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Journal of Earth Science

, Volume 29, Issue 6, pp 1291–1303 | Cite as

Geological Evidence for the Operation of Plate Tectonics throughout the Archean: Records from Archean Paleo-Plate Boundaries

  • Timothy M. KuskyEmail author
  • Brian F. Windley
  • Ali Polat
Open Access
Invited Review

Abstract

Plate tectonics describes the horizontal motion of rigid lithospheric plates away from midoceanic ridges and parallel to transforms, towards deep-sea trenches, where the oceanic lithosphere is subducted into the mantle. This process is the surface expression of modern-day heat loss from Earth. One of the biggest questions in Geosciences today is “when did plate tectonics begin on Earth” with a wide range of theories based on an equally diverse set of constraints from geology, geochemistry, numerical modeling, or pure speculation. In this contribution, we turn the coin over and ask “when was the last appearance in the geological record for which there is proof that plate tectonics did not operate on the planet as it does today”. We apply the laws of uniformitarianism to the rock record to ask how far back in time is the geologic record consistent with presently-operating kinematics of plate motion, before which some other mechanisms of planetary heat loss may have been in operation. Some have suggested that evidence shows that there was no plate tectonics before 800 Ma ago, others sometime before 1.8–2.7 Ga, or before 2.7 Ga. Still others recognize evidence for plate tectonics as early as 3.0 Ga, 3.3–3.5 Ga, the age of the oldest rocks, or in the Hadean before 4.3 Ga. A key undiscussed question is: why is there such a diversity of opinion about the age at which plate tectonics can be shown to not have operated, and what criteria are the different research groups using to define plate tectonics, and to recognize evidence of plate tectonics in very old rocks? Here, we present and evaluate data from the rock record, constrained by relevant geochemical-isotopic data, and conclude that the evidence shows indubitably that plate tectonics has been operating at least since the formation of the oldest rocks, albeit with some differences in processes, compositions, and products in earlier times of higher heat generation and mantle temperature, weaker oceanic lithosphere, hotter subduction zones caused by more slab-melt generation, and under different biological and atmospheric conditions.

Key words

Archean tectonics ophiolite OPS (oceanic plate stratigraphy) orogeny 

Notes

Acknowledgments

This work was supported by the National Natural Science Foundation of China (Nos. 91755213, 41672212, 41572203), the MOST Special Fund (No. MSFGPMR02-3) and the Opening Fund (Nos. GPMR201607, 201701) of the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (Wuhan). Miss Yating Zhong is thanked for assistance with final manuscript preparation and figure drafting. We dedicate this contribution to the memory of Kevin Burke, for his lifelong contribution to Precambrian tectonics. The final publication is available at Springer via  https://doi.org/10.1007/s12583-018-0999-6.

