Abstract
Recently, Yang et al. (Contrib Mineral Petrol 167:1013, 2014a) proposed that “cataclasites,” “breccias” and “pseudotachylytes” of eclogites at Yangkou in the Chinese Sulu UHP metamorphic belt are formed by “a compression stress wave of earthquake.” They suggested that the intergranular coesite resulted from a rapid cooling from about 700 °C to below 375–400 °C and a “sudden pressure release of seismic wave” from 3.3 to 1.2 GPa in some hours. However, the earthquake-induced UHP metamorphism under fluid-deficient conditions, proposed by these authors, remains inconclusive and inconsistent with the available data from the UHP metamorphic belt. The coesite inclusions within garnet, zircon and omphacite, and intergranular coesite grains between these minerals can be preserved by the presence of the pressure vessel effect, the lack of fluid infiltration, and the presence of a low-temperature and nonhydrostatic deformation environment during rapid exhumation.
References
Austrheim H, Boundy TM (1994) Pseudotachylytes generated during seismic faulting and eclogitization of the deep crust. Science 265:82–83
Brace WF, Kohlstedt DL (1980) Limits on lithospheric stress imposed by laboratory experiments. J Geophys Res 85:6248–6252
Brace WF, Ernst WG, Kallberg RW (1970) An experimental study of tectonic overpressure in Franciscan rocks. Geol Soc Am Bull 81:1325–1338
Burov E, Jolivet L, Le Pourhiet L, Poliakov A (2001) A thermomechanical model of exhumation of high pressure (HP) and ultrahigh pressure (UHP) metamorphic rocks in Alpine-type collision belts. Tectonophysics 342:113–136
Chopin C (2003) Ultrahigh-pressure metamorphism: tracing continental crust into the mantle. Earth Planet Sci Lett 212:1–14
Clark MK, Royden LH (2000) Topographic ooze: building the eastern margin of Tibet by lower crustal flow. Geology 28:703–706
Collettini C, Niemeijer A, Viti C, Marone C (2009) Fault zone fabric and fault weakness. Nature 462:907–911
Di Toro G, Hirose T, Nielsen S, Pennacchioni G, Shimamoto T (2006) Natural and experimental evidence of melt lubrication of faults during earthquakes. Science 311:647–649
Gillet P, Ingrin J, Chopin C (1984) Coesite in subducted continental crust: P-T history deduced from an elastic model. Earth Planet Sci Lett 70:426–436
Green HW (2005) Psychology of a changing paradigm: 40+ years of high-pressure metamorphism. Int Geol Rev 47:439–456
Hemingway BS, Bohlen SR, Hankins WB, Westrum EF Jr, Kuskov OL (1998) Heat capacity and thermodynamic properties for coesite and jadeite, re-examination of the quartz-coesite equilibrium boundary. Am Miner 83:409–418
Hirth G, Tullis J (1992) Dislocation creep regimes in quartz aggregates. J Struct Geol 14:145–159
Ji SC, Wang Q (2010) Interfacial friction-induced pressure and implications for the formation and preservation of intergranular coesite in metamorphic rocks. J Struct Geol 33:107–113
Ji SC, Xia B (2002) Rheology of polyphase earth materials. Polytechnic International Press, Montreal, Canada, p 259
Ji SC, Li A, Wang Q, Long C, Wang H, Marcotte D, Salisbury M (2013) Seismic velocities, anisotropy and shear-wave splitting of antigorite serpentinites and tectonic implications for subduction zones. J Geophys Res 118:1015–1037
Kanamori H (1994) Mechanics of earthquakes. Ann Rev Earth Planet Sci 22:207–237
Kohlstedt DL, Evans B, Mackwell SJ (1995) Strength of the lithosphere: constraints imposed by laboratory experiments. J Geophys Res 100:17587–17602
Lachenbruch AH, Sass JH (1992) Heat flow from Cajon Pass, fault strength, and tectonic implications. J Geophs Res 97:4995–5015
Li ZH, Gerya TV, Burg JP (2010) Influence of tectonic overpressure on P-T paths of HP-UHP rocks in continental collision zones: thermomechanical modeling. J Metamorph Geol 28:227–247
Liou JG, Zhang RY (1996) Occurrence of intragranular coesite in ultrahigh-P rocks from the Sulu region, eastern China: implications for lack of fluid during exhumation. Am Miner 81:1217–1221
Liou JG, Zhang RY, Ernst WG, Rumble D, Maruyama S (1998) High-pressure minerals from deeply subducted metamorphic rocks. In: Hemley RJ (ed) Ultrahigh-pressure mineralogy: physics and chemistry of the earth’s deep interior. Mineralogical Society of America, Washington, pp 33–96
Mancktelow NS (2008) Tectonic pressure: theoretical concepts and modeled examples. Lithos 103:149–177
Melosh HJ (1996) Dynamical weakening of faults by acoustic fluidization. Nature 279:601–606
Moore DE, Lockner DA (2013) Chemical controls on fault behavior: weakening of serpentinite sheared against quartz-bearing rocks and its significance for fault creep in the San Andreas system. J Geophys Res 118:2558–2570
Moore DE, Lockner DA, Ma S, Summers R, Byerlee JD (1997) Strengths of serpentinite gouges at elevated temperatures. J Geophys Res 102:14787–14801
Mosenfelder JL, Bohlen SR (1997) Kinetics of the coesite to quartz transformation. Earth Planet Sci Lett 153:133–147
