Chinese Journal of Geochemistry

, Volume 8, Issue 2, pp 97–111 | Cite as

Petrochemical comparison of 3.5 Ga old mafic amphibolite inclusions from eastern Hebei province with Archean mafic — ultramafic supracrustals of uncertain antiquity, southern Jilin eastern Liaoning provinces, China

  • W. G. Ernst
Article

Abstract

New major element data for coexisting minerals and bulk-rock REE analyses, combined with previously obtained petrologic/geologic information, allow comparison of Archean mafic-ultramafic meta-igneous rocks from adjacent portions of northeastern Sino-Korean shield. Isotope data published by previous workers document an Early Archean age of formation for metabasaltic rocks now occurring as mafic amphibolite inclusions in tonalitic gneisses west of Bohai Bay (area A). Mafic-ultramafic mineral assemblages developed in amphibolite fades Archean supracrustals east of Bohai Bay (area B) are chemically similar, but pre-existing phase associations have been overprinted by the effects of several later metamorphic events. Non-peridotitic area B protoliths appear to be more magnesian, averaging ∼ 12 wt. % MgO (versus ∼ 7 wt. % for area A), and are slightly less fractionated in REE concentrations relative to chondrites (La-Lu=30-8X versus 37-14X for area A), thus perhaps being more mantle-like than area A metabasaltic analogues. The basaltic-komatiitic series east of Bohai Bay probably represents the most ancient crust of that region, being invaded by Archean tonalites, which were subsequently converted to orthogneisses. These observations are compatible with the hypothesis that, similar to area A metabasaltic rocks now found as amphibolitic inclusions in orthogneisses, area B mafic supracrustals were formed during Early or Middle Archean time, prior to widespread isofacial amphibolite facies metamorphism (600–700°C, 5–7 kb, low αH2O).