References Cited

  1. Abbott, D. H., Hoffman, S. E., 1984. Archaean Plate Tectonics Revisited 1. Heat Flow, Spreading Rate, and the Age of Subducting Oceanic Lithosphere and Their Effects on the Origin and Evolution of Continents. Tectonics, 3(4): 429–448. https://doi.org/10.1029/tc003i004p00429 Google Scholar
  2. Anonymous, 1972. Ophiolites. Geotimes, 17: 24–25Google Scholar
  3. Bleeker, W., Hall, H. C., 2007. The Slave Craton: Geologic and Metallogenic Evolution. In: Goodfellow, W. D., ed., Mineral Deposits of Canada. Geological Association of Canada, Mineral Deposits Division, Special Publication, 5: 849–879Google Scholar
  4. Bradley, D. C., Kusky, T. M., 1992. Deformation History of the McHugh Accretionary Complex, Seldovia Quadrangle, South-Central Alaska. In: Bradley, D. C., Ford, A., eds., Geologic Studies in Alaska. Geologic Studies in Alaska by the U.S. Geological Survey during 1990, United States Geological Survey, Bulletin 1992. 17–32. https://doi.org/alaska.usgs.gov/staff/geology/bradley/pubs/1992_Bradley_McHugh_Grewingk.pdf Google Scholar
  5. Brown, M., 2006. Duality of Thermal Regimes is the Distinctive Characteristic of Plate Tectonics since the Neoarchean. Geology, 34(11): 961–964. https://doi.org/10.1130/g22853a.1 Google Scholar
  6. Brown, M., 2007. Metamorphic Conditions in Orogenic Belts: A Record of Secular Change. International Geology Review, 49(3): 193–234. https://doi.org/10.2747/0020-6814.49.3.193 Google Scholar
  7. Brown, M., Johnson, T., 2018. Secular Change in Metamorphism and the Onset of Global Plate Tectonics. American Mineralogist, 103(2): 181–196. https://doi.org/10.2138/am-2018-6166 Google Scholar
  8. Burke, K., Kidd, W. S. F., Kusky, T. M., 1985. The Pongola Structure of Southeastern Africa: The World’s Oldest Preserved Rift?. Journal of Geodynamics, 2(1): 35–49. https://doi.org/10.1016/0264-3707(85)90031-6 Google Scholar
  9. Calvert, A. J., Sawyer, E. W., Davis, W. J., et al., 1995. Archaean Subduction Inferred from Seismic Images of a Mantle Suture in the Superior Province. Nature, 375(6533): 670–674. https://doi.org/10.1038/375670a0 Google Scholar
  10. Casey, J. F., Dewey, J. F., Fox, P. J., et al., 1981. Heterogeneous Nature of Oceanic Crust and Upper Mantle: A Perspective from the Bay of Islands Ophiolite Complex. The Sea, 7: 305–338Google Scholar
  11. Cawood, P. A., Kröner, A., Pisarevsky, S., 2006. Precambrian Plate Tectonics: Criteria and Evidence. GSA Today, 16(7): 4–11. https://doi.org/10.1130/gsat01607.1 Google Scholar
  12. Cawood, P. A., Kröner, A., Collins, W., et al., 2009. Earth Accretionary Orogens in Space and Time. Geological Society of London Special Publications, 318: 1–36Google Scholar
  13. Coleman, R. G., 2012. Ophiolites: Ancient Oceanic Lithosphere?. Springer, Berlin. 229Google Scholar
  14. Collet, L. W., 1927. The Structure of the Alps, 2nd Edition. E. Arnold, London. 304Google Scholar
  15. Condie, K. C., 2018. A Planet in Transition: The Onset of Plate Tectonics on Earth between 3 and 2 Ga?. Geoscience Frontiers, 9(1): 51–60. https://doi.org/10.1016/j.gsf.2016.09.001 Google Scholar
  16. Condie, K. C., Kröner, A., 2008. When did Plate Tectonics Begin? Evidence from the Geologic Record. In: Condie, K. C., Pease, V., eds., When did Plate Tectonics Begin on Planet Earth? Geological Society of America Special Paper, 440: 281–294Google Scholar
  17. Cook, F. A., van der Velden, A. J., Hall, K. W., et al., 1999. Frozen Subduction in Canada’s Northwest Territories: Lithoprobe Deep Lithospheric Reflection Profiling of the Western Canadian Shield. Tectonics, 18(1): 1–24. https://doi.org/10.1029/1998tc900016 Google Scholar
  18. de Wit, M. J., 2004. Archean Greenstone Belts do Contain Fragments of Ophiolites. In: Kusky, T. M., ed., Precambrian Ophiolites and Related Rocks. Developments in Precambrian Geology 13. Elsevier, Amsterdam. 599–614Google Scholar
