华北克拉通北缘早二叠世堆晶岩及其构造意义

邵济安; 田伟; 张吉衡

doi:10.3799/dqkx.2015.131

Volume 40 Issue 9

Sep. 2015

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2015 > 40(9): 1441-1457

Shao Ji'an, Tian Wei, Zhang Jiheng, 2015. Early Permian Cumulates in Northern Margin of North China Craton and Their Tectonic Significances. Earth Science, 40(9): 1441-1457. doi: 10.3799/dqkx.2015.131

Citation:

Shao Ji'an, Tian Wei, Zhang Jiheng, 2015. Early Permian Cumulates in Northern Margin of North China Craton and Their Tectonic Significances. Earth Science, 40(9): 1441-1457. doi: 10.3799/dqkx.2015.131

Citation:

PDF( 4311 KB)

Early Permian Cumulates in Northern Margin of North China Craton and Their Tectonic Significances

doi: 10.3799/dqkx.2015.131

Shao Ji'an^{1, 2
,},
Tian Wei^{1, 2},
Zhang Jiheng³

1.
Key Laboratory of Orogenic Belts and Crustal Evolution of the Ministry of Education, Peking University, Beijing 100871, China
2.
School of Earth and Space Sciences, Peking University, Beijing 100871, China
3.
Key Laboratory of Computational Geodynamics of Chinese Academy of Sciences; University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2015-05-18
Publish Date: 2015-09-15

Abstract

Abstract

Understanding about genesis of the Early Permian basic-ultrabasic rocks in the northern margin of North China craton are varied, with one of the influential viewpoints suggesting that they are related with activities of "Andes-type continental margin", which is discussed in this paper based on researches of the cumulates in east Hebei Province. Early Permian basic-ultrabasic cumulates controlled by Fengning-Longhua lithospheric faults are distributed discontinuously in the northern margin of North China craton. The SHRIMP Zircon U-Pb ages from cumulates are 280-300 Ma. Petrographic studies confirm that the complexes consist of a suite of cumulates including dunite, pyroxenite, amphibolite, gabbro, diorite, anorthosite, and so on, which in turn can be further divided into layered and circular ones, both with obvious cumulate texture. Mineralogical studies show that hornblende, pyroxene, and phlogolite in cumulates all are characterized by mantle sourced components of high Mg and high Cr. Sr/Ba ratio of cumulates with different components does not change with their melting degrees, showing that cumulates possess a fractional crystallization trend. Similar REE patterns and transition group elements reveal their consanguinity. Comparison of cumulates of the Late Paleozoic with those of the Early Mesozoic from the concerned area indicates that these Early Permian cumulates have characteristics of an initial-rift magma, which offers the earliest evidence of the transformation from the stable to the active one of continental crust of North China craton. Viewed from broader regions, activities of this period in this area are driven by deeper geodynamics.
- northern margin of North China craton,
- Early Permian,
- cumulate,
- crust-mantle transition zone,
- extensional background,
- tectonics

FullText(HTML)

References(59)

References

Bai, W.J., Zhou, M.F., Hu, X.F., et al., 1993. Mafic/Ultramafic Magmatism and Tectonic Evolution of the Northern China Craton. Seismological Press, Beijing, 224-273 (in Chinese).

Bhattacharji, S., Smith, C.H., 1964. Flowage Differentiation. Science, 145(3628): 150-153. doi: 10.1126/science.145.3628.150

Bureau of Geology and Mineral Resources of Hebei Province, 1989. Regional Geology of Hebei Province, Beijing Municipality and Tianjin Municipality. Geological Publishing House, Beijing, 567-569 (in Chinese with English abstract).

Chen, B., Suzuki, K., Tian, W., et al., 2009. Geochemistry and Os-Nd-Sr Isotopes of the Gaositai Alaskan-Type Ultramafic Complex from the Northern North China Craton: Implications for Mantle-Crust Interaction. Contributions to Mineralogy and Petrology, 158(5): 683-702. doi: 10.1007/s00410-009-0404-7

Cocherie, A., 1986. Systematic Use of Trace Element Distribution Patterns in logA-logB Diagrams for Plutonic Suites. Geochim. et Cosmochim. Acta, 50(11): 2517-2522. doi: 10.1016/0016-7037(86)90034-7

Condie, K.C., 1989. Geochemical Changes in Basalts and Andesites across the Archean-Proterozoic Boundary Identification and Significance. Lithos, 23(1-2): 1-18. doi: 10.1016/0024-4937(89)90020-0

Courtillot, V., Besse, J., 1987. Magnetic Field Reversals, Polar Wander, and Core-Mantle Coupling. Science, 237(4819): 1140-1147. doi: 10.1126/science.237.4819.1140

de la Roche, H., Leterrier, J., Grandclaude, P., et al., 1980. A Classification of Volcanic and Plutonic Rocks Using R₁-R₂ Diagram and Major-Element Analyses—Its Relationships with Current Nomenclature. Chemical Geology, 29(1-4): 183-210. doi: 10.1016/0009-2541(80)90020-0

