Page 11 - i1052-5173-26-9
P. 11
Holmes, A., 1965, Principles of Physical Geology: London, Nelson, 1288 p. Early Precambrian: Physics of the Earth and Planetary Interiors, v. 146, GSA TODAY | www.geosociety.org/gsatoday
Hutton, J., 1785, Abstract of a dissertation read in the Royal Society of p. 369–394, doi: 10.1016/j.pepi.2003.09.024.
Roberts, N.M.W., and Spencer, C.J., 2014, The zircon archive of continent
Edinburgh, upon the seventh of March, and fourth of April, formation through time: Geological Society, London, Special Publication
MDCCLXXXV, Concerning the System of the Earth, Its Duration, and 389 p., doi: 10.1144/SP1389.1114.
Stability: Edinburgh, 30 p. Rudnick, R.L., and Gao, S., 2003, Composition of the continental crust, in
Hutton, J., 1788, Theory of the Earth; or an Investigation of the Laws observable Rudnick, R.L., ed., Treatise on Geochemistry, v. 3, The Crust: Amsterdam,
in the Composition, Dissolution, and Restoration of Land upon the Elsevier, p. 64.
Globe: Transactions of the Royal Society of Edinburgh, v. 1, p. 209–304, Scholl, D.W., and von Huene, R., 2007, Exploring the implications for
doi: 10.1017/S0080456800029227. continental basement tectonics if estimated rates of crustal removal
Johnson, T.E., Brown, M., Kaus, B.J.P., and VanTongeren, J.A., 2013, (recycling) at Cenozoic subduction zones are applied to Phanerozoic and
Delamination and recycling of Archaean crust caused by gravitational Precambrian convergent ocean margins, in Hatcher, R.D., Jr., Carlson,
instabilities: Nature Geoscience, v. 7, no. 1, p. 47–52, doi: 10.1038/ M.P., McBride, J.H., and Catalán, J.M., eds., 4-D Framework of
ngeo2019. Continental Crust: Geological Society of America Memoir 200, p. 9–32.
Kamber, B.S., 2015, The evolving nature of terrestrial crust from the Hadean, Scholl, D.W., and von Huene, R., 2009, Implications of estimated magmatic
through the Archaean, into the Proterozoic: Precambrian Research, v. 258, additions and recycling losses at the subduction zones of accretionary
p. 48–82, doi: 10.1016/j.precamres.2014.12.007. (non-collisional) and collisional (suturing) orogens, in Cawood, P.A.,
Kamber, B.S., Whitehouse, M.J., Bolhar, R., and Moorbath, S., 2005, Volcanic and Kröner, A., eds., Earth Accretionary Systems in Space and Time:
resurfacing and the early terrestrial crust: Zircon U-Pb and REE Geological Society, London, Special Publication 318, p. 105–125, doi:
constraints from the Isua Greenstone Belt, southern West Greenland: 10.1144/SP318.4.
Earth and Planetary Science Letters, v. 240, no. 2, p. 276–290, doi: 10.1016/ Shields, G.A., 2007, A normalised seawater strontium isotope curve: Possible
j.epsl.2005.09.037. implications for Neoproterozoic-Cambrian weathering rates and the
Kemp, A.I.S., Wilde, S.A., Hawkesworth, C.J., Coath, C.D., Nemchin, A., further oxygenation of the Earth: eEarth, v. 2, p. 35–42.
Pidgeon, R.T., Vervoort, J.D., and DuFrane, S.A., 2010, Hadean crustal Shields, G., and Veizer, J., 2002, Precambrian marine carbonate isotope
evolution revisited: New constraints from Pb-Hf isotope systematics of database: Version 1.1: Geochemistry Geophysics Geosystems, v. 3, no. 6,
the Jack Hills zircons: Earth and Planetary Science Letters, v. 296, no. 1–2, p. 1–12, doi: 10.1029/2001GC000266.
p. 45–56, doi: 10.1016/j.epsl.2010.04.043. Sizova, E., Gerya, T., Brown, M., and Perchuk, L.L., 2010, Subduction styles in
Korenaga, J., 2013, Initiation and evolution of plate tectonics on Earth: Theories the Precambrian: Insight from numerical experiments: Lithos, v. 116,
and observations: Annual Review of Earth and Planetary Sciences, v. 41, no. 3–4, p. 209–229, doi: 10.1016/j.lithos.2009.05.028.
no. 1, p. 117–151, doi: 10.1146/annurev-earth-050212-124208. Sizova, E., Gerya, T., and Brown, M., 2014, Contrasting styles of Phanerozoic
Kramers, J.D., 2002, Global modelling of continent formation and destruction and Precambrian continental collision: Gondwana Research, v. 25, no. 2,
through geological time and implications for CO2 drawdown in the p. 522–545, doi: 10.1016/j.gr.2012.12.011.