  19. de Wit, M. J., Ashwal, L. D., 1997. Greenstone Belts. Oxford Monograph on Geology and Geophysics 35. Clarendon Press, Oxford. 809Google Scholar
  20. de Wit, M. J., Furnes, H., MacLennan, S., et al., 2018. Paleoarchean Bedrock Lithologies Across the Makhonjwa Mountains of South Africa and Swaziland Linked to Geochemical, Magnetic and Tectonic Data Reveal Early Plate Tectonic Genes Flanking Subduction Margins. Geoscience Frontiers, 9(3): 603–665. https://doi.org/10.1016/j.gsf.2017.10.005 Google Scholar
  21. Dewey, J. F., 1977. Suture Zone Complexities: A Review. Tectonophysics, 40(1/2): 53–67. https://doi.org/10.1016/0040-1951(77)90029-4 Google Scholar
  22. Dewey, J. F., Bird, J. M., 1970. Mountain Belts and the New Global Tectonics. Journal of Geophysical Research, 75(14): 2625–2647. https://doi.org/10.1029/jb075i014p02625 Google Scholar
  23. Dhuime, B., Hawkesworth, C. J., Cawood, P. A., et al., 2012. A Change in the Geodynamics of Continental Growth 3 Billion Years Ago. Science, 335(6074): 1334–1336. https://doi.org/10.1126/science.1216066 Google Scholar
  24. Dilek, Y., Furnes, H., 2011. Ophiolite Genesis and Global Tectonics: Geochemical and Tectonic Fingerprinting of Ancient Oceanic Lithosphere. Geological Society of America Bulletin, 123(3/4): 387–411. https://doi.org/10.1130/b30446.1 Google Scholar
  25. Dokukina, K. A., Kaulina, T. V., Konilov, A. N., et al., 2014. Archaean to Palaeoproterozoic High-Grade Evolution of the Belomorian Eclogite Province in the Gridino Area, Fennoscandian Shield: Geochronological Evidence. Gondwana Research, 25(2): 585–613. https://doi.org/10.1016/j.gr.2013.02.014 Google Scholar
  26. Dolan, J. F., Mann, P., 1998. Active Strike-Slip and Collisional Tectonics of the Northern Caribbean Plate Boundary Zone. Geological Society of America Special Paper, 326: 174Google Scholar
  27. Drabon, N., Lowe, D. R., Byerly, G. R., et al., 2017. Detrital Zircon Geochronology of Sandstones of the 3.6–3.2 Ga Barberton Greenstone Belt: No Evidence for Older Continental Crust. Geology, 45(9): 803–806. https://doi.org/10.1130/g39255.1 Google Scholar
  28. Drummond, B. J., Goleby, B. R., Swager, C. P., 2000. Crustal Signature of Late Archaean Tectonic Episodes in the Yilgarn Craton, Western Australia: Evidence from Deep Seismic Sounding. Tectonophysics, 329(1/2/3/4): 193–221. https://doi.org/10.1016/s0040-1951(00)00196-7 Google Scholar
  29. Duncan, M. S., Dasgupta, R., 2017. Rise of Earth’s Atmospheric Oxygen Controlled by Efficient Subduction of Organic Carbon. Nature Geoscience, 10(5): 387–392. https://doi.org/10.1038/ngeo2939 Google Scholar
  30. Ernst, W. G., 1972. Occurrence and Mineralogic Evolution of Blueschist Belts with Time. American Journal of Science, 272(7): 657–668. https://doi.org/10.2475/ajs.272.7.657 Google Scholar
  31. Ernst, W. G., 1973. Blueschist Metamorphism and P-T Regimes in Active Subduction Zones. Tectonophysics, 17(3): 255–272. https://doi.org/10.1016/0040-1951(73)90006-1 Google Scholar
  32. Fitch, T. J., 1972. Plate Convergence, Transcurrent Faults, and Internal Deformation Adjacent to Southeast Asia and the Western Pacific. Journal of Geophysical Research, 77(23): 4432–4460. https://doi.org/10.1029/jb077i023p04432 Google Scholar
  33. Foley, B. J., Bercovici, D., Elkins-Tanton, L. T., 2014. Initiation of Plate Tectonics from Post-Magma Ocean Thermochemical Convection. Journal of Geophysical Research: Solid Earth, 119(11): 8538–8561. https://doi.org/10.1002/2014jb011121 Google Scholar
  34. Foley, S. F., Buhre, S., Jacob, D. E., 2003. Evolution of the Archaean Crust by Delamination and Shallow Subduction. Nature, 421(6920): 249–252. https://doi.org/10.1038/nature01319 Google Scholar
  35. Fritz, H., Abdelsalam, M., Ali, K. A., et al., 2013. Orogen Styles in the East African Orogens: A Review of Neoproterozoic to Early Phanerozoic Tectonic Evolution. Journal of African Earth Sciences, 86: 65–106Google Scholar
