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Could tectonic overpressure cause ultrahigh-pressure metamorphism?

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Chinese Science Bulletin

Abstract

Could ultrahigh-pressure metamorphic rocks be caused, at depth of 32 km, by tectonic overpressure resulting from differential stress? The differential stress is limited by rock strength, which depends on strain rate and temperature. Therefore, tectonic overpressure could not go beyond 1 GPa, and could not cause the uitrahigh-pressure metamorphism. The stress-strain in plastic deformation, or in plastic stage of elasto-plastic deformation, has no linear relation, and should not be described by using linear equation of elastic deformation.

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References

  1. Lü, G., Chen, J., Li, X., Liu, R., The formation depth of coesite-bearing eclogite, Dabie UHPM zone, China, modified by tectono-original additional hydrostatic pressure,Chinese Science Bulletin, 1999, 44(5): 398.

    Article  Google Scholar 

  2. Wang, Q., Cong, B., Supracrustal sleeve experienced ultrahigh-pressure metamorphism,Continental Dynamics, 1998, 12: 54.

    CAS  Google Scholar 

  3. Dobrzhineskaya, L., Green, H. W., Wang, S., Alpe Arami: a peridotite massif from depths more than 300 km,Science, 1996, 272: 1841.

    Article  Google Scholar 

  4. Jin, Z., Jin, S., Gao, S.et al., Is the depth where UHP rocks were formed in the Dabie Mountains limited to 100–150 km?Chinese Science Bulletin, 1998, 43: 767.

    Google Scholar 

  5. Haggerty, S. E., Sauter, V., Ultra-deep (> 300 km) ultramafic upper mantle xenoliths,Science, 1990, 248: 993.

    Article  PubMed  CAS  Google Scholar 

  6. Sauter, V., Haggerty, S. E., Field, S., Ultra-deep (> 300 km) ultramafic xenolith: new petrologic evidence from the transition zone,Science, 1991, 252: 827.

    Article  Google Scholar 

  7. Clark, S. P., A redetermination of equilibrium relations between kyanite and sillimanite,Am. J. Sci., 1961, 259: 641.

    Google Scholar 

  8. Touloukian, Y. S., Judd, W, R., Roy, R. F.,Physical Properties of Rocks and Minerals, New York: McGraw-Hill Book Company, 1981, 400.

    Google Scholar 

  9. Carter, N. L., Tsenn, M. C., Flow properties of continental lithosphere,Tectonophysics, 1987, 136: 27.

    Article  Google Scholar 

  10. Brace, W. F., Ernst, W. G., Kallberg, R. W., An experimental study of tectonic overpressure in Franciscan rocks,Geol. Soc. Am. Bull., 1970, 81: 1325.

    Article  Google Scholar 

  11. Mancktelow, N., On metamorphic “pressure” during deformation, Schweiz,Mineral. Petrogr. Mitt., 1993, 73: 340.

    Google Scholar 

Download references

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Wang, Q., Liu, J. & Cong, B. Could tectonic overpressure cause ultrahigh-pressure metamorphism?. Chin.Sci.Bull. 44, 2295–2298 (1999). https://doi.org/10.1007/BF02885943

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  • DOI: https://doi.org/10.1007/BF02885943

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