The DOI matches its Crossref record; 66 of the 66 references it cites were found in a registry or an index.
Archean Plate Tectonics: Constraints and Inferences
Abstract
The earth has been cooling since Archean time. The higher temperatures beneath Archean ridges resulted in more partial melting which extended down to greater depths than at present. The Archean oceanic crust was much thicker (>20 km) than modern crust (~5 km). This inference is compatible with previous ideas of suspected oceanic crust. The thicker oceanic crust in the Archean tended to resist subduction similar to modern aseismic ridges, but could not prevent it. Short-lived episodes of intra-arc spreading followed by Cordilleran-type compression may have produced Archean greenstone belts. Archean meta-tonalites represent a significant part of the continental crust and were probably produced by melting of the subducted slab which was favored by the higher mantle temperatures.
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Citations
Cites
Implications of plate tectonics for the Cenozoic tectonic evolution of western North America
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Anhydrous melting of peridotite at 0?15 Kb pressure and the genesis of tholeiitic basalts
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Windley, B. F. (1977) · Andalas University Repository (Andalas University) · Cited by 841
Self-citationPetrogenesis of basalts from the FAMOUS area: Mid-Atlantic Ridge
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Chemical characteristics and origin of oceanic ridge volcanic rocks1
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A phase diagram for mid-ocean ridge basalts: Preliminary results and implications for petrogenesis
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Cited by
Partial melting of amphibolite/eclogite and the origin of Archean trondhjemites and tonalites
Rapp, R. P., Watson, E. B., & Miller, C. F. (1991) · Precambrian Research · doi:10.1016/0301-9268(91)90092-o · Cited by 1,260
Thermal history of the Earth and its petrological expression
Herzberg, C., Condie, K., & Korenaga, J. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.01.022 · Cited by 1,148
Bédard, J. H. (2006) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2005.11.008 · Cited by 887
Phanerozoic addition rates to the continental crust and crustal growth
Reymer, A., & Schubert, G. (1984) · Tectonics · doi:10.1029/tc003i001p00063 · Cited by 569
Melting in an Archaean mantle plume: Heads it’s basalts, tails it’s komatiites
Campbell, I. H., Griffiths, R. W., & Hill, R. I. (1989) · Nature · doi:10.1038/339697a0 · Cited by 470
Metadata
- Authors
- Sleep, N. H., & Windley, B. F.
- Venue
- The Journal of Geology
- Publisher
- University of Chicago Press
- Published
- 1982-07
- Volume
- 90
- Issue
- 4
- Pages
- 363-379
- ISSN
- 0022-1376 (ISSN-L)
- 1537-5269
- OpenAlex
- W2081583490
- Cited by
- 373
- References
- 66
- FWCI
- 6.38
- Type
- journal article
- Language
- en
- Open access
- closed
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