  36. Furnes, H., de Wit, M., Dilek, Y., 2014. Four Billion Years of Ophiolites Reveal Secular Trends in Oceanic Crust Formation. Geoscience Frontiers, 5(4): 571–603. https://doi.org/10.1016/j.gsf.2014.02.002 Google Scholar
  37. Furnes, H., de Wit, M., Staudigel, H., et al., 2007. A Vestige of Earth’s Oldest Ophiolite. Science, 315(5819): 1704–1707. https://doi.org/10.1126/science.1139170 Google Scholar
  38. Furnes, H., Dilek, Y., de Wit, M., 2015. Precambrian Greenstone Sequences Represent Different Ophiolite Types. Gondwana Research, 27(2): 649–685. https://doi.org/10.1016/j.gr.2013.06.004 Google Scholar
  39. Ganne, J., De Andrade, V., Weinberg, R. F., et al., 2011. Modern-Style Plate Subduction Preserved in the Palaeoproterozoic West African Craton. Nature Geoscience, 5(1): 60–65. https://doi.org/10.1038/ngeo1321 Google Scholar
  40. Gold, D. J. C., 2006. The Pongola Supergroup. In: Johnson, M. R., Anhaeusser, C. R., Thomas, R. J., eds., The Geology of South Africa. Geological Society of South Africa, Johannesburg. 135–147Google Scholar
  41. Grosch, E., Slama, J., 2017. Evidence for 3.3-Billion-Year-Old Oceanic Crust in the Barberton Greenstone Belt, South Africa. Geology, 45: 695–698. https://doi.org/10.1130/g39035.1 Google Scholar
  42. Harrison, T. M., 2009. The Hadean Crust: Evidence from >4 Ga Zircons. Annual Review of Earth and Planetary Sciences, 37(1): 479–505. https://doi.org/10.1146/annurev.earth.031208.100151 Google Scholar
  43. Hickman, A. H., 2012. Review of the Pilbara Craton and Fortescue Basin, Western Australia: Crustal Evolution Providing Environments for Early Life. Island Arc, 21(1): 1–31. https://doi.org/10.1111/j.1440-1738.2011.00783.x Google Scholar
  44. Hildebrand, R. S., 2005. Autochthonous and Allochthonous Strata of the El Callao Greenstone Belt: Implications for the Nature of the Paleoproterozoic Trans-Amazonian Orogeny and the Origin of Gold-Bearing Shear Zones in the El Callao Mining District, Guayana Shield, Venezuela. Precambrian Research, 143(1/2/3/4): 75–86. https://doi.org/10.1016/j.precamres.2005.09.009 Google Scholar
  45. Hildebrand, R. S., 2013. Mesozoic Assembly of the North American Cordillera. Geological Society of America Special Paper, 495: 178Google Scholar
  46. Kato, Y., Nakamura, K., 2003. Origin and Global Tectonic Significance of Early Archean Cherts from the Marble Bar Greenstone Belt, Pilbara Craton, Western Australia. Precambrian Research, 125(3/4): 191–243. https://doi.org/10.1016/s0301-9268(03)00043-3 Google Scholar
  47. Kato, Y., Ohta, I., Tsunematsu, T., et al., 1998. Rare Earth Element Variations in Mid-Archean Banded Iron Formations: Implications for the Chemistry of Ocean and Continent and Plate Tectonics. Geochimica et Cosmochimica Acta, 62(21/22): 3475–3497. https://doi.org/10.1016/s0016-7037(98)00253-1 Google Scholar
  48. Keller, B., Schoene, B., 2018. Plate Tectonics and Continental Basaltic Geochemistry throughout Earth History. Earth and Planetary Science Letters, 481: 290–304. https://doi.org/10.1016/j.epsl.2017.10.031 Google Scholar
  49. Kersting, A., 1995. Pb Isotope Ratios of North Pacific Sediments, Sites 881, 883, and 884: Implications for Sediment Recycling in the Kamchatkan Arc. In: Rea, D. K., Baslov, I. A., Scholl, D. W., et al., eds., Proceedings of the Ocean Drilling Program, Scientific Results, 145: 383–388Google Scholar
  50. Komiya, T., Yamamoto, S., Aoki, S., et al., 2015. Geology of the Eoarchean, >3.95 Ga, Nulliak Supracrustal Rocks in the Saglek Block, Northern Labrador, Canada: The Oldest Geological Evidence for Plate Tectonics. Tectonophysics, 662: 40–66. https://doi.org/10.1016/j.tecto.2015.05.003 Google Scholar