Holm, P.E., 1985. The Geochemical Fingerprints of Different Tectonomagmatic Environments Using Hygromagmatophile Element Abundances of Tholeiitic Basalts and Basaltic Andesites. Chemical Geology, 51(3-4): 303-323. doi: 10.1016/0009-2541(85)90139-1

Humphreys, M.C.S., 2009. Chemical Evolution of Intercumulus Liquid, as Recorded in Plagioclase Overgrowth Rims from the Skaergaard Intrusion. Journal of Petrology, 50(1): 127-145. doi: 10.1093/petrology/egn076

Jahn, B.M., Litvinovsky, B.A., Zanvilevich, A.N., et al., 2009. Peralkaline Granitoid Magmatism in the Mongolian-Transbaikalian Belt: Evolution, Petrogenesis and Tectonic Significance. Lithos, 113(3-4): 521-539. doi: 10.1016/j.lithos.2009.06.015

Jiang, C.Y., An, S.Y., 1984. On Chemical Characteristics of Calcic Amphiboles from Igneous Rocks and Their Petrogenesis Significance. Journal of Mineralogy and Petrology, 4(3): 1-9 (in Chinese with English abstract). http://www.researchgate.net/publication/284045336_On_chemical_characteristics_of_calcic_amphiboles_from_igneous_rocks_and_their_petrogenesis_significance

Li, C.F., Li X.H., Li Q.L., et al., 2012. Rapid and Precise Determination of Sr and Nd Isotopic Ratios in Geological Samples from the Same Flament Loading by Thermal Ionization Mass Spectrometry Employing a Single-Step Separation Scheme. Analytica Chimica Acta, 727: 54-60. doi: 10.1016/j.aca.2012.03.040

Li, W.P., Li, X.H., 2005. Geochemical Characteristics of the Late Paleozoic Diabase Dyke Swarms of Changmaohezi from Western Liaoning, Northeast China. Earth Science—Journal of China University of Geoscinces, 30(6): 761-770 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200506011.htm

Liu, Y., Zong, K., Kelemen, P.B., et al., 2008. Geochemistry and Magmatic History of Eclogites and Ultramafic Rocks from the Chinese Continental Scientific Drill Hole: Subduction and Ultrahigh-Pressure Metamorphism of Lower Crustal Cumulates. Chemical Geology, 247(1-2): 133-153. doi: 10.1016/j.chemgeo.2007.10.016

Lu, F.X., Sang, L.K., 2002. Petrology. Geological Publishing House, Beijing, 133 (in Chinese).

Ludwig, K.R., 2001. Users Manual for a Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, Special Publication, 1-59.

Ma, F., Mu, Z.G., Liu, Y.L., 2004. Geochronology and Geologic Significance of the Orbicular Dioritic Rocks in Luanping, Hebei Province. Geological Review, 50(4): 360-364 (in Chinese with English abstract). http://search.cnki.net/down/default.aspx?filename=DZLP200404003&dbcode=CJFD&year=2004&dflag=pdfdown

Ma, X., Chen, B., Chen, J.F., et al., 2012. Zircon SHRIMP U-Pb Age, Geochemical, Sr-Nd Isotopic, and In-Situ Hf Isotopic Data of the Late Carboniferous-Early Permian Plutons in the Northern Margin of the North China Craton. Science China: Earth Sciences, 42(12): 1830-1850 (in Chinese).

Mu, B.L., Yan, G.H., 1992. Geochemistry of Trissic Alkaline or Subalkaline Igneous Complexes in the Yan-Liao Area and Their Significance. Acta Geologica Sinica, 66(2): 108-121 (in Chinese with English abstract). http://www.researchgate.net/publication/284581802_Geochemistry_of_Triassic_alkaline_or_subalkaline_igneous_complexes_in_the_Yan-Liao_area_and_their_significance

Onuma, N., Ninomiya, S., Nagasawa, H., 1981. Mineral/Groundmass Partition Coefficients for Nepheline, Melilite, Clinopyroxene and Perovskite in Melilite-Nepheline Basalt, Nyiragongo, Zaire. Geochemical Journal, 15(4): 221-228. doi: 10.2343/geochemj.15.221

Peng, R.M., Zhai, Y.S., Wang, S.G., et al., 2012. Characteristics of Zircon SHRIMP Age and Its Significance to Trace-Iron of the Bearing Nichel Minerals Ultramafic Rock Body in Ebutu, Westeen Part of Northern Margin of the North China Platform. Minerral Deposits, 31(Suppl. ): 595-596 (in Chinese).

