.1360/02tb9019 [34] Shao, J.A., Li, X.H., Zhang, L.Q., et al., 2001. Geochemical condition for genetic mechanism of the Mesozoic bimodal dike swarms in Nankou-Guyaju. Geochimica, 30 (6): 517-524(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX200106002.htm [35] Stolz, A.J., Jochum, K.P., Spette, L.B., et al., 1996. Fluid and melt-related enrichment in the sub-arc mantle: Evidence from Nb/Ta variations in island-arc basalts. Geology, 24: 587-590. [36] Sun, S.S., McDonough, W.F., 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. In: Saunder, A.D., Norry, M.J., eds., Magmatism in the ocean basins. Geol. Soc. Spe. Publ., 42: 313-345. [37] Tan, D.J., Lin, J.Q., 1994. The Mesozoic potassic igneous rock zones in North China platform. Seismological Press, Beijing, 1-184(in Chinese). [38] Tatsumoto, M., Basu, A.R., Huang, J.W., et al., 1992. Sr, Nd, and Pb isotopes of ultramafic xenoliths in volcanic rocks of eastern China: Enriched components EMⅠ and EMⅡ in subcontinental lithosphere. Earth and Plane- tary Science Letters, 113: 107-128. doi: 10.1016/0012-821X(92)90214-G [39] Wang, Y.X., Yang, J.D., Tao, X.C., et al., 1988. A study of the Sm-Nd method for fossil, mineral and rock samples, and its application. J. Nanjing Uni. (Natural Sciences Edition), 24(2): 297-308(in Chinese with English abstract). [40] Weaver, B.L., 1991. The origin of ocean island basalt endmember compositions: Trace element and isotopic constraints. Earth and Planetary Science Letters, 104: 381-397. doi: 10.1016/0012-821X(91)90217-6 [41] Zhang, H.F., Sun, M., Zhou, X.H., et al., 2002. Mesozoic lithosphere destruction beneath the North China craton: Evidence from major-, trace-element and Sr-Nd-Pb isotope studies of Fangcheng basalts. Contrib. Min. Petrol. , 144: 241-253. doi: 10.1007/s00410-002-0395-0 [42] Zhang, H.F., Ying, J.F., Xu, P., et al., 2004. Mantle olivine xenocrysts entrained in Mesozoic basalts from the North China craton: Implication for replacement process of lithospheric mantle. Chinese Science Bulletin, 49(9): 961-966. doi: 10.1007/BF03184019 [43] Zhang, Q., Qian, Q., Wang, E.Q., et al., 2001. An east China plateau in Mid-Late Yanshanian period: Implication from adakites. Chinese Journal of Geology, 36(2): 248 -255(in Chinese with English abstract). [44] Zhang, Z. Q., 1998. On the continental growth periods of North China craton based on Sm-Nd isotopic characteristics of the Early Precambrian metamorphic rocks. In: Chen, Y.Q., ed., Contributions on the Early Precambrian geology in North China craton. Geological Publishing House, Beijing, 133-136(in Chinese). [45] Zheng, J.P., Lu, F.X., O'Reilly, S.Y., et al., 2000. Mantle modification and replacement beneath east China: A study on clinopyroxenes of Laser ICPMS. Sciences in China(Series D), 30(4): 373-382(in Chinese). [46] Zheng, J.P., Lu, F.X., Yu, C.M., et al., 2003. Mantle replacement: Evidence from comparison in trace elements between peridotite and diopside from refractory and fertile mantle, North China. Earth Science—Journal of China University of Geosciences, 28(3): 235-240(in Chinese with English abstract). [47] Zheng, J. P., Griffin, W. L., O'Reilly, S. Y., et al., 2005. Late Mesozoic-Cenozoic mantle replacement beneath the eastern North China craton: Evidence from the Paleozoic and Cenozoic peridotite xenoliths. International Geology Review, 47: 457-472. doi: 10.2747/0020-6814.47.5.457 [48] Zhi, X.C., 1990. Trace element geochemistry and petrogenesis of Cenozoic alkalic basalts from the Penglai and Linqu areas, Shandong Province. Geological Review, 36(5): 385-393(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP199005000.htm [49] Zhi, X.C., Chen, D.G., Zhang, Z.Q., et al., 