  51. Komiya, T., Yamamoto, S., Aoki, S., et al., 2017. A Prolonged Granitoid Formation in Saglek Block, Labrador: Zonal Growth and Crustal Reworking of Continental Crust in the Eoarchean. Geoscience Frontiers, 8(2): 355–385. https://doi.org/10.1016/j.gsf.2016.06.013 Google Scholar
  52. Korenaga, J., 2006. Archean Geodynamics and the Thermal Evolution of Earth. In: Benn, K., Mareschal, J.-C., Condie, K. C., eds., Archean Geodynamics and Environments. American Geophysical Union Monograph, 164: 7–32Google Scholar
  53. Korenaga, J., 2013. Initiation and Evolution of Plate Tectonics on Earth: Theories and Observations. Annual Review of Earth and Planetary Sciences, 41(1): 117–151. https://doi.org/10.1146/annurev-earth-050212-124208 Google Scholar
  54. Korsch, R. J., Kositcin, N., Champion, D. C., 2011. Australian Island Arcs through Time: Geodynamic Implications for the Archean and Proterozoic. Gondwana Research, 19(3): 716–734. https://doi.org/10.1016/j.gr.2010.11.018 Google Scholar
  55. Krapez, B., Barley, M. E., 1987. Archaean Strike-Slip Faulting and Related Ensialic Basins: Evidence from the Pilbara Block, Australia. Geological Magazine, 124(6): 555–567. https://doi.org/10.1017/s0016756800017386 Google Scholar
  56. Kusky, T. M., 1989. Accretion of the Archean Slave Province. Geology, 17(1): 63–67.  https://doi.org/10.1130/0091-7613(1989)017<0063:aotasp>2.3.co;2 Google Scholar
  57. Kusky, T. M., 1993. Collapse of Archean Orogens and the Generation of Late-to Postkinematic Granitoids. Geology, 21(10): 925–928.  https://doi.org/10.1130/0091-7613(1993)021<0925:coaoat>2.3.co;2 Google Scholar
  58. Kusky, T. M., 1998. Tectonic Setting and Terrane Accretion of the Archean Zimbabwe Craton. Geology, 26(2): 163–166.  https://doi.org/10.1130/0091-7613(1998)026<0163:tsatao>2.3.co;2 Google Scholar
  59. Kusky, T. M., Li, J. H., Tucker, R. D., 2001. The Archean Dongwanzi Ophiolite Complex, North China Craton: 2.505-Billion-Year-Old Oceanic Crust and Mantle. Science, 292(5519): 1142–1145. https://doi.org/10.1126/science.1059426 Google Scholar
  60. Kusky, T. M., 2004. Precambrian Ophiolites and Related Rocks, Introduction. In: Kusky, T. M., ed., Precambrian Ophiolites and Related Rocks, Developments in Precambrian Geology 13. Elsevier, Amsterdam. 1–35Google Scholar
  61. Kusky, T. M., 2011. Geophysical and Geological Tests of Tectonic Models of the North China Craton. Gondwana Research, 20(1): 26–35. https://doi.org/10.1016/j.gr.2011.01.004 Google Scholar
  62. Kusky, T. M., Bradley, D. C., 1999. Kinematic Analysis of Mélange Fabrics: Examples and Applications from the McHugh Complex, Kenai Peninsula, Alaska. Journal of Structural Geology, 21(12): 1773–1796. https://doi.org/10.1016/s0191-8141(99)00105-4 Google Scholar
  63. Kusky, T. M., Li, J. H., 2010. Origin and Emplacement of Archean Ophiolites of the Central Orogenic Belt, North China Craton. Journal of Earth Science, 21(5): 744–781. https://doi.org/10.1007/s12583-010-0119-8 Google Scholar
  64. Kusky, T. M., Li, X. Y., Wang, Z. S., et al., 2014a. Are Wilson Cycles Preserved in Archean Cratons? A Comparison of the North China and Slave Cratons. Canadian Journal of Earth Sciences, 51(3): 297–311. https://doi.org/10.1139/cjes-2013-0163 Google Scholar
  65. Kusky, T. M., Windley, B. F., Wang, L., et al., 2014b. Flat Slab Subduction, Trench Suction, and Craton Destruction: Comparison of the North China, Wyoming, and Brazilian Cratons. Tectonophysics, 630: 208–221. https://doi.org/10.1016/j.tecto.2014.05.028 Google Scholar
  66. Kusky, T. M., Polat, A., 1999. Growth of Granite-Greenstone Terranes at Convergent Margins, and Stabilization of Archean Cratons. Tectonophysics, 305(1/2/3): 43–73. https://doi.org/10.1016/s0040-1951(99)00014-1 Google Scholar
  67. Kusky, T. M., Polat, A., Windley, B. F., et al., 2016. Insights into the Tectonic Evolution of the North China Craton through Comparative Tectonic Analysis: A Record of Outward Growth of Precambrian Continents. Earth-Science Reviews, 162: 387–432. https://doi.org/10.1016/j.earscirev.2016.09.002 Google Scholar