Shao, J.A., Zhang, L.Q., Mu, B.L., et al., 2007. Upwelling of Da Hinggan Mountains and Its Geodynamic Background. Geological Publishing House, Beijing, 24-29 (in Chinese).

Shao, J.A., Yang, J.H., 2011. The Geological Corridor Recording the Early Mesozoic Crust-Mantle Evolution from Chifeng to Lingyuan. Acta Petrologica Sinica, 27(12): 3525-3534 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201112003.htm

Shao, J.A., He, G.Q., Tang K.D., 2015. The Evolution of Permian Continental Crust in Northern Part of North China. Acta Petrologica Sinica, 31(1): 47-55 (in Chinese with English abstract). http://d.wanfangdata.com.cn/periodical/ysxb98201501003

Shao, J.A., Zhang, Z., She, H.Q., et al., 2012. The Discovery of Phanerozoic Granulite in Chifeng Area of North Craton and Its Implication. Earth Science Frontiers, 19(3): 188-198 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201203021.htm

Steiger, R.H., Jäger, E., 1977. Subcommission on Geochronology: Convention on the Use of Decay Constants in Geo- and Cosmochronology. Earth and Planetary Science Letters, 36(3): 359-362. doi: 10.1016/0012-821x(77)90060-7

Sun, S.H., Yu, J., 1989. Interpretation of Chemical Composition and Subdivision of Mg-Fe Micas, Part B: The Natural Subdivision of Mg-Fe Micas. Scientia Geologica Sinica, 24(2): 176-189 (in Chinese with English abstract). http://www.researchgate.net/publication/316930153_Interpretation_of_chemical_composition_and_subdivision_of_Mg-Fe_micas_Part_B_the_natural_subdivision_of_Mg-Fe_micas

Tian, W., Chen, B., Ireland, T.R., et al., 2011. Petrology and Geochemistry of Dunites, Chromitites and Mineral Inclusions from the Gaositai Alaskan-Type Complex, North China Craton: Implications for Mantle Source Characteristics. Lithos, 127(1-2): 165-175. doi: 10.1016/j.lithos.2011.08.013

Wang, H.C., Zhao, F.Q., Li, H.M., et al., 2007. Zircon SHRIMP U-Pb Age of the Dioritic Rocks from Northern Hebei: The Geological Records of Late Paleozoic Magmatic Arc. Acta Petrologica Sinica, 23(3): 587-604 (in Chinese with English abstract). http://d.wanfangdata.com.cn/periodical/ysxb98200703007

Wang, L.B., 2001. Hornblende Nomenclature. Acta Petrologica et Mineralogica, 20(1): 84-100 (in Chinese).

Wei, X., Xu, Y.G., Feng, Y.X., et al. 2014. Plume-Lithosphere Interaction in the Generation of the Tarim Large Igneous Province, NW China: Geochronological and Geochemical Constraints. American Journal of Science, 314(1): 314-356. doi: 10.2475/01.2014.09

Williams, I.S., 1998. U-Th-Pb Geochronology by Ion Microprobe. In: McKibben, M.A., Shanks, W.C., Ridley, W.I., eds., Applications of Microanalytical Techniques to Understanding Mineralizing Processes. Rev. Economic Geol., 7: 1-35.

Wood, D.A., Joron, J.L., Treuil, M., 1979. A Re-appraisal of the Use of Trace Elements to Classify and Discriminate between Magma Series Erupted in Different Tectonic Settings. Earth and Planetary Science Letters, 45(2): 326-336. doi: 10.1016/0012-821X(79)90133-X

Xia, L.Q., Li, X.M., Xia, Z.C., et al., 2006. Carboniferous-Permian Rift-Related Volcanism and Mantle Plume in the Tianshan, Northwestern China. Northwestern Geology, 39(1): 1-49 (in Chinese with English abstract). http://www.researchgate.net/publication/285794242_Carboniferous-Permian_rift-related_volcanism_and_mantle_plume_in_the_Tianshan_northwestern_China

Yan, G.H., Mu, B.L., Xu, B.L., et al., 2000. Triassic Alkaline in the Yanliao-Yinshan Area: Their Chronology, Sr, Nd and Pb Isotopic Characteristics and Their Implication. Science in China (Series D), 30(4): 383-387 (in Chinese). doi: 10.1007/BF02877785

Yang, J.H., Wu, F.Y., 2009. Triassic Magmatism and Its Relation to Decratonization in the Eastern North China Craton. Science in China (Series D), 39(7): 910-921 (in Chinese). doi: 10.1007/s11430-009-0137-5

Zhang, S.H., Zhao, Y., Kröner, A., et al., 2009. Early Permian Plutons from the Northern North China Block: Constraints on Continental Arc Evolution and Convergent Margin Magmatism Related to the Central Asian Orogenic Belt. International Journal of Earth Sciences, 98(6): 1441-1467. doi: 10.1007/s00531-008-0368-2