Keywords

Liaoning Province Isochron Tonalitic Gneiss Mafic Inclusion Komatiitic Basalt 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. [1]
    Huang, T. K., 1978: An outline of the tectonic characteristics of China:Eclogae Geol. Helv., v. 71, p. 611–635.Google Scholar
  2. [2]
    Huang, T. K., 1980: An outline of the tectonic characteristics of China: in p. 184–197, Continental Tectonics, Acad. Sci., Washington, D.C.Google Scholar
  3. [3]
    Miyashiro, A., 1981: Tectonic and Petrologic Aspects of Asia: Mem. 4, Geol. Soc. China, p. 1–31.Google Scholar
  4. [4]
    Ma, X. Y., and Wu, Z. W., 1981: Early tectonic evolution of China:Precambrian Res., v. 14, p. 185–202.CrossRefGoogle Scholar
  5. [5]
    Zhong, F. D., Chen, Y. W., Liu, J. Y., Mao, C. X., and Hong, W. X., 1984: Pb isotopic dating of some Precambrian rocks from north China—an ensuing discussion on Precambrian geochronological scale of China:Geochemistry, v. 3, p. 24–36.Google Scholar
  6. [6]
    Jahn, B. M., and Zhang, Z. Q., 1984: Archean granulite gneisses from eastern Hebei Province, China: rare earth geochemistry and tectonic implications:Contrib. Mineral. Petrology, v. 85, p. 224–243.CrossRefGoogle Scholar
  7. [7]
    Zhu, B. Q., and Chen, Y. W., 1984: Features of Pb isotopic composition of ores and evolution of continental crust of China:Scientia Sinica, Ser. B., v. 27, p. 635–646.Google Scholar
  8. [8]
    Huang, X., Bi, Z., and DePaolo, D. J., 1986: Sm-Nd isotope study of early Archean rocks, Qianan, Hebei Province, China:Geochim. Cosmochim. Acta, v. 50, p. 625–635.CrossRefGoogle Scholar
  9. [9]
    Jahn, B. M., Auvray, B., Cornichet, J., Bai, Y. L., Shen, Q.H., and Liu, D.Y., 1987: 3.5 Ga old amphibolites from eastern Hebei Province, China: field occurrence, petrography, Sm-Nd isochron age and REE geochemistry:Precambrian Res., v. 34, p. 311–346.CrossRefGoogle Scholar
  10. [10]
    Xu, G. R., and Chen, H. J., 1984: A preliminary study of komatiites in Anshan-Benxi-Fushun region, northeast China:Geochemistry, v. 3, p. 128–141.Google Scholar
  11. [11]
    Zhai, M. G., Yang, R. Y., Lu, W. J., and Zhou, J., 1985: Geochemistry and evaluation of the Qingyuan Archean granite-greenstone terrain, NE China:Precambrian Res., v. 27, p. 37–62.CrossRefGoogle Scholar
  12. [12]
    Wang, R. S. S., Zai, M. G., Hu, S. L., Sang, H. Q., and Qiu, J., 1986:40Ar/39Ar age spectrum for biotite separated from Qingyuan tonalite, NE China:Sci. Geol. Sinica, no.1, p. 97–100.Google Scholar
  13. [13]
    Ernst, W. G., 1988: Element partitioning and thermobarometry in polymetamorphic Late Archean and Early — Mid Proterozoic rocks from eastern Liaoning and southern Jilin provinces, P. R. C.:Amer. Jour. Sci., Wones Vol.Google Scholar
  14. [14]
    Ernst, W. G., Cao, R., and Jiang, J., 1988: Reconnaissance study of Precambrian rocks, northeastern Sino — Korean shield, People’s Republic of China:Geol. Soc. America Bull., v. 100.Google Scholar
  15. [15]
    Zhu, B. Q., Zhai, M., Stacey, J. S., and Lanphere, M. A., 1986: Ages of petrogenesis and metamorphism in Archean rocks, Huadian region, NE China:Terra Cognita, v. 6, p. 145.Google Scholar
  16. [16]
    Pidgeon, R. T., 1980: 2480 Ma old zircons from granulite facies rocks from East Hebei Province, North China:Geol. Rev., v. 26, p. 198–207.Google Scholar
  17. [17]
    Wang, K. Y., Yan, Y. H., Yang, R. Y., and Chen, Y. F., 1985: REE geochemistry of early Precambrian charnockites and tonalitic — granodioritic gneisses of the Qianan Region, eastern Hebei, North China:Precambrian Res., v. 27, p. 63–84.CrossRefGoogle Scholar
  18. [18]
    Wang, R. M., He, S., Chen, Z., Li, P., and Dai, F., 1985: Geochemical evolution and metamorphic development of the early Precambrian in eastern Hebei, China:Precambrian Res., v. 27, p. 111–129.CrossRefGoogle Scholar
  19. [19]
    Sills, J. D., Wang, K., Yan, Y., and Windley, B. F., The Archean high grade gneiss terrain in E. Hebei Province, NE China: Geological Framework and Conditions of Metamorphism: Geol. Soc. London, Special Pub. No. 27, p. 297–305 (in press).Google Scholar
  20. [20]
    Chen, J. B., Zhang, H. M., Xing, Y. S., and Ma, G. G., 1981: On the upper Precambrian (Sinian Suberathem) in China:Precambrian Res., v. 15, p. 207–228.CrossRefGoogle Scholar
  21. [21]
    Liu, D. Y., Page, R. W., Compston, W., and Wu, J., 1985: U-Pb zircon geochemistry of Late Archean metamorphic rocks in the Taihangshan — Wutaishan area, North China:Precambrian Res., v. 27, p. 85–109.CrossRefGoogle Scholar
  22. [22]
    Zhang, G.W., Bai, Y. B., Sun, Y., Guo, A. L., Zhou, D. W., and Li, T. H., 1985: Composition and evolution of the Archean crust in central Henan, China:Precambrian Res., v. 27, p. 7–35.CrossRefGoogle Scholar
  23. [23]
    Xu, J. W., Zhu, G., Tong, W. X., Cui, K. R., and Liu, Q., 1987: Formation and evolution of the Tancheng — Lujiang wrench fault system: a major shear system to the northwest of the Pacific Ocean:Tectonophysics, v. 134, p. 273–310.CrossRefGoogle Scholar
  24. [24]
    Klimetz, M. P., 1987: The Mesozoic tectonostratigraphic terranes and accretionary heritage of south—eastern mainland Asia: p. 221–234 in Leitch, E. C., and Scheibner, E. (eds.), Terrane Accretion and Orogenic Belts,Geodynam. Ser., v. 19, Amer. Geophys. Union, 343 p.Google Scholar
  25. [25]
    Zhang, Z. M., and Liu, J. G., 1987: The highP/T metamorphic rocks of China: p. 235–247 in: Leitch, E. C., and Scheibner (eds.), Terrane Accretion and Orogenic Belts,Geodynam. Ser., v. 19, Amer. Geophys. Union, 343 p.Google Scholar
  26. [26]
    Viljoen, M. J., and Viljoen, R. P., 1969: Evidence for the existence of a mobile extrusive peridotitic magma from the Komati Formation of the Onverwacht group: Geol. Soc. South Africa Spec. Pub. 2, Upper Mantle Project, p. 87–112.Google Scholar
  27. [27]
    Arndt, N. T., and Nisbet, E. T., 1982: Komatiites: George Allen and Unwin, 526 p.Google Scholar
  28. [28]
    Guidotti, C. B., Cheney, J. T., and Guggenheim, S., 1977: Distribution of titanium between coexisting muscovite and biotite in metapelites from N. W. Maine:Amer. Mineral., v. 62, p. 438–448.Google Scholar
  29. [29]
    Hamilton, W., 1979: Tectonics of the Indonesian Region: U.S. Geol. Survey Prof. Paper No. 1078, 345 p.Google Scholar
  30. [30]
    Li, C. Y., Wang, Q., Liu, X. Y., and Tang, Y. Q., 1982: Explanatory notes to the tectonic map of Asia: Res. Inst. Geol., Chinese Acad. Geol. Sci., Beijing, 49p.Google Scholar
  31. [31]
    Lee, S. M., 1984: Metamorphic map of South and East Asia: Commission Geol. Map of World, 1: 10000000, Korean Inst. Energy and Resources, Seoul, Korea.Google Scholar
  32. [32]
    Wager, L. R., and Deer, W. A., 1939: Geological investigations in East Greenland, part III, The petrology of the Skaergaard intrusion, Kangerdlugssuaq, East Greenland;Medd. om Gronland, v. 105, no. 4, 352 p.Google Scholar
  33. [33]
    Daly, R. A., 1933: Igneous Rocks and the Depths of the Earth: McGraw-Hill, Inc., New York, 598 p.Google Scholar

Copyright information

© Institute of Geochemistry, Chinese Academy of Sciences 1989

Authors and Affiliations

  • W. G. Ernst
    • 1
  1. 1.Institute of Geophysics and Planetary Physics Department of Earth and Space SciencesUniversity of CaliforniaLos Angeles

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