  68. Kusky, T. M., Stern, R. J., Dewey, J. F., 2013a. Secular Changes in Geologic and Tectonic Processes. Gondwana Research, 24(2): 451–452. https://doi.org/10.1016/j.gr.2013.03.015 Google Scholar
  69. Kusky, T. M., Windley, B. F., Safonova, I., et al., 2013b. Recognition of Ocean Plate Stratigraphy in Accretionary Orogens through Earth History: A Record of 3.8 Billion Years of Sea Floor Spreading, Subduction, and Accretion. Gondwana Research, 24(2): 501–547. https://doi.org/10.1016/j.gr.2013.01.004 Google Scholar
  70. Kusky, T. M., Vearncombe, J., 1997. Structure of Archean Greenstone Belts. In: de Wit, M. J., Ashwal, L. D., eds., Tectonic Evolution of Greenstone Belts. Oxford Monograph on Geology and Geophysics. Clarendon Press, Oxford. 95–128Google Scholar
  71. Kusky, T. M., Wang, L., Dilek, Y., et al., 2011. Application of the Modern Ophiolite Concept with Special Reference to Precambrian Ophiolites. Science China Earth Sciences, 54(3): 315–341. https://doi.org/10.1007/s11430-011-4175-4 Google Scholar
  72. Kusky, T. M., Zhai, M. G., 2012. The Neoarchean Ophiolite in the North China Craton: Early Precambrian Plate Tectonics and Scientific Debate. Journal of Earth Science, 23(3): 277–284. https://doi.org/10.1007/s12583-012-0253-6 Google Scholar
  73. Liou, J. G., Maruyama, S., Wang, X., et al., 1990. Precambrian Blueschist Terranes of the World. Tectonophysics, 181(1/2/3/4): 97–111. https://doi.org/10.1016/0040-1951(90)90010-6 Google Scholar
  74. Maruyama, S., Kawai, T., Windley, B. F., 2010. Ocean Plate Stratigraphy and Its Imbrication in an Accretionary Orogen: The Mona Complex, Anglesey-Lleyn, Wales, UK. Geological Society, London, Special Publications, 338(1): 55–75. https://doi.org/10.1144/sp338.4a Google Scholar
  75. Maruyama, S., Santosh, M., Azuma, S., 2018. Initiation of Plate Tectonics in the Hadean: Eclogitization Triggered by the ABEL Bombardment. Geoscience Frontiers, 9(4): 1033–1048. https://doi.org/10.1016/j.gsf.2016.11.009 Google Scholar
  76. McClay, K. R., 2012. Thrust Tectonics. Springer, Netherlands. 447Google Scholar
  77. Mohan, M. R., Satyanarayanan, M., Santosh, M., et al., 2013. Neoarchean Suprasubduction Zone Arc Magmatism in Southern India: Geochemistry, Zircon U-Pb Geochronology and Hf Isotopes of the Sittampundi Anorthosite Complex. Gondwana Research, 23(2): 539–557. https://doi.org/10.1016/j.gr.2012.04.004 Google Scholar
  78. Moyen, J.-F., Stevens, G., Kisters, A. F. M., 2006. 3.2 Ga High-Pressure, Low-Temperature Metamorphism in the Barberton Greenstone Belt: The Evidence for Archaean Mountain Belts and Subduction Zones. In: Condie, K. C., Kröner, A., Stein, R. J., eds., When did Plate Tectonics Begin on Earth? Theoretical and Empirical Constraints. GSA Penrose Conference, Geological Society of America. 13–18 June 2006, Lander, WyomingGoogle Scholar
  79. Musacchio, G., White, D. J., Asudeh, I., et al., 2004. Lithospheric Structure and Composition of the Archean Western Superior Province from Seismic Refraction/Wide-Angle Reflection and Gravity Modeling. Journal of Geophysical Research, 109(B3): B03304. https://doi.org/10.1029/2003jb002427 Google Scholar
  80. Myers, J. S., 1995. The Generation and Assembly of an Archaean Supercontinent: Evidence from the Yilgarn Craton, Western Australia. Geological Society, London, Special Publications, 95(1): 143–154. https://doi.org/10.1144/gsl.sp.1995.095.01.09 Google Scholar
  81. Næraa, T., Scherstén, A., Rosing, M. T., et al., 2012. Hafnium Isotope Evidence for a Transition in the Dynamics of Continental Growth 3.2 Gyr Ago. Nature, 485(7400): 627–630. https://doi.org/10.1038/nature11140 Google Scholar