Zhang. X.H., Mao, Q., Zhang, H.F., et al., 2011. Mafic and Felsic Magma Interaction during the Construction of High-K Calc-Alkaline Plutons within a Metacratonic Passive Margin: The Early Permian Guyang Batholith from the Northern North China Craton. Lithos, 125(1-2): 569-591. doi: 10.1016/j.lithos.2011.03.008

Ярмолюк, B.B., Дураите, М. В., Коваленко, В. И. 1981. Возраст Комендим-Щелочно-Оранитных Ассоциации Южной Монголии, Изв. АН СССР, Сер. Теол, 9: 40-48 (in Russian). https://cpfd.cnki.com.cn/Article/CPFDTOTAL-DXES201901001011.htm

白文吉, 周美付, 胡旭峰, 等, 1993. 华北地块岩石圈构造演化与镁铁-超镁铁杂岩及矿化特征. 北京: 地震出版社, 224-273.

河北省地质矿产局, 1989. 河北省-北京市-天津市区域地质. 北京: 地质出版社, 567-569.

姜常义, 安三元, 1984. 论火成岩中钙质角闪石的化学组成特征及其岩石学意义. 矿物岩石, 4(3): 1-9. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS198403000.htm

李伍平, 李献华, 2005. 辽西晚古生代长茂河子辉绿岩墙群的地球化学特征. 地球科学——中国地质大学学报, 30(6): 761-770. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200506011.htm

路凤香, 桑隆康, 2002. 岩石学, 北京: 地质出版社, 133.

马芳, 穆治国, 刘玉琳, 2004. 河北滦平球状闪长岩年代学及其地质意义. 地质论评, 50(4): 360-364. doi: 10.3321/j.issn:0371-5736.2004.04.004

马旭, 陈斌, 陈家富, 等, 2012. 华北克拉通北缘晚古生代岩体的成因和意义: 岩石学、锆石U-Pb年龄、Nd-Sr同位素及锆石原位Hf同位素证据. 中国科学: 地球科学, 42(12): 1830-1850. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201212006.htm

牟保磊, 阎国翰, 1992. 燕辽三叠纪碱性偏碱性杂岩体地球化学特征及意义. 地质学报, 66(2): 108-121. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199202001.htm

彭润民, 翟裕生, 王守光, 等, 2012. 华北地台北缘西段额布图镍矿超镁铁质岩岩体锆石SHRIMP年龄特征及其示踪意义. 矿床地质, 31(增刊): 595-596. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ2012S1301.htm

邵济安, 张履桥, 牟保磊, 等, 2007. 大兴安岭的隆起与地球动力学背景. 北京: 地质出版社, 24-29.

邵济安, 杨进辉, 2011. 记载了早中生代壳幔演化的赤峰-凌源地质走廊. 岩石学报, 27(12): 3525-3534. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201112003.htm

邵济安, 张舟, 佘宏全, 等, 2012. 华北克拉通北缘赤峰地区显生宙麻粒岩的发现及其意义. 地学前缘, 19(3): 188-198. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201203021.htm

邵济安, 何国琦, 唐克东, 2015. 华北北部二叠纪陆壳演化. 岩石学报, 31(1): 47-55. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201501003.htm

孙世华, 于杰, 1989, Mg-Fe云母化学成分的解释和分类(Ⅱ)Mg-Fe云母的自然分类. 地质科学, 24(2): 176-189. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX198902005.htm

王惠初, 赵凤清, 李惠民, 等, 2007. 冀北闪长质岩石锆石SHRIMP U-Pb年龄: 晚古生代岩浆弧的地质记录. 岩石学报, 23(3): 597-604. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200703009.htm

王立本, 2001. 角闪石命名法——国际矿物学协会新矿物及矿物命名委员会角闪石专业委员会的报告. 岩石矿物学杂志, 20(1): 84-100. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200101011.htm

夏林圻, 李向民, 夏祖春, 等, 2006. 天山石炭-二叠纪大火成岩省裂谷火山作用与地幔柱. 西北地质, 39(1): 1-49. doi: 10.3969/j.issn.1009-6248.2006.01.001

阎国翰, 牟保磊, 许保良, 等, 2000. 燕辽-阴山三叠纪碱性侵入岩年代学和Sr, Nd, Pb同位素特征及意义. 中国科学(D辑), 30(4): 383-387. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200004005.htm

杨进辉, 吴福元, 2009. 华北东部三叠纪岩浆作用与克拉通破坏. 中国科学(D辑), 39(7): 910-921. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200907005.htm

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(10) / Tables(8)

Get Citation

PDF

XML

Article views (3902) PDF downloads(530)

Early Permian Cumulates in Northern Margin of North China Craton and Their Tectonic Significances

doi: 10.3799/dqkx.2015.131

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content