Archaean eon, in Fowler, C.M.R., Ebinger, C.J., and Hawkesworth, C.J., Smith, A.B., and McGowan, A.J., 2007, The shape of the Phanerozoic marine
eds., The Early Earth: Physical, Chemical and Biological Development, palaeodiversity curve: How much can be predicted from the sedimentary
Geological Society, London, Special Publication 199, p. 259–274, doi: rock record of Western Europe?: Palaeontology, v. 50, no. 4, p. 765–774,
10.1144/GSL.SP.2002.199.01.13. doi: 10.1111/j.1475-4983.2007.00693.x.
Marchi, S., Bottke, W.F., Elkins-Tanton, L.T., Bierhaus, M., Wuennemann, K., Spencer, C.J., Cawood, P.A., Hawkesworth, C.J., Raub, T.D., Prave, A.R., and
Morbidelli, A., and Kring, D.A., 2014, Widespread mixing and burial of Roberts, N.M.W., 2014, Proterozoic onset of crustal reworking and
Earth’s Hadean crust by asteroid impacts: Nature, v. 511, 7511, p. 578–582, collisional tectonics: Reappraisal of the zircon oxygen isotope record:
doi: 10.1038/nature13539. Geology, v. 42, no. 5, p. 451–454, doi: 10.1130/G35363.1.
McKenzie, D., 1984, The generation and compaction of partially molten rock: Stern, C.R., 2011, Subduction erosion: Rates, mechanisms, and its role in arc
Journal of Petrology, v. 25, no. 3, p. 713–765, doi: 10.1093/petrology/ magmatism and the evolution of the continental crust and mantle:
25.3.713. Gondwana Research, v. 20, no. 2–3, p. 284–308, doi: 10.1016/j.gr.2011
Moore, W.B., and Webb, A.A.G., 2013, Heat-pipe Earth: Nature, v. 501, no. 7468, .03.006.
p. 501–505, doi: 10.1038/nature12473. Stern, R.J., 2005, Evidence from ophiolites, blueschists, and ultrahigh-pressure
Mora, C., Tittensor, D., Adl, S., Simpson, A., and Worm, B., 2011, How many metamorphic terranes that the modern episode of subduction tectonics
species are there on Earth and in the ocean?: PLoS Biology, v. 9, no. 8, began in Neoproterozoic time: Geology, v. 33, no. 7, p. 557–560, doi:
p. 1–8, doi: 10.1371/journal.pbio.1001127. 10.1130/G21365.1.
Nance, R.D., Murphy, J.B., and Santosh, M., 2014, The supercontinent cycle: Tang, M., Chen, K., and Rudnick, R.L., 2016, Archean upper crust transition
A retrospective essay: Gondwana Research, v. 25, no. 1, p. 4–29, doi: 10.1016/ from mafic to felsic marks the onset of plate tectonics: Science, v. 351,
j.gr.2012.12.026. p. 372–375, doi: 10.1126/science.aad5513.
Nisbet, E.G., Cheadle, M.J., Arndt, N.T., and Bickle, M.J., 1993, Constraining Taylor, S.R., and McLennan, S.M., 1985, The Continental Crust: Its Composition
the potential temperature of the Archaean mantle: A review of the and Evolution: Oxford, Blackwell Scientific Publications, 312 p.
evidence from komatiites: Lithos, v. 30, no. 3–4, p. 291–307, doi: 10.1016/ Voice, P.J., Kowalewski, M., and Eriksson, K.A., 2011, Quantifying the timing
0024-4937(93)90042-B. and rate of crustal evolution: Global compilation of radiometrically dated
Parman, S.W., 2015, Time-lapse zirconography: Imaging punctuated detrital zircon grains: The Journal of Geology, v. 119, no. 2, p. 109–126,
continental evolution: Geochemical Perspective Letters, v. 1, p. 43–52, doi: 10.1086/658295.
doi: 10.7185/geochemlet.1505. Western Australia Geological Survey, 2016, Geochemistry Database Search:
Rapp, R.P., and Watson, E.B., 1995, Dehydration melting of metabasalt at Government of Western Australia Department of Mines and Petroleum,
8–32 kbar: Implications for continental growth and crust-mantle http://geochem.dmp.wa.gov.au/geochem/ (last accessed 24 June 2016).
recycling: Journal of Petrology, v. 36, no. 4, p. 891–931, doi: 10.1093/ Wilkinson, B.H., and Kesler, S.E., 2007, Tectonism and exhumation in
petrology/36.4.891. convergent margin orogens: Insights from ore deposits: The Journal of
Raup, D.M., 1972, Taxonomic diversity during the Phanerozoic: Science, v. 177, Geology, v. 115, no. 6, p. 611–627, doi: 10.1086/521606.
no. 4054, p. 1065–1071, doi: 10.1126/science.177.4054.1065.
Rino, S., Komiya, T., Windley, B.F., Katayama, I., Motoki, A., and Hirata, T., Manuscript received 12 Nov. 2015; accepted 1 Apr. 2016.
2004, Major episodic increases of continental crustal growth determined
from zircon ages of river sands; implications for mantle overturns in the
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