  82. Nutman, A. P., Bennett, V. C., Friend, C. R. L., 2015. The Emergence of the Eoarchaean Proto-Arc: Evolution of a C. 3 700 Ma Convergent Plate Boundary at Isua, Southern West Greenland. Geological Society, London, Special Publications, 389(1): 113–133. https://doi.org/10.1144/sp389.5 Google Scholar
  83. Percival, J. A., Skulski, T., Sanborn-Barrie, M., et al., 2012. Geology and Tectonic Evolution of the Superior Province, Canada. In: Percival, J. A., Cook, F. A., Clowes, R. M., eds., Tectonic Styles in Canada: The Lithoprobe Perspective. Geological Association of Canada Special Paper, 49: 321–378Google Scholar
  84. Plank, T., Ludden, J. N., Escutia, C., et al., 2000. Site 1149. Proceedings of the Ocean Drilling Program, Initial Reports. 185Google Scholar
  85. Polat, A., 2012. Growth of Archean Continental Crust in Oceanic Island Arcs. Geology, 40(4): 383–384. https://doi.org/10.1130/focus042012.1 Google Scholar
  86. Richardson, S. H., Shirey, S. B., 2008. Continental Mantle Signature of Bushveld Magmas and Coeval Diamonds. Nature, 453(7197): 910–913. https://doi.org/10.1038/nature07073 Google Scholar
  87. Richardson, S. H., Shirey, S. B., Harris, J. W., et al., 2001. Archean Subduction Recorded by Re-Os Isotopes in Eclogitic Sulfide Inclusions in Kimberley Diamonds. Earth and Planetary Science Letters, 191(3/4): 257–266. https://doi.org/10.1016/s0012-821x(01)00419-8 Google Scholar
  88. Rollinson, H., 2010. Coupled Evolution of Archean Continental Crust and Subcontinental Lithospheric Mantle. Geology, 38(12): 1083–1086. https://doi.org/10.1130/g31159.1 Google Scholar
  89. Sajeev, K., Windley, B. F., Connolly, J. A. D., et al., 2009. Retrogressed Eclogite (20 kbar, 1 020 °C) from the Neoproterozoic Palghat-Cauvery Suture Zone, Southern India. Precambrian Research, 171(1/2/3/4): 23–36. https://doi.org/10.1016/j.precamres.2009.03.001 Google Scholar
  90. Sawaki, Y., Shibuya, T., Kawai, T., et al., 2010. Imbricated Ocean-Plate Stratigraphy and U-Pb Zircon Ages from Tuff Beds in Cherts in the Ballantrae Complex, SW Scotland. Geological Society of America Bulletin, 122(3/4): 454–464. https://doi.org/10.1130/b26329.1 Google Scholar
  91. Şengör, A. M. C., Natal’in, B. A., Sunal, G., et al., 2014. A New Look at the Altaids: A Superorogenic Complex in Northern and Central Asia as a Factory of Continental Crust. Part I: Geological Data Compilation (Exclusive of Palaeomagnetic Observations). Austrian Journal of Earth Sciences, 107: 169–232Google Scholar
  92. Shibuya, T., Komiya, T., Nakamura, K., et al., 2010. Highly Alkaline, High-Temperature Hydrothermal Fluids in the Early Archean Ocean. Precambrian Research, 182(3): 230–238. https://doi.org/10.1016/j.precamres.2010.08.011 Google Scholar
  93. Shipboard Scientific Party, 2000. Leg 190 Preliminary Report: Deformation and Fluid Flow Processes in the Nankai Trough Accretionary Prism. ODP Prelim. Rpt., 190. [2018-10-29]. https://doi.org/www-odp.tamu.edu/publications/prelim/190_prel/190Prel.pdf
  94. Shirey, S. B., Richardson, S. H., 2011. Start of the Wilson Cycle at 3 Ga Shown by Diamonds from Subcontinental Mantle. Science, 333(6041): 434–436. https://doi.org/10.1126/science.1206275 Google Scholar
  95. Sleep, N. H., Windley, B. F., 1982. Archean Plate Tectonics: Constraints and Inferences. The Journal of Geology, 90(4): 363–379. https://doi.org/10.1086/628691 Google Scholar
  96. Smart, K. A., Tappe, S., Stern, R. A., et al., 2016. Early Archaean Tectonics and Mantle Redox Recorded in Witwatersrand Diamonds. Nature Geoscience, 9(3): 255–259. https://doi.org/10.1038/ngeo2628 Google Scholar
  97. Smithies, R. H., Van Kranendonk, M. J., Champion, D. C., 2007. The Mesoarchean Emergence of Modern-Style Subduction. Gondwana Research, 11(1/2): 50–68. https://doi.org/10.1016/j.gr.2006.02.001 Google Scholar
  98. Sol, S., Thomson, C. J., Kendall, J. M., et al., 2002. Seismic Tomographic Images of the Cratonic Upper Mantle beneath the Western Superior Province of the Canadian Shield—A Remnant Archean Slab?. Physics of the Earth and Planetary Interiors, 134(1/2): 53–69. https://doi.org/10.1016/s0031-9201(02)00081-x Google Scholar