1994. The neodymium and strontium isotopic compositions of Cenozoic alkalic basalts from Penglai and Linqu, Shandong Province. Geological Review, 40(6): 526-533(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP199406007.htm [50] Zhou, X.H., Yang, J.H., Zhang, L.C., 2002. Metallogenesis of superlarge gold deposits in Jiaodong region and deep processes of subcontinental lithosphere beneath North China craton in Mesozoic. Science in China(Series D), 32(Suppl. ), 46: 14-25. [51] Zhou, X.H., Zhang, G.H., Yang, J.H., et al., 2001. Sr-Nd-Pb isotope mapping of Late Mesozoic volcanic rocks across northern margin of North China craton and implications to geodynamic processes. Geochimica, 30(1): 10-23(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX200101002.htm [52] 陈道公, 1992. 郯庐断裂带中南段新生代玄武岩地球化学. 见: 刘若新, 中国新生代火山岩年代学与地球化学. 北京: 地震出版社, 1-43. [53] 邓晋福, 赵海玲, 莫宣学, 等, 1996. 中国大陆根-柱构造—大陆动力学的钥匙. 北京: 地质出版社, 1-110. [54] 范蔚茗, 郭锋, 2005. 华北地区晚中生代镁铁质岩浆作用及其地球动力学背景. 大地构造与成矿学, 29(1): 44-55. doi: 10.3969/j.issn.1001-1552.2005.01.008 [55] 洪大卫, 王涛, 童英, 等, 2003. 华北地台和秦岭-大别-苏鲁造山带的中生代花岗岩与深部地球动力学过程. 地学前缘, 10(3): 231-256. doi: 10.3321/j.issn:1005-2321.2003.03.022 [56] 金隆裕, 1985. 郯庐断裂带中段新生代火山岩的K-Ar年龄值和分期. 地质论评, 31(4): 309-315. doi: 10.3321/j.issn:0371-5736.1985.04.004 [57] 金隆裕, 1989. 郯庐断裂带中段新生代火山岩的岩石学和地球化学特征. 岩石学报, 5(4): 45-57. doi: 10.3321/j.issn:1000-0569.1989.04.005 [58] 李昶绩, 1992. 济南—邹平地区侵入岩期次划分之我见. 山东地质, 8(1): 68-79. https://www.cnki.com.cn/Article/CJFDTOTAL-SDDI199201006.htm [59] 李曙光, 张宗清, 1990. 华北太古代上地幔钕同位素组成、演化及对该区岩石圈地幔不均一性的制约. 地球化学, 4: 277-285. doi: 10.3321/j.issn:0379-1726.1990.04.001 [60] 路凤香, 郑建平, 1996. 华北地台古生代岩石圈地幔特征及深部过程. 见: 池际尚, 路凤香. 华北地台金伯利岩及古生代岩石圈地幔特征. 北京: 科学出版社, 215-274. [61] 牛漫兰, 朱光, 宋传中, 等, 2001. 郯庐断裂带中南段新生代玄武岩源区地幔特征及其演化. 现代地质, 15(4): 383-390. doi: 10.3969/j.issn.1000-8527.2001.04.005 [62] 裴福萍, 许文良, 王清海, 等, 2004. 鲁西费县中生代玄武岩及幔源捕虏晶的矿物化学: 对岩石圈地幔性质的制约. 高校地质学报, 10(1): 88-97. doi: 10.3969/j.issn.1006-7493.2004.01.008 [63] 邱检生, 王德滋, 1999. 山东五莲七宝山辉石二长岩的地球化学及岩浆源区性质. 地质论评, 45(增刊): 612-617. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP1999S1087.htm [64] 邱检生, 王德滋, 刘洪, 等, 2002. 大别造山带北缘后碰撞富钾火山岩: 地球化学与岩石成因. 岩石学报, 18(3): 319-330. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200203005.htm [65] 邱检生, 王德滋, 曾家湖, 等, 1997. 鲁西中生代富钾火山岩及煌斑岩微量元素和Nd-Sr同位素地球化学. 高校地质学报, 3(4): 384-395. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX199704003.htm [66] 山东省地质矿产局, 1991. 山东省区域地质志. 北京: 地质出版社, 1-572. [67] 邵济安, 李献华, 张履桥, 等, 2001. 南口-古崖居中生代双峰式岩墙群形成机制的地球化学制约. 地球化学, 30(6): 517-524. doi: 10.3321/j.issn:0379-1726.2001.06.003 [68] 谭东娟, 林景仟, 1994. 华北地台中生代钾质岩浆岩区. 北京: 地震出版社, 1-184. [69] 王银喜, 杨杰东, 陶仙聪, 等, 1988. 化石、矿物和岩石样品的Sm-Nd同位素实验方法及其应用. 南京大学学报(自然科学版), 24(2): 297-308. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ198802017.htm [70] 张旗, 钱青, 王二七, 等, 2001. 燕山中晚期的中国东部高原: 埃达克岩的启示. 地质科学, 36(2): 248-255. doi: 10.3321/j.issn:0563-5020.2001.02.014 [71] 张宗清, 1998. 从华北古陆早前寒武纪变质岩的Sm-Nd同位素特征论其地壳的主要生长时期. 见: 程裕淇. 华北地台早前寒武纪地质研究论文集. 北京: 地质出版社, 133-136. [72] 郑建平, 路凤香, O'Reilly, S.Y., 等, 2000. 华北东部地幔改造作用和置换作用: 单斜辉石激光探针研究. 中国科学, 30(4): 373-382. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200004004.htm [73] 郑建平, 路凤香, 余淳梅, 等, 2003. 地幔置换作用: 华北两类橄榄岩及其透辉石微量元素对比证据. 地球科学—中国地质大学学报, 28(3): 235-240. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200303000.htm [74] 支霞臣, 1990. 山东蓬莱、临朐新生代碱性玄武岩的痕量元素和岩石成因. 地质论评, 36(5): 385-393. doi: 10.3321/j.issn:0371-5736.1990.05.001 [75] 支霞臣, 陈道公, 张宗清, 等, 1994. 山东蓬莱、临朐新生代碱性玄武岩的钕、锶同位素组成. 地质论评, 40(6): 526-533. doi: 10.3321/j.issn:0371-5736.1994.06.008 [76] 周新华, 张国辉, 杨进辉, 等, 2001. 华北克拉通北缘晚中生代火山岩Sr-Nd-Pb同位素填图及其意义. 地球化学, 30(1): 10-23. doi: 10.3321/j.issn:0379-1726.2001.01.003 -
下载:
点击查看大图
计量
- 文章访问数: 3559
- HTML全文浏览量: 84
- PDF下载量: 6
- 被引次数: 0