Mosenfelder JL, Schertl HR, Smyth JR, Liou JG (2005) Factors in the preservation of coesite: the importance of fluid infiltration. Am Miner 90:779–789
Noda H, Dunham EM, Rice JR (2009) Earthquake ruptures with thermal weakening and the operation of major faults at low overall stress levels. J Geophys Res 114:B07302
Parkinson CD, Katayama I (1999) Present-day ultrahigh-pressure conditions of coesite inclusions in zircon and garnet: evidence from laser Raman microspectroscopy. Geology 27:979–982
Passchier CW, Trouw RAJ (2005) Microtectonics. Springer, New York 366
Paterson MS, Wong TF (2005) Experimental rock deformation—the brittle field. Springer, New York 347
Perrillat JP, Daniel I, Lardeaux JM, Cardon H (2003) Kinetics of the coesite-quartz transition: application to the exhumation of ultrahigh-pressure rocks. J Petrol 44:773–788
Petrini K, Podladchikov Y (2000) Lithospheric pressure-depth relationship in compressive regions of thickened crust. J Metamorph Geol 18:67–77
Powell R, Holland TJB (2008) On thermobarometry. J Metamorph Geol 26:155–179
Renner J, Stockhert B, Zerbian A, Roller K, Rummel F (2001) An experimental study into the rheology of synthetic polycrystalline coesite aggregates. J Geophys Res 106:19411–19429
Royden LH, Burchfiel BC, King RW, Wang E, Chen Z, Shen F, Liu Y (1997) Surface deformation and lower crustal flow in eastern Tibet. Science 276:788–790
Rutland RWR (1965) Tectonic overpressures. In: Pitcher WS, Flinn GW (eds) Controls of metamorphism. Oliver & Boyd, Edinburgh, pp 119–139
Schmid SM, Paterson MS, Boland JN (1980) High temperature flow and dynamic recrystallization in Carrara marble. Tectonophysics 65:245–280
Scholz CH (2002) The mechanics of earthquakes and faulting. 2nd edn, Cambridge University Press, Cambridge pp 1-508
Sibson RH, Robert F, Poulsen KH (1988) High-angle reverse faults, fluid-pressure cycling, and mesothermal gold-quartz deposits. Geology 16:551–555
Sleep NH, Blanpied ML (1992) Creep, compaction and the weak rheology of major faults. Nature 359:687–692
Spray JG (1992) A physical basis for the frictional melting of some rock-forming minerals. Tectonophysics 204:205–221
Twiss RJ, Moores EM (1992) Structural geology. Freeman, New York 532
van der Molen I, van Roermund HLM (1986) The pressure path of solid inclusions in minerals: the retention of coesite inclusions during uplift. Lithos 19:317–324
Wain AL, Waters DJ, Austrheim H (2001) Metastability of granulites and processes of eclogitization in the UHP region of western Norway. J Metamorph Geol 19:609–625
Walker AN, Rutter EH, Brodie KH (1990) Experimental study of grain-size sensitive flow of synthetic, hot-pressed calcite rocks. In: Knipe RJ, Agar SM (eds) Deformation mechanisms, rheology and tectonics. Geological Society, UK, pp 259–284
Wallis SR, Ishiwatari A, Hirajima T, Ye K, Guo J, Nakamura D, Kato T, Zhai M, Enami M, Cong B, Banno S (1997) Occurrence and field relationships of ultrahigh-pressure metagranitoid and coesite eclogite in the Su-Lu terrane, eastern China. J Geol Soc 154:45–54
Wibberley CAJ, Shimamoto T (2005) Earthquake slip weakening and asperities explained by thermal pressurization. Nature 436:689–692
Yang JJ, Huang MX, Wu QY, Zhang HR (2014a) Coesite-bearing eclogite breccia: implication for coseismic ultrahigh-pressure metamorphism and the rate of the process. Contrib Mineral Petrol 167:1013
Yang JJ, Fan ZF, Yu C, Yan R (2014b) Coseismic formation of eclogite facies cataclasite dykes at Yangkou in the Chinese Su-Lu UHP metamorphic belt. J Metamorph Geol 32:937–960
Zhang RY, Liou JG (1996) Coesite inclusions in dolomite from eclogite in the southern Dabie Mountains, China: the significance of carbonate minerals in UHPM rocks. Am Miner 81:181–186
Zhang RY, Liou JG (1997) Partial transformation of gabbro to coesite-bearing eclogite from Yankou, the Sulu terrane, eastern China. J Metamorph Geol 15:183–202
Zhao ZY, Wei CJ, Fang AM (2005) Plastic flow of coesite eclogite in a deep continent subduction regime: microstructures, deformation mechanisms and rheological implications. Earth Planet Sci Lett 237:209–222
Acknowledgments
I thank the Natural Sciences and Engineering Research Council of Canada for a discovery grant. The constructive reviews by Drs. Jochen Hoefs, Masaaki Obata and John Spray are highly appreciated.
Author information
Authors and Affiliations
Corresponding author
Additional information
Communicated by Jochen Hoefs.
Rights and permissions
About this article
Cite this article
Ji, S. Discussion on “Coesite-bearing eclogite breccia: implication for coseismic ultrahigh-pressure metamorphism and the rate of the process” by Yang et al. (Contrib. Mineral. Petrol., 2014a, 167: 1013). Contrib Mineral Petrol 170, 1 (2015). https://doi.org/10.1007/s00410-015-1154-3
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s00410-015-1154-3