  99. Stern, R. J., 2007. When and how did Plate Tectonics Begin? Theoretical and Empirical Considerations. Chinese Science Bulletin, 52(5): 578–591. https://doi.org/10.1007/s11434-007-0073-8 Google Scholar
  100. Stern, R. J., 2008. Modern-Style Plate Tectonics Began in Neoproterozoic Time: An Alternative Interpretation of Earth’s Tectonic History. Geological Society of America Special Paper, 440: 265–280Google Scholar
  101. Szilas, K., Tusch, J., Hoffmann, J. E., et al., 2016. Hafnium Isotope Constraints on the Origin of Mesoarchaean Andesites in Southern West Greenland, North Atlantic Craton. Geological Society, London, Special Publications, 449(1): 19–38. https://doi.org/10.1144/sp449.2 Google Scholar
  102. van Hunen, J., Moyen, J. F., 2012. Archean Subduction: Fact or Fiction?. Annual Review of Earth and Planetary Sciences, 40(1): 195–219. https://doi.org/10.1146/annurev-earth-042711-105255 Google Scholar
  103. von Huene, R., Scholl, D. W., 1993. The Return of Sialic Material to the Mantle Indicated by Terrigeneous Material Subducted at Convergent Margins. Tectonophysics, 219(1/2/3): 163–175. https://doi.org/10.1016/0040-1951(93)90294-t Google Scholar
  104. Wakita, K., 1997. Accretionary Complex and Ocean Plate Stratigraphy. Earth Science (Chikyu Kagaku), 51: 300–310 (in Japanese)Google Scholar
  105. Wakita, K., 2012. Mappable Features of Mélanges Derived from Ocean Plate Stratigraphy in the Jurassic Accretionary Complexes of Mino and Chichibu Terranes in Southwest Japan. Tectonophysics, 568/569: 74–85. https://doi.org/10.1016/j.tecto.2011.10.019 Google Scholar
  106. Wang, J. P., Kusky, T. M., Polat, A., et al., 2013. A Late Archean Tectonic Mélange in the Central Orogenic Belt, North China Craton. Tectonophysics, 608: 929–946. https://doi.org/10.1016/j.tecto.2013.07.025 Google Scholar
  107. Wang, J. P., Kusky, T. M., Wang, L., et al., 2016. Structural Relationships along a Neoarchean Arc-Continent Collision Zone, North China Craton. Geological Society of America Bulletin, 129(1/2): 59–75. https://doi.org/10.1130/b31479.1 Google Scholar
  108. Wilson, J. T., 1965. A New Class of Faults and Their Bearing on Continental Drift. Nature, 207(4995): 343–347. https://doi.org/10.1038/207343a0 Google Scholar
  109. Wilson, J. T., 1968. Static or Mobile Earth: The Current Scientific Revolution. Proceedings American Philosophical Society, 112: 309–320Google Scholar
  110. Windley, B. F., 1993. Uniformitarianism Today: Plate Tectonics is the Key to the Past. Journal of the Geological Society, 150(1): 7–19. https://doi.org/10.1144/gsjgs.150.1.0007 Google Scholar
  111. Windley, B. F., Garde, A. A., 2009. Arc-Generated Blocks with Crustal Sections in the North Atlantic Craton of West Greenland: Crustal Growth in the Archean with Modern Analogues. Earth-Science Reviews, 93(1/2): 1–30. https://doi.org/10.1016/j.earscirev.2008.12.001 Google Scholar
  112. Zibra, I., Korhonen, F. J., Peternell, M., et al., 2017. On Thrusting, Regional Unconformities and Exhumation of High-Grade Greenstones in Neoarchean Orogens. the Case of the Waroonga Shear Zone, Yilgarn Craton. Tectonophysics, 712/713: 362–395. https://doi.org/10.1016/j.tecto.2017.05.017 Google Scholar

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Authors and Affiliations

  1. 1.State Key Laboratory for Geological Processes and Mineral ResourcesChina University of GeosciencesWuhanChina
  2. 2.Center for Global Tectonics, School of Earth SciencesChina University of GeosciencesWuhanChina
  3. 3.Department of GeologyUniversity of LeicesterLeicesterUK
  4. 4.Department of Earth and Environmental SciencesUniversity of WindsorOntarioCanada

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