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.
Similar content being viewed by others
References
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.
Wang, Q., Cong, B., Supracrustal sleeve experienced ultrahigh-pressure metamorphism,Continental Dynamics, 1998, 12: 54.
Dobrzhineskaya, L., Green, H. W., Wang, S., Alpe Arami: a peridotite massif from depths more than 300 km,Science, 1996, 272: 1841.
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.
Haggerty, S. E., Sauter, V., Ultra-deep (> 300 km) ultramafic upper mantle xenoliths,Science, 1990, 248: 993.
Sauter, V., Haggerty, S. E., Field, S., Ultra-deep (> 300 km) ultramafic xenolith: new petrologic evidence from the transition zone,Science, 1991, 252: 827.
Clark, S. P., A redetermination of equilibrium relations between kyanite and sillimanite,Am. J. Sci., 1961, 259: 641.
Touloukian, Y. S., Judd, W, R., Roy, R. F.,Physical Properties of Rocks and Minerals, New York: McGraw-Hill Book Company, 1981, 400.
Carter, N. L., Tsenn, M. C., Flow properties of continental lithosphere,Tectonophysics, 1987, 136: 27.
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.
Mancktelow, N., On metamorphic “pressure” during deformation, Schweiz,Mineral. Petrogr. Mitt., 1993, 73: 340.
Author information
Authors and Affiliations
About this article
Cite this article
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